Plate I.— First Conditions of Accumulation and Fusion in Motionless Snow DEUCALION ALSO THE KING OF THE GOLDEN RIVER THE EAGLE'S NEST ARROWS OF THE CHACE BY JOHN RUSKIN, M.A. OF "the seven lamps of architecture," "the crown of wild olive," "sesame and lilies," etc. BOSTON ALDINE book PUBLISHING CO. PUBLISHERS CONTENTS. DEUCALION. Volume I. Introduction, .... CHAPTER I. The Alps and Jura, CHAPTER XL The Three Alras, . , CHAPTER III. On Ice Cream, CHAPTER IV. Labitur, et Labetur, CHAPTER V. The Valley of Cluse, . ctlAPTER v£ Of Butter and Honey, CHAPTER VII. The Iris of the Earth, CHAPTER VIII. The Alphabet, CHAPTER IX, Fife and Water, CHAPTER X. Thirty Years Since, CHAPTER XL Of Silica in Lavas, CHAPTER XII. Yew dale and its Streamlets, CHAPTER XIII. Of Stellar Silica, CHAPTER XIV. SCHISMA MONTIUM, .... APPENDIX, .... Living Waves, Revision, r Kruma Artifex, INDEX, , o Volume II. CHAPTER I. CHAPTER II. CHAPTER III. « » » THE KING OF THE GOLDEN RIVER. CHAPTER I. PAGH How the Agricultural System of the Black Brothers was interfered with by Southwest Wind, Esquire, . . 239 CHAPTER II. Of the Proceedings of the Three Brothers after the Visit of Southwest Wind, Esquire; and how Little Gluck had an Interview with the King of the Golden River 250 CHAPTER III. i • How Mr. Hans set off on an Expedition to the Golden River, and how he prospered therein, . . 258 CHAPTER IV. How Mr. Schwartz set off on an Expedition to the Golden River, and how he prospered therein, . . . 265 CHAPTER V. How little Gluck set off on an Expedition to the Golden River, and how he prospered therein ; with other matters of interest, ..... 268 Dame Wiggins of Lee, ...... 273 EAGLE'S NEST. LECTURE I. February 8, 1872. PAGE The function in Art of the faculty called by the Greeks, aoQta. ...... . 301 LECTURE II. February 10, 1872. The function in Science of the faculty called by the Greeks, ia . . . . . . . 313 LECTURE III. February 15, 1872. The Relation of Wise Art to Wise Science, . . 324 LECTURE IV. February 17, 1872. The function in Art and Science of the virtue called by the Greeks, ffaxppocrvvy} . ..... 340 LECTURE V. February, 22, 1872. The function in Art and Science of the virtue called by the Greeks, aurdptcsia ..... 348 LECTURE VI. February 24, 1872. The relation to Art of the Science of Light, PAGE • 36l LECTURE VII. February 29, 1872. The relation to Art of the Sciences of Inorganic Form 373 LECTURE VIII. March 2, 1872. The relation to Art of the Science of Organic Form, . 385 LECTURE IX. March 7, 1872. Introduction to Elementary Exercises in Physiologic Art. The Story of the Halcyon, . • • 399 LECTURE X. March 9, 1872. Introduction to Elementary Exercises in Historic Art. The Heraldic Ordinaries, ..... 4ig LIST OF ILLUSTRATIONS. THE KING OF THE GOLDEN RIVER. DESIGNED AND DRAWN ON WOOD BY RICHARD DOYLE. TAGE Southwest Wind, Esq., knocking at the Black Brothers' door, engraved by C. Thurston Thompson, Froiitispiece The Treasure Valley, engraved by C. Thurston Thomp- son, ........ Title Initial Letter, and Mountain Range, engraved by G. and E. Dalziel, . . . . . • . . 239 Southwest Wind, Esq., seated on the hob, engraved by G. and E. Dalziel, ...... 244 Southwest Wind, Esq., bowing to the Black Brothers, engraved by H. Orrin Smith, .... 246 Storm Scene, engraved by G. and E. Dalziel, . . 248 Card of Southwest Wind, Esq., engraved by H. Orrin Smith, ........ 249 Initial Letter, and Cottage in the Treasure Valley, engraved by Isabel Thompson, .... 250 The Black Brothers drinking, and Gluck working, ENGRAVED BY C. S CHELTNAM, . . . . 251 Gluck looking out at the Golden River, engraved by H. D. Linton, . . . . . . -252 The Golden Dwarf appearing to Gluck, engraved by G. and E. Dalziel, ...... 255 PAGE Gluck looking up the Chimney, engraved by H. Orrin Smith, . . . . . . . .257 The Black Brothers beating Gluck, engraved by C. S. Cheltnam, ....... 258 Hans and Schwartz fighting, engraved by H. Orrin Smith, 259 Schwartz before the Magistrate, engraved by C. S. Cheltnam, ...... 260 Hans and the Dog, engraved by H. Orrin Smith, . . 262 The Black Stone, engraved by G. and E. Dalziel, . 264 Initial Letter — Gluck releasing Schwartz, engraved by G. and E. Dalziel, . . . . . . 265 Schwartz ascending the Mountain, engraved by H. Orrin Smith, ....... 266 Initial Letter— Gluck ascending the Mountain, engraved by H. Orrin Smith, ...... 268 Priest giving Gluck Holy Water, engraved by G. and E. Dalziel, ....... 269 Gluck and the Child, engraved by C. S. Cheltnam, . 270 LIST OF PLATES. DEUCALION. PLATE FACING PAGE 1. First conditions of Accumulation and Fusion in Motionless Snow, .... Frontispiece 2. The progress of Modern Science in Glacier Survey, . 58 3. Mural Agates, ...... 72 4. Amethyst Quartz, . . . . .92 5. Structure of Lake Agate, . . . 125 6. Lateral Compression of Strata, . . . . 139 7. The Strata of Switzerland and Cumberland, . 154 8. "Development." Crocodile Latent in Toucan, . 176 9. "Development." Short Noses into Long, . . 190 10. Modes of Crystalline Increment, • . . 222 11. The Olympian Lightning, . . • • 225 DEUCALION COLLECTED STUDIES ON THE LAPSE OF WAVES AND LIFE OF STONES IETKODUCTIOK Brantwood, 13th July, 1875. I have been glancing lately at many biographies, and have been much struck by the number of deaths which occur be- tween the ages of fifty and sixty, (and, for the most part, in the earlier half of the decade,) in cases where the brain has been much used emotionally : or perhaps it would be more accurate to say, where the heart, and the faculties of percep- tion connected with it, have stimulated the brain-action. Sup- posing such excitement to be temperate, equable, and joyful, I have no doubt the tendency of it would be to prolong, rather than depress, the vital energies. But the emotions of indig- nation, grief, controversial anxiety and vanity, or hopeless, and therefore uncontending, scorn, are all of them as deadly to the body as poisonous air or polluted water ; and when I reflect how much of the active part of my past life has been spent in these states, — and that what may remain to me of life can never more be in any other, — I begin to ask myself, with somewhat pressing arithmetic, how much time is likely to be left me, at the age of fifty-six, to complete the various designs for which, until past fifty, I was merely collecting materials. Of these materials, I have now enough by me for a most interesting (in my own opinion) history of fifteenth-century Florentine art, in six octavo volumes ; an analysis of the Attic art of the fifth century b.c, in three volumes ; an exhaustive history of northern thirteenth-century art, in ten volumes ; a life of Turner, with analysis of modern landscape art, in four volumes ; a life of Walter Scott, with analysis of modern epic art, in seven volumes ; a life of Xenophon, with analysis of the general principles of Education, in ten volumes ; a commen- 6 INTRODUCTION. tary on Hesiod, with final analysis of the principles of Political Economy, in nine volumes ; and a general description of the geology and botany of the Alps, in twenty-four volumes. Of these works, though all carefully projected, and some already in progress, — yet, allowing for the duties of my Pro- fessorship, possibly continuing at Oxford, and for the increas- ing correspondence relating to Fors Clavigera, — it does not seem to me, even in my most sanguine moments, now probable that I shall live to effect such conclusion as would be satisfac- tory to me ; and I think it will therefore be only prudent, how- ever humiliating, to throw together at once, out of the heap of loose stones collected for this many-towered city which I am not able to finish, such fragments of good marble as may perchance be useful to future builders ; and to clear away, out of sight, the lime and other rubbish which I meant for mortar. And because it is needful, for my health's sake, hencefor- ward to do as far as possible what I find pleasure, or at least tranquillity, in doing, I am minded to collect first what I have done in geology and botany ; for indeed, had it not been for grave mischance in earlier life, (partly consisting in the unlucky gift, from an affectionate friend, of Rogers' poems, as related in Fors Clavigera for August of this year,) my natural dispo- sition for these sciences would certainly long ago have made me a leading member of the British Association for the Ad- vancement of Science ; or — who knows ? — even raised me to the position which it was always the summit of my earthly ambition to attain, that of President of the Geological Society. For, indeed, I began when I was only twelve years old, a 'Minera- logical Dictionary/ intended to supersede everything done by Werner and Mohs, (and written in a shorthand composed of crystallographic signs now entirely unintelligible to me,) — and year by year have endeavoured, until very lately, to keep abreast with the rising tide of geological knowledge ; some- times even, I believe, pushing my way into little creeks in ad- vance of the general wave. I am not careful to assert for my- self the petty advantage of priority in discovering what, some day or other, somebody must certainly have discovered. But INTRODUCTION. 7 X think it due to my readers, that they may receive what real good there may be in these studies with franker confidence, to tell them that the first sun-portrait ever taken of the Mat- terhorn, (and as far as I know of any Swiss mountain what- ever,) was taken by me in the year 1849 ; that the outlines, (drawn by measurement of angle,) given in 'Modern Painters' of the Cervin, and aiguilles of Chamouni, are at this day de- monstrable by photography as the trustworthiest then in ex- istence ; that I was the first to point out, in my lecture given in the Royal Institution,* the real relation of the vertical cleavages to the stratification, in the limestone ranges belong- ing to the chalk formation in Savoy ; and that my analysis of the structure of agates, ('Geological Magazine/) remains, even to the present day, the only one which has the slightest claim to accuracy of distinction, or completeness of arrangement. 1 propose therefore, if time be spared me, to collect, of these detached studies, or lectures, what seem to me deserving of preservation; together with the more carefully written chapters on geology and botany in the latter volumes of ' Modern Painters ; ' adding the memoranda I have still by me in manu- script, and such further illustrations as may occur to me on revision. Which fragmentary work, — trusting that among the flowers or stones let fall by other hands it may yet find service and life, — I have ventured to dedicate to Proserpina and Deucalion. Why not rather to Eve, or at least to one of the wives of Lamech, and to Noah? asks, perhaps, the pious modern reader. Because I think it well that the young student should first learn the myths of the betrayal and redemption, as the Spirit which moved on the face of the wide first waters, taught them to the heathen world. And because, in this power, Proser- pine and Deucalion are at least as true as Eve or Noah ; and all four together incomparably truer than the Darwinian The- ory. And, in general, the reader may take it for a first prin- ciple, both in science and literature, that the feeblest myth is * Reported in the ' Journal de Geneve/ date ascertainable, but of no consequence, 9 INTRODUCTION. better than the strongest theory : the one recording a natural impression on the imaginations of great men, and of unpre- tending multitudes ; the other, an unnatural exertion of the wits of little men, and half-wits of impertinent multitudes. It chanced, this morning, as I sat down to finish my preface, that I had, for my introductory reading, the fifth chapter of the second book of Esdras ; in which, though often read care- fully before, I had never enough noticed the curious verse, " Blood shall drop out of wood, and the stone shall give his voice, and the people shall be troubled." Of which verse, so far as I can gather the meaning from the context, and from the rest of the chapter, the intent is, that in the time spoken of by the prophet, which, if not our own, is one exactly cor- responding to it, the deadness of men to all noble things shall be so great, that the sap of trees shall be more truly blood, in God's sight, than their hearts' blood ; and the silence of men, in praise of all noble things, so great, that the stones shall cry out, in God's hearing, instead of their tongues ; and the rattling of the shingle on the beach, and the roar of the rocks driven by the torrent, be truer Te Deum than the thun- der of all their choirs. The writings of modern scientific prophets teach us to anticipate a day when even these lower voices shall be also silent ; and leaf cease to wave, and stream to murmur, in the grasp of an eternal cold. But it may be, that rather out of the mouths of babes and sucklings a better peace may be promised to the redeemed Jerusalem ; and the strewn branches, and low-laid stones, remain at rest at the gates of the city, built in unity with herself, and saying with her human voice, ' ' My King cometh." DEUOALIOK CHAPTER I. THE ALPS AND JURA. {Part of a Lecture given in the Museum of Oxford, in October^ 1874.) 1. It is often now a question with me whether the persons who appointed me to this Professorship have been disap- pointed, or pleased, by the little pains I have hitherto taken to advance the study of landscape. That it is my own favourite branch of painting seemed to me a reason for caution in press- ing it on your attention ; and the range of art-practice which I have hitherto indicated for you, seems to me more properly connected with the higher branches of philosophical inquiry native to the University. But, as the second term of my Pro- fessorship will expire next year, and as I intend what remains of it to be chiefly employed in giving some account of the art of Florence and Umbria, it seemed to me proper, before en- tering on that higher subject, to set before you some of the facts respecting the great elements of landscape, which I first stated thirty years ago ; arranging them now in such form as my farther study enables me to give them. I shall not, in- deed, be able to do this in a course of spoken lectures ; nor do I wish to do so. Much of what I desire that you .should notice is already stated, as well as I can do it- in ' Modern Painters ; • and it would be waste of time to recast it in the form of address. But I should not feel justified in merely 10 DEUCALION. reading passages of my former writings to you from this chair ; and will only ask your audience, here, of some addi- tional matters, as, for instance, to-day, of some observations I have been making recently, in order to complete the account given in ' Modern Painters/ of the structure and aspect of the higher Alps. 2. Not that their structure — (let me repeat, once more, what I am well assured you will, in spite of my frequent as- sertion, find difficult to believe,) — not that their structure is any business of yours or mine, as students of practical art. All investigations of internal anatomy, whether in plants, rocks, or animals, are hurtful to the finest sensibilities and in- stincts of form. But very few of us have any such sensibili- ties to be injured ; and that we may distinguish the excellent art which they have produced, we must, by duller processes, become cognizant of the facts. The Torso of the Vatican was not wrought by help from dissection ; yet all its supreme qualities could only be explained by an anatomical master. And these drawings of the Alps by Turner are in landscape, what the Elgin marbles or the Torso are in sculpture. There is nothing else approaching them, or of their order. Turner made them before geology existed ; but it is only by help of geology that I can prove their power. 3. I chanced, the other day, to take up a number of the 'Alpine Journal' (May, 1871,) in which there was a review by Mr. Leslie Stephen, of Mr. "Whymper's ' Scrambles among the Alps/ in which it is said that " if the Alpine Club has done nothing else, it has taught us for the first time really to see the mountains." I have not the least idea whom Mr. Stephen means by 'us / but I can assure him that mountains had been seen by several people before the nineteenth century; that both Hesiod and Pindar occasionally had eyes for Parnassus, Virgil for the Apennines, and Scott for the Grampians ; and without speaking of Turner, or of any other accomplished artist, here is a little bit of old-fashioned Swiss drawing of the two Mythens, above the central town of Switzerland,* showing a degree of affection, intelligence, and tender observation, com- * In the Educational Series of my Oxford Schools. THE ALPS AND JURA. 11 pared to which our modern enthusiasm is, at best, childish ; and commonly also as shallow as it is vulgar. 4. Believe me, gentlemen, your power of seeing mountains cannot be developed either by your vanity, your curiosity, or your love of muscular exercise. It depends on the cultivation of the instrument of sight itself, and of the soul that uses it. As soon as you can see mountains rightly, you will see hills also, and valleys, with considerable interest ; and a great many other things in Switzerland with which you are at present but poorly acquainted. The bluntness of your present capacity of ocular sensation is too surely proved by your being unable to enjoy any of the sweet lowland country, which is incom- parably more beautiful than the summits of the central range, and which is meant to detain you, also, by displaying — if you have patience to observe them — the loveliest aspects of that central range itself, in its real majesty of proportion, and mystery of power. 5. For, gentlemen, little as you may think it, you can no more see the Alps from the Col du Geant, or the top of the Matterhorn, than the pastoral scenery of Switzerland from the railroad carriage. If you want to see the skeletons of the Alps, you may go to Zermatt or Chamouni ; but if you want to see the body and soul of the Alps, you must stay awhile among the Jura, and in the Bernese plain. And, in general, the way to see mountains, is to take a knapsack and a walking- stick ; leave alpenstocks to be nourished in each other s faces, and between one another's legs, by Cook's tourists ; and try to find some companionship in yourself with yourself ; and not to be dependent for your good cheer either on the gossip of the table-d'hote, or the hail-fellow and well met, hearty though it be, of even the pleasantest of celebrated guides. 6. Whether, however, you think it necessary or not, for true sight of the Alps, to stay awhile among the Jura or in the Bernese fields, very certainly, for understanding, or ques- tioning, of the Alps, it is wholly necessary to do so. If you look back to the lecture, which I gave as the fourth of my inaugural series, on the Relation of Art to Use, you will see it stated, as a grave matter of reproach to the modern traveller, 12 DEUCALION. that, crossing the great plain of Switzerland nearly every sum* mer, he never thinks of inquiring why it is a plain, and why the mountains to the south of it are mountains. 7. For solution of which, as it appears to me, not un- natural inquiry, all of you, who have taken any interest in geology whatever, must recognize the importance of studying the calcareous ranges which form the outlying steps of the Alps on the north ; and which, in the lecture just referred to, I requested you to examine for their crag scenery, markedly developed in the Stockhorn, Pilate, and Sentis of Appenzell. The arrangements of strata in that great calcareous belt give the main clue to the mode of elevation of the central chain, the relations of the rocks over the entire breadth of North Switzerland being, roughly, as in this first section : v B C D E F Fig. 1. A. Jura limestones, moderately undulating in the successive chains of Jura. B. Sandstones of the great Swiss plain. C. Pebble breccias of the first ranges of Alpine hills. D. Chalk formations violently contorted, forming the rock scenery of which I have just spoken. E. Metamorphic rocks lifted by the central Alps. Fo Central gneissic or granitic mass, narrow in Mont Blanc, but of enormous extent southward from St. Gothard. 8. Now you may, for first grasp of our subject, imagine these several formations all fluted longitudinally, like a Gothic moulding, thus forming a series of ridges and valleys parallel to the Alps ; — such as the valley of Chamouni, the Simmen- thal, and the great vale containing the lakes of Thun and Brienz ; to which longitudinal valleys we now obtain access through gorges or defiles, for the most part cut across the THE ALPS AND JURA. 13 formations, and giving geological sections all the way from the centres of the Alps to the plain. 9. Get this first notion very simply and massively set in your thoughts. Longitudinal valleys, parallel with the beds ; more or less extended and soft in contour, and often occupied by lakes. Cross defiles like that of Lauterbrunnen, the Via Mala, and the defile of Gondo ; cut down across the beds, and traversed by torrents, but rarely occupied by lakes. The bay of Uri is the only perfect instance in Switzerland of a portion of lake in a diametrically cross valley ; the crossing arms of the lake Lucerne mark the exactly rectangular schism of the forces ; the main direction being that of the lakes of Kuss- nacht and Alpnacht, carried on through those of Sarnen and Lungern, and across the low intervening ridge of the Brunig, joining the depressions of Brienz and Thun ; of which last lake the lower reach, however, is obliquely transverse. Forty miles of the Lago Maggiore, or, including the portion of lake now filled by delta, fifty, from Baveno to Bellinzona, are in the longitudinal valley which continues to the St. Bernardino ; and the entire length of the lake of Como is the continuation of the great lateral Valtelline. 10. Now such structure of parallel valley and cross defile would be intelligible enough, if it were confined to the lateral stratified ranges. But, as you are well aware, the two most notable longitudinal valleys in the Alps are cut right along the heart of their central gneissic chain ; how much by dividing forces in the rocks themselves, and how much by the sources of the two great rivers of France and Germany, there will yet be debate among geologists for many a day to come. For us, let the facts at least be clear ; the questions definite ; but all debate declined. 11. All lakes among the Alps, except the little green pool of Lungern, and a few small tarns on the cols, are quite at the bottom of the hills. We are so accustomed to this con- dition, that we never think of it as singular. But in its un- exceptional character, it is extremely singular. How comes it to pass, think you, that through all that wilderness of mountain — raised, in the main mass of it, some six thousand 14 DEUCALION. feet above the sea, so that there is no col lower, — there is not a single hollow shut in so as to stay the streams of it ; — that no valley is ever barred across by a ridge which can keep so much as ten feet of water calm above it, — that every such ridge that once existed has been cut through, so as to let the stream escape? I put this question in passing ; we will return to it : let me first ask you to examine the broad relations of the beds that are cut through. My typical section, Fig. 1, is strin- gently simple ; it must be much enriched and modified to fit any locality ; but in the main conditions it is applicable to the entire north side of the Alps, from Annecy to St. Gall. 12. You have first — (I read from left to right, or north to south, being obliged to do so because all Studer's sections are thus taken) — this mass of yellow limestone, called of the Jura, from its development in that chain ; but forming an immense tract of the surface of France also ; and, as you well know, this our city of Oxford stands on one of its softer beds, and is chiefly built of it. We may, I think, without entering any forbidden region of theory, assume that this Jura limestone extends under the plain of Switzerland, to reappear where we again find it on the flanks of the great range ; where on the top of it the beds drawn with fine lines in my section correspond generally to the date of our English chalk, though they are far from white in the Alps. Curiously adjusted to the chalk beds, rather than superimposed, we have these notable masses of pebble breccia, w T hich bound the sandstones of the great Swiss plain. 13. I have drawn that portion of the section a little more boldly in projection, to remind you of the great Eigi prom- ontory; and of the main direction of the slope of these beds, with their backs to the Alps, and their escarpments to the plain. Both these points are of curious importance. Have you ever considered the reason of the fall of the Koss- berg, the most impressive physical catastrophe that has chanced in Europe in modern times? Few mountains in Switzerland looked safer. It was of inconsiderable height, of very moderate steepness ; but its beds lay perfectly THE ALPS AND JURA. 15 straight, and that over so large a space, that when the clay between two of them got softened by rain, one slipped off the other. Now this mathematical straightness is characteristic of these pebble beds, — not universal in them, but characterestic of them, and of them only. The lime- stones underneath are usually, as you see in this section, violently contorted ; if not contorted, they are at least so irregular in the bedding that you can't in general find a sur- face of a furlong square which will not either by its depres- sion, or projection, catch and notch into the one above it, so as to prevent its sliding. Also the limestones are continually torn, or split, across the beds. But the breccias, though in many places they suffer decomposition, are curiously free from fissures and rents. The hillside remains unshattered Fig. 2. unless it comes down in a mass. But their straight bed- ding, as compared with the twisted limestone, is the notablest point in them ; and see how very many difficulties are gath- ered in the difference. The crushed masses of limestone are supposed to have been wrinkled together by the lateral thrust of the emerging protogines ; and these pebble beds to have been raised into a gable, or broken into a series of colossal fragments set over each other like tiles, all along the south shore of the Swiss plain, by the same lateral thrust ; nay, "though we may leave in doubt," says Studer, "by what cause the folded forms of the Jura may have been pushed back, there yet remains to us, for the explanation of this gabled form of the Nagelfluh, hardly any other choice than to adopt the opinion of a lateral pressure communicated by the Alps to the tertiary bottom. We have often found in the outer limestone chains themselves clear evidence of a pressure 16 DEUCALION. going out from the inner Alps ; and the pushing of the oldei over the younger formations along the flank of the limestone hills, leaves hardly any other opinion possible." 14. But if these pebble beds have been heaved up by the same lateral thrust, how is that a force which can bend lime- stone like leather, cannot crash anywhere, these pebble beds into the least confusion ? Consider the scale on which opera- tions are carried on, and the forces of which this sentence of Studer's so serenely assumes the action. Here, A, Fig. 2, is his section of the High Sentis of Appenzell, of which the height is at least, in the parts thus bent, 6,000 feet. And here, B, Fig. 2, are some sheets of paper, crushed together by my friend Mr. Henry Woodward, from a length of four inches, into what you see ; the High Sentis, exactly resem- bles these, and seems to consist of four miles of limestone similarly crushed into one. Seems, I say, remember : I never theorize, I give you the facts only. The beds do go up and down like this : that they have been crushed together, it is Mr. Studer who says or supposes ; I can't go so far ; never- theless, I admit that he appears to be right, and I believe he is right ; only don't be positive about it, and don't debate ; but think of it, and examine. 15. Suppose, then, you have a bed of rocks, four miles long by a mile thick, to be crushed laterally into the space of a mile. It may be done, supposing the mass not to be reduci- ble in bulk, in two ways : you may either crush it up into folds, as I crush these pieces of cloth ; or you may break it into bits, and shuffle them over one another like cards. Now, Mr. Studer, and our geologists in general, believe the first of these operations to have taken place with the limestones, and the second with the breccias. They are, as I say, very proba- bly right : only just consider what is involved in the notion of shuflling up your breccias like a pack of cards, and folding up your limestones like a length of silk which a dexterous draper's shopman is persuading a young lady to put ten times as much of into her gown as is wanted for it ! Think, I say, what is involved in the notion. That you may shuffle your pebble beds, you must have them strong and well knit. Thes THE ALPS AND JURA. 17 what sort of force must you have to break and to heave them ? Do but try the force required to break so much as a Captain's biscuit by a slow push, — it is the illustration I gave long ago in 'Modern Painters/ — and then fancy the results of such fracturing power on a bed of conglomerate two thousand feet thick ! And here is indeed a very charming bookbinder's pattern, produced by my friend in crushed paper, and the length of silk produces lovely results in these arrangements a la Paul Veronese. But when you have the cliffs of the Dia- blerets, or the Dent du Midi of Bex, to deal with ; and have to fold them up similarly, do you mean to fold your two-thou- sand-fee t-thick Jura limestone in a brittle state, or a ductile one ? If brittle, won't it smash ? If ductile, won't it squeeze ? Yet your whole mountain theory proceeds on the assumption that it has neither broken nor been compressed, — more than the folds of silk or coils of paper. 16. You most of you have been upon the lake of Thun. You have been at least carried up and down it in a steamer ; you smoked over it meanwhile, and countenanced the French- men and Germans who were spitting into it. The steamer carried you all the length of it in half an hour ; you looked at the Jungfrau and Blumlis Alp, probably, for five minutes, if it was a fine day ; then took to your papers, and read the last news of the Tichborne case ; then you lounged about, — thought it a nuisance that the steamer couldn't take you up in twenty minutes, instead of half an hour ; then you got into a row about your luggage at Neuhaus ; and all that you recollect afterwards is that lunch where you met the so-and- sos at Interlaken. 17. Well, we used to do it differently in old times. Look here ; — this * is the quay at Neuhaus, with its then travelling arrangements. A flat-bottomed boat, little better than a punt ; — a fat Swiss girl with her schatz, or her father, to row it ; oars made of a board tied to a pole : and so one paddled along over the clear water, in and out among the bays and villages, for half a day of pleasant life. And one knew some* * Turner's first study of the Lake of Thun, 1803. 18 DEUCALION. thing about the lake, ever after, if one had a head with eye* in it. It is just possible, however, that some of you also who have been learning to see the Alps in your new fashion, may re- member that the north side of the lake of Thun consists, first, next Thun, of a series of low green hills, with brown cliffs here and there among the pines ; and that above them, just after passing Oberhofen, rears up suddenly a great precipice, with its flank to the lake, and the winding wall of it prolonged upwards, far to the north, losing itself, if the day is fine, in faint tawny crests of rock among the distant blue ; and if stormy, in wreaths of more than commonly torn and fantastic cloud. 18. To form the top of that peak on the north side of the lake of Thun, you have to imagine forces which have taken — say, the whole of the North Foreland, with Dover castle on it, and have folded it upside-down on the top of the parade at Margate, — then swept up Whitstable oyster-beds, and put them on the bottom of Dover cliffs turned topsy-turvy, — and then wrung the whole round like a wet towel, till it is as close and hard as it will knit ; — such is the beginning of the opera- tions which have produced the lateral masses of the higher Alps. 19. Next to these, you have the great sculptural force, which gave them, approximately, their present forms, — which let out all the lake waters above a certain level, — -which cut the gorge of the Devil's Bridge — of the Via Mala — of Gondo — of the valley of Cluse ; — which let out the Khone at St. Maurice, the Ticino at Faido, and shaped all the vast ravines which make the flanks of the great mountains awful. 20. Then, finally, you have the rain, torrent, and glacier of human days. Of whose action, briefly, this is the sum. Over all the high surfaces, disintegration — melting away — diffusion — loss of height and terror. In the ravines, — whether occupied by torrent or glacier,— gradual incumbrance by materials falling from above ; chok- ing up of their beds by silt — by moraine — by continual ad THE ALPS AND JURA. 19 vances of washed slopes on their flanks : here and there, only, exceptional conditions occur in which a river is still continu- ing feebly the ancient cleaving action, and cutting its ravine deeper, or cutting it back. Fix this idea thoroughly in your minds. Since the valley of Lauterbrunnen existed for human eyes, — or its pastures for the food of flocks, — it has not been cut deeper, but par- tially filled up by its torrents. The town of Interlachen stands where there was once lake, — and the long slopes of grassy sward on the north of it, stand where once was preci- pice. Slowly — almost with infinite slowness, — the declining and encumbering action takes place ; but incessantly, and, — as far as our experience reaches, — irredeemably. 21. Now I have touched in this lecture briefly on the theories respecting the elevation of the Alps, because I want to show you how uncertain and unsatisfactory they still remain. For our own work, we must waste no time on them ; we must begin where all theory ceases ; and where observation becomes possible, — that is to say, with the forms which the Alps have actually retained while men have dwelt among them, and on which we can trace the progress, or the power, of existing conditions of minor change. Such change has lately affected, and with grievous deterioration, the outline of the highest mountain of Europe, with that of its beautiful supporting buttresses, — the aiguille de Bionassay. I do not care, and I want you not to care, — how crest or aiguille was lifted, or where its materials came from, or how much bigger it was once. I do care that you should know, and I will endeavour in these following pages securely to show you, in what strength and beauty of form it has actually stood since man was man, and what subtle modifications of aspect, or majesties of con- tour, it still suffers from the rains that beat upon it, or owes to the snows that rest. 20 DEUCALION. CHAPTER II. THE THREE 2E R A S # (Part of a Lecture given at the London Institution in March 1875, with added pieces from Lectures in Oxford.) 1. We are now, so many of us, some restlessly and some wisely, in the habit of spending our evenings abroad, that I do not know if any book exists to occupy the jDlace of one classical in my early clays, called 'Evenings at Home.' It contained, among many w T ell-written lessons, one, under the title of 'Eyes and No Eyes,' which some of my older hearers may remember, and which I should myself be sorry to forget. For if such a book were to be written in these days, I suppose the title and the moral of the story would both be changed ; and, instead of 6 Eyes and No Eyes/ the tale would be called * Microscopes and No Microscopes.' Fori observe that the prevailing habit of learned men is now to take interest only in objects which . cannot be seen without the aid of instru- ments ; and I believe many of my learned friends, if they were permitted to make themselves, to their own liking, in- stead of suffering the slow process of selective development, would give themselves heads like wasps', with three micro- scopic eyes in the middle of their foreheads, and two ears at the ends of their antennae. 2. It is the fashion, in modern days, to say that Pope was no poet. Probably our schoolboys also, think Horace none. They have each, nevertheless, built for themselves a monu- ment of enduring wisdom ; and all the temptations and errors of our own day, in the narrow sphere of lenticular curiosity, were anticipated by Pope, and rebuked, in one couplet : " Why has not man a microscopic eye ? For this plain reason,-— Man is not a fly." While the nobler following lines, il Say, what avail, were finer optics given To inspect a mite, not comprehend the heaven ? 17 THE THREE ^JRAS. 21 only fall short of the truth of our present clulness, in that wo inspect heaven itself, without understanding it. 3. In old times, then, it was not thought necessary for human creatures to know either the infinitely little, or the infinitely distant ; nor either to see, or feel, by artificial help, Old English people used to say they perceived things with their five — or it may be, in a hurry, they would say, their seven, senses ; and that word ' sense ' became, and for ever must remain, classical English, derived from classical Latin, in both languages signifying, not only the bodily sense, but the moral one. If a man heard, saw, and tasted rightly, we used to say he had his bodily senses perfect. If he judged, wished, and felt rightly, we used to say he had his moral senses perfect, or was a man £ in his senses/ And we were then able to speak precise truth respecting both matter and morality ; and if we heard any one saying clearly absurd things, — as, for instance, that human creatures were automata, ■ — we used to say they were out of their 6 senses/ and were talking non- c sense/ "Whereas, in modern days, by substituting analysis for sense in morals, and chemistry for sense in matter, we have literally blinded ourselves to the essential qualities of both matter and morals ; and are entirely incapable of understanding what is meant by the description given us, in a book we once honoured, of men who " by reason of use, have their senses exercised to discern both good and evil." 4. And still, with increasingly evil results to all of us, the separation is every day widening between the man of science and the artist — in that, whether painter, sculptor, or musician, the latter is pre-eminently a person who sees with his Eyes, hears with his Ears, and labours with his Body, as God constructed them ; and who, in using instruments, limits him- self to those which convey or communicate his human power, while he rejects all that increase it. Titian would refuse to quicken his touch by electricity ; and Michael Angelo to sub- stitute a steam hammer for his mallet. Such men not only do not desire, they imperatively and scornfully refuse, either the force 3 or the information, which are beyond the scope of the 22 DEUCALION. flesh and the senses of humanity. And it is at once the wis< dom, the honour, and the peace, of the Masters both of paint- ing and literature, that they rejoice in the strength, and rest in the knowledge, which are granted to active and disciplined life ; and are more and more sure, every day, of the wisdom of the Maker in setting such measure to their being ; and more and more satisfied, in their sight and their audit of Nature, that " the hearing ear, and the seeing eye, — the Lord hath made even both of them." 5. This evening, therefore, I venture to address you speak- ing limitedly as an artist ; but, therefore, I think, with a defi- nite advantage in having been trained to the use of my eyes and senses, as my chief means of observation : and I shall try to show you things which w T ith your own eyes you may any day see, and with your own common sense, if it please you to trust it, account for. Things wdiich you may see, I repeat ; not which you might perhaps have seen, if you had been born when you were not born ; nor which you might perhaps in future see, if you were alive when you will be dead. But what, in the span of earth, and space of time, allotted to you, may be seen with your hu- man eyes, if you learn to use them. And this limitation has, with respect to our present subject, a particular significance, which I must explain to you before entering on the main matter of it. G. No one more honours the past labour — no one more re- grets the present rest — of the late Sir Charles Lyell, than his scholar, who speaks to you. But his great theorem of the constancy and power of existing phenomena was only in meas- ure proved, — in a larger measure disputable ; and in the broad- est bearings of it, entirely false. Pardon me if I spend no time in qualifications, references, or apologies, but state clearly to you what Sir Charles LyelFs work itself enables us now to perceive of the truth. There are, broadly, three great demon- strable periods of the Earth's history. That in which it was crystallized ; that in which it was sculptured ; and that in which it is now being unsculptured, or deformed. These three periods interlace with each other, and gradate into each other THE THREE JERAS. 23 ^-as the periods of human life do. Something dies in the child on the day that it is born, — something is born in the man on the day that he dies : nevertheless, his life is broadly divided into youth, strength, and decrepitude. In such clear sense, the Earth has its three ages : of their length we know as yet nothing, except that it has been greater than any man had imagined. 7. (THE FIEST PERIOD.) — But there was a period, or a succession of periods, during which the rocks which are now hard were soft ; and in which, out of entirely different posi- tions, and under entirely different conditions from any now existing or describable, the masses, of which the mountains you now see are made, were lifted, and hardened, in the posi- tions they now occupy, though in what forms we can now no more guess than we can the original outline of the block from the existing statue. 8. (THE SECOND PERIOD. ) — Then, out of those raised masses, more or less in lines compliant with their crystalline structure, the mountains we now r see were hewn, or worn, dur- ing the second period, by forces for the most part differing both in mode and violence from any now in operation, but the result of which was to bring the surface of the earth into a form approximately that which it has possessed as far as the records of human history extend. — The Ararat of Moses's time, the Olympus and Ida of Homer's, are practically the same mountains now, that they were then. 9. (THE THIRD PERIOD.)— Not, however, without some calculable, though superficial, change, and that change, one of steady degradation. For in the third, or historical period, the valleys excavated in the second period are being filled up, and the mountains, hewn in the second period, worn or ruined down. In the second sera the valley of the Rhone was being cut deeper every day ; now it is every day being filled up with gravel. In the second sera, the scars of Derbyshire and York- shire were cut white and steep ; now they are being darkened by vegetation, and crumbled by frost. You cannot, I repeat, separate the periods with precision ; but, in their characters, they are as distinct as youth from age. 24 DEUCALION. 10. The features of mountain form, to which during my own life I have exclusively directed my study, and which I en- deavour to bring before the notice of my pupils in Oxford, are exclusively those produced by existing forces, on mount- ains whose form and substance have not been materially changed during the historical period. For familiar example, take the rocks of Edinburgh castle, and Salisbury Craig. Of course we know that they are both basaltic, and must once have been hot. But I do not myself care in the least what happened to them till they were cold.* They have both been cold at least longer than young Harry Percy's spur ; and, since they were last brought out of the oven, in the shape which, approximately, they still retain, with a hollow beneath one of them, which, for aught I know, or care, may have been cut by a glacier out of white-hot lava, but * More curious persons, who are interested in their earlier condition, will find a valuable paper by Mr. J. W. Judd, in the quarterly ' Journal of the Geological Society,' May, 1875 ; very successfully, it seems tome, demolishing all former theories on the subject, which the author thus sums, at p. 135. "The series of events which we are thus required to believe took place in this district is therefore as follows : — A. At the point where the Arthur's Seat group of hills now rises, a series of volcanic eruptions occurred during the Lower Calciferous Sand- stone period, commencing with the emission of basaltic lavas, and end- ing with that of porphyrites. B. An interval of such enormous duration supervened as to admit of— a. The deposition of at least 3,000 feet of Carboniferous strata. b. The bending of all the rocks of the district into a series of great anticlinal and synclinal folds. c. The removal of every vestige of the 3,000 feet of strata by de- nudation. C. The outburst, after this vast interval, of a second series of volcanic eruptions upon the identical site of the former ones, presenting in its succession of events precisely the same sequence, and resulting in the production of rocks of totally itndistinguishable character. Are we not entitled to regard the demand for the admission of such a series of extraordinary accidents as evidence of the antecedent improb- ability of the theory ? And when we find that all attempts to suggest a period for the supposed second series of outburstshave successively failed, do not the difficulties of the li vpothesir; appear to be overwhelming ? " THE THREE uERAS. assuredly at last got itself filled with pure, sweet, cold water, and called, in Lowland Scotch, the ' Nor' Loch ; ' — since the time, I say, when the basalt, above, became hard, and the lake beneath, drinkable, I am desirous to examine with you what effect the winter's frost and summer's rain have had on the crags and their hollows ; how far the £ Kittle nine steps ' under the castle- walls, or the firm slope and cresting precipice above the dark ghost of Holyrood, are enduring or departing forms ; and how long, unless the young engineers of New Edinburgh blast the incumbrance away, the departing mists of dawn may each day reveal the form, unchanged, of the Eock which was the strength of their Fathers. 11. Unchanged, or so softly modified that eye can scarcely Irace, or memory measure, the work of time. Have you ever practically endeavoured to estimate the alterations of form in any hard rocks known to you, during the course of }^our own lives ? You have all heard, a thousand times over, the com- mon statements of the school of Sir Charles Lyell. You know all about alluviums and gravels ; and what torrents do, and what rivers do, and what ocean currents do ; and when you see a muddy stream coming down in a flood, or even the yel- low gutter more than usually rampant by the roadside in a thunder shower, you think, of course, that all the forms of the Alps are to be accounted for by aqueous erosion, and that it's a wonder any Alps are still left. Well — any of you who have fished the pools of Scottish or a Welsh stream, — have you ever thought of asking an old keeper how much deeper they had got to be, while his hairs were silvering ? Do you suppose he wouldn't laugh in your face ? There are some sitting here, I think, who must have them- selves fished, for more than one summer, years ago, in Dove or Derwent, — in Tweed or Teviot. Can any of you tell me a single pool, even in the limestone or sandstone, where you could spear a salmon then, and can't reach one now — (providing always the wretches of manufacturers have left you one to be speared, or water that you can see through) ? Do you know so much as a single rivulet of clear water which has cut away a visible half-inch of Highland rock, to your own knowledge, DEUCALION. in your own day ? You have seen whole banks, whole fields washed away ; and the rocks exposed beneath ? Yes, of course you have ; and so have L The rains wash the loose earth about everywhere, in any masses that they chance to catch — loose earth, or loose rock. But yonder little rifted well in the native whinstone by the sheepfold, — did the gray shepherd not put his lips to the same ledge of it, to drink — when he and you were boys together ? 12. ' But Niagara, and the Delta of the Ganges — and — all the rest of it ? ' Well, of course a monstrous mass of conti- nental drainage, like Niagara, trill wash down a piece of crag once in fifty years, (but only that, if it's rotten below ;) and tropical rains will eat the end off a bank of slime and alliga- tors, — and spread it out lower down. But does any Scotchman know a change in the Fall of Fyers ? — any Yorkshireman in the Force of Tees ? Except of choking up, it may be — not of cutting down. It is true, at the side of every stream you see the places in the rocks hollowed by the eddies. I suppose the eddies go on at their own rate. But I simply ask, Has any human being ever known a stream, in hard rock, cut its bed an inch deeper down at a given spot ? 13. I can look back, myself, now pretty nearly, I am sorry to say, half a century, and recognize no change whatever in any of my old dabbling-places ; but that some stones are mossier, and the streams usually dirtier, — the Derwent above Keswick, for example. 1 But denudation does go on, somehow : one sees the whole glen is shaped by it ? ' Yes, but not by the stream. The stream only sweeps down the loose stones ; frost and chemical change are the powers that loosen them. I have indeed not known one of my dabbling-places changed in fifty years. But I have known the eboulement under the Kochers des Fyz, which filled the Lac de Chede ; I passed through the valley of Cluse a night after some two or three thousand tons of limestone came off the cliffs of Maglans — burying the road and field be- side it. I have seen half a village buried by a landslip, and its people killed, under Monte St. Angelo, above Amalfi. I THE THREE JERAS. 21 have seen the lower lake of Llanberis destroyed, merely by artificial slate quarries ; and the Waterhead of Coniston seri- ously diminished in purity and healthy flow of current by the debris of its copper mines. These are all cases, you will ob- serve, of degradation ; diminishing majesty in the mountain, and diminishing depth in the valley, or pools of its waters. I cannot name a single spot in which, during my lifetime spent among the mountains, I have seen a peak made grander, a watercourse cut deeper, or a mountain pool made larger and purer. 14. I am almost surprised, myself, as I write these words, at the strength which, on reflection, I am able to give to my assertion. For, even till I began to write these very pages, and was forced to collect my thoughts, I remained under the easily adopted impression, that, at least among soft earthy eminences, the rivers were still cutting out their beds. And it is not so at all. There are indeed banks here and there which they visibly remove ; but whatever they sweep down from one side, they sweep up on the other, and extend a promontory of land for every shelf they undermine : and as for those radiating fibrous valleys in the Apennines, and such other hills, which look symmetrically shaped by streams, — they are not lines of trench from below, but lines of wash or slip from above : they are the natural wear and tear of the surface, directed indeed in easiest descent by the bias of the stream, but not dragged down by its grasp. In every one of those ravines the water is being choked up to a higher level ; it is not gnawing down to a lower. So that, I repeat, ear- nestly, their chasms being choked below, and their precipices shattered above, all mountain forms are suffering a deliques- cent and corroding change, — not a sculpturesque or anato- mizing change. All character is being gradually effaced ; all crooked places made straight, — all rough places, plain ; and among these various agencies, not of erosion, but co?Tosion, none are so distinct as that of the glacier, in filling up, not cutting deeper, the channel it fills ; and in rounding and smoothing, but never sculpturing, the rocks over which it passes. 28 DEUCALION-. In this fragmentary collection of former work, now patched and darned into serviceable ness, I cannot finish my chapters with the ornamental fringes I used to twine for them ; nor even say, by any means, all I have in my mind on the matters they treat of : in the present case, however, the reader will find an elucidatory postscript added at the close of the fourth chapter, which he had perhaps better glance over before be- ginning the third. CHAPTER HI. OF ICE-CREAM. (Continuation of Lecture delivered at London Institution, with added Illustrations from Lectures at Oxford.) 1. The statement at the close of the last chapter, doubtless surprising and incredible to many of my readers, must, be- fore I reinforce it, be explained as referring only to glaciers visible, at this day, in temperate regions. For of formerly deep and continuous tropical ice, or of existing Arctic ice, and their movements, or powers, I know, and therefore say, nothing.* But of the visible glaciers couched upon the visi- * The following passage, quoted in the 1 Geological Magazine ' for June of this year, by Mr. Clifton "Ward, of Keswick, from a letter of Professor Sedgwick's, dated May 24th, 1842, is of extreme value ; and Mr. Ward s following comments are most reasonable and just: — l *No one will, I trust, be so bold as to affirm that an uninterrupted glacier could ever have extended from Shap Fells to the coast of Holder- ness, and borne along the blocks of granite through the whole distance, without any help from the floating power of water. The supposition involves difficulties tenfold greater than are implied in the phenomenon it pretends to account for. The glaciers descending through the val~ leys of the higher Alps have an enormous transporting power: but there is no such power in a great sheet of ice expanded over a country with- out mountains, and at a nearly dead level. The difficulties involved in the theories of Messrs. Croll, Belt, Good- child, and others of the same extreme school, certainly press upon me — and I think I may say abo upon others of my colleagues — increas- ingly, as the country becomes more and more lain i liar in its features. OF ICE- CREAM, 29 ble Alps, two great facts are very clearly ascertainable, which, in my lecture at the London Institution, I asserted in their simplicity, as follows : — % The first great fact to be recognized concerning them is that they are Fluid bodies. Sluggishly fluid, indeed, but definitely and completely so ; and therefore, they do not scramble down, nor tumble down, nor crawl down, nor slip down ; but flow down. They do not move like leeches, nor like caterpillars, nor like stones, but like, what they are made of, water. That is the main fact in their state, and progress, on which all their great phenomena depend. Fact first discovered and proved by Professor James Forbes, of Edinburgh, in the year 1842, to the astonishment of all the glacier theorists of his time ; — fact strenuously denied, disguised, or confusedly and partially apprehended, by all of the glacier theorists of subsequent times, down to our ow r n day ; else there had been no need for me to tell it you again to-night. 3. The second fact of which I have to assure you is partly, I believe, new to geologists, and therefore may be of some farther interest to you because of its novelty, though I do not myself care a grain of moraine-dust for the newness of things; but rather for their oldness ; and w r onder more willingly at It is indeed a most startling thought, as one stands upon the eastern borders of the Lake-mountains, to fancy the ice from the Scotch hills stalking boldly across the Sol way, marching steadily up the Eden Val- ley, and persuading some of the ice from Shap to join it on an excur- sion over Stainmoor, and bring its boulders with it. The outlying northern parts of the Lake-district, and the flat country beyond, have indeed been ravished in many a raid by our Scotch neigh- bours, but it is a question whether, in glacial times, the Cumbrian mountains and Pennine chain had not strength in their protruding icy arms to keep at a distance the ice proceeding from the district of the southern uplands, the mountains of which are not superior in elevation. Let us hope that the careful geological observations which will doubt- less be made in the forthcoming scientific Arctic Expedition will throw much new light on our past glacial period. J. Clifton Ward Keswick, April 26*7*, 1875. so DEUCALION. what my father and grandfather thought wonderful, (as, for instance, that the sun should rise, or a seed grow,) than at any newly-discovered marvel. Nor do I know, any more than I care, whether this that I have to tell you be new or not ; but I did not absolutely know it myself, until lately ; for though I had ventured with some boldness to assert it as a consequence of other facts, I had never been under the bot- tom of a glacier to look. But, last summer, I was able to cross the dry bed of a glacier, which I had seen flowing, two hundred feet deep, over the same spot, forty years ago. And there I saw, what before I had suspected, that modern gla- ciers, like modern rivers, were not cutting their beds deeper, but filling them up. These, then, are the two facts I wish to lay distinctly before you this evening, — first that glaciers are fluent ; and, secondly, that they are filling up their beds, not cutting them deeper. 4. (I.) Glaciers are fluent; slowly, like lava, but distinct]y. And now I must ask you not to disturb yourselves, as I speak, with bye-thoughts about ' the theory of regulation.' It is very interesting to know that if you put two pieces of ice together, they will stick together ; let good Professor Faraday have all the credit of showing us that ; and the human race in general, the discredit of not having known so much as that, about the substance they have skated upon, dropped through, and eat any quantity of tons of — these two or three thousand years. It was left, nevertheless, for Mr. Faraday to show them that two pieces of ice will stick together when they touch — as two pieces of hot glass will. But the capacity of ice for sticking together no more accounts for the making of a glacier,, than the capacity of glass for sticking together accounts for the making of a bottle. The mysteries of crystalline vitrifica- tion, indeed, present endless entertainment to the scientific in- quirer ; but by no theory of vitrification can he explain to us how the bottle was made narrow at the neck, or dishonestly vacant at the bottom. Those conditions of it are to be ex- plained only by the study of the centrifugal and moral powers to which it has been submitted. OF ICE-CREAM. 31 5. In like manner, I do not doubt but that wonderful phe- nomena of congelation, regelation, degelation, and gelation pure without preposition, take place whenever a schoolboy makes a snowball ; and that miraculously rapid changes in the structure and temperature of the particles accompany the experiment of producing a star with it on an old gentleman's back. But the principal conditions of either operation are still entirely dynamic. To make your snowball hard, you must squeeze it hard ; and its expansion on the recipient sur- face is owing to a lateral diversion of the impelling forces, and not to its regelatic properties. 6. Our first business, then, in studying a glacier, is to con- sider the mode of its original deposition, and the large forces of pressure and fusion brought to bear on it, with their necessary consequences on such a substance as we practicahy know snow to be, — a powder, ductile by wind, compressible by weight ; diminishing by thaw, and hardening by time and frost ; a thing which sticks to rough ground, and slips on smooth ; which clings to the branch of a tree, and slides on a slated roof. 7. Let us suppose, then, to begin with, a volcanic cone in which the crater has been filled, and the temperature cooled, and which is now exposed to its first season of glacial agen- cies. Then let P]ate 1, Fig. 1, represent this mountain, with part of the plans at its foot under an equally distributed depth of a first winter's snow, and place the level of perpetual snow at any point you like — for simplicity's sake, I put it half- way up the cone. Below this snow-line, all snow disappears in summer ; but above it, the higher we ascend, the more of course we find remaining. It is quite wonderful how few feet in elevation make observable difference in the quantity of snow that will lie. This last winter, in crossing the moors of the peak of Derbyshire, I found, on the higher masses of them, that ascent certainly not greater than that at Harrow from the bottom of the hill to the school-house, made all the difference between easy and difficult travelling, by the change in depth of snow. 8. At the close of the summer, we have then the remnant 32 DEUCALION. represented in Fig. 2, on which the snows of the ensuing winter take the form in Fig. 3 ; and from this greater heap we shall have remaining a greater remnant, which, supposing no wind or other disturbing force modified its form, would appear as at Fig. 4 ; and, under such necessary modification, together with its own deliquescence, would actually take some such figure as that shown at Fig. 5. Now, what is there to hinder the continuance of accumula- tion ? If we cover this heap with another layer of winters snow (Fig. 6), we see at once that the ultimate condition would be, unless somehow prevented, one of enormous mass, superincumbent on the peak — like a colossal haystack, and extending far down its sides below the level of the snow -line. You are, however, doubtless well aware that no such accu- mulation as this ever does take place on a mountain-top. 9. So far from it, the eternal snows do not so much as fill the basins between mountain-tops ; but, even in these hollows, form depressed sheets at the bottom of them. The difference between the actual aspect of the Alps, and that which they would present if no arrest of the increasing accumulation on them took place, may be shown before you with the greatest ease ; and in doing so I have, in all humility, to correct a grave error of my own, which, strangely enough, has remained undetected, or at least unaccused, in spite of all the animos- ity provoked by my earlier writings. 10. When I wrote the first volume of 'Modern Painters,' scarcely any single fact was rightly known by anybody, about either the snow or ice of the Alps. Chiefly the snows had been neglected : very few eyes had ever seen the higher snows near ; no foot had trodden the greater number of Alpine summits ; and I had to glean what I needed for my pictorial purposes as best I could, — and my best in this case was a blunder. The thing that struck me most, when I saw the Alps myself, was the enormous accumulation of snow on them ; and the way it clung to their steep sides. Well, I said to my- self, ' of course it must be as thick as it can stand ; because, as there is an excess which doesn't melt, it would go on build- ing itself up like the Tower of Babel, unless it tumbled off OF ICE-CREAM. 33 There must be always, at the end of winter, as much snow on every high summit as it can carry.' There must, I said. That is the mathematical method of science as opposed to the artistic. Thinking of a thing, and demonstrating, — instead of looking at it. Very fine, and very sure, if you happen to have before you all the elements of thought ; but always very dangerously inferior to the unpre- tending method of sight — for people who have eyes, and can use them. If I had only looked at the snow carefully, I should have seen that it wasn't anywhere as thick as it could stand or lie — or, at least, as a hard substance, though deposited in powder, could stand. And then I should have asked myself, with legitimate rationalism, why it didn't ; and if I had but asked — Well, it's no matter what perhaps might have hap- pened if I had. I never did. 11. Let me now show you, practically, how great the error was. Here is a little model of the upper summits of the Ber- nese range. I shake over them as much flour as they will carry ; now I brush it out of the valleys, to represent the melting. Then you see what is left stands in these domes and ridges, representing a mass of snow about six miles deep. That is what the range would be like, however, if the snow stood up as the flour does ; and snow is at least, you will admit, as adhesive as flour. 12. But, you will say, the scale is so different, you can't reason from the thing on that scale. A most true objection. You cannot ; and therefore I beg you, in like manner, not to suppose that Professor Tyndall's experiments on " a straight prism of ice, four inches long, an inch wide, and a little more than an inch in depth," * are conclusive as to the modes of glacier motion. In what respect then, we have to ask, would the difference in scale modify the result of the experiment made here on the table, supposing this model was the Jungfrau itself, and the flour supplied by a Cyclopean miller and his men ? 13. In the first place, the lower beds of a mass six miles * * Glaciers of the Alps,' p. 348. DEUCALION. deep would be much consolidated by pressure. But would they be only consolidated ? Would they be in nowise squeezed out at the sides ? The answer depends of course on the nature of flour, and on its conditions of dryness. And you must feel in a mo- ment that, to know what an Alpine range would look like,' heaped with any substance whatever, as high as the sub- stance would stand — you must first ascertain how high the given substance will stand — on level ground. You might, perhaps heap your Alp high with wheat, — not so high with sand, — nothing like so high with dough ; and a very thin coating indeed would be the utmost possible result of any quantity whatever of showers of manna, if it had the consist- ence, as well as the taste, of wafers made with honey. 14. It is evident, then, that our first of inquiries bearing on the matter before us, must be, How high will snow stand on level ground, in a block or column ? Suppose you were to plank in a square space, securely — twenty feet high — thirty — fifty ; and to fill it with dry snow. How high could you get your pillar to stand, when you took away the wooden walls ? and when you reached your limit, or approached it, whafc would happen ? Three more questions instantly propose themselves ; namely, What happens to snow under given pressure ? will it under some degrees of pressure change into anything else than snow? and what length of time will it take to effect the change ? Hitherto, we have spoken of snow as dry only, and there- fore as solid substance, permanent in quantity and quality. You know that it very often is not dry ; and that, on the Alps, in vast masses, it is throughout great part of the year thawing, and therefore diminishing in quantity. It matters not the least, to our general inquiry, how much of it is wet, or thawing, or at what times. I merely at present have to introduce these two conditions as elements in the business. It is not dry snow always, but often soppy snow — snow and water, — that you have to squeeze. And it is not freezing snow always, but very often thawing snow. OF ICE-CREAM. 35 — diminishing therefore in bulk every instant, — that you have to squeeze. It does not matter, I repeat, to our immediate purpose, when, or how far, these other conditions enter our ground ; but it is best, I think, to put the dots on the is as we go along. You have heard it stated, hinted, suggested, im- plied, or whatever else you like to call it, again and again, by the modern school of glacialists, that the discoveries of James Forbes were anticipated by Rendu. 15. I have myself more respect for Rendu than any modern glacialist has. He was a man of de Saussure's temper, and of more than de Saussure's intelligence ; and if he hadn't had the misfortune to be a bishop, would very certainly have left James Forbes's work a great deal more than cut out for him ; — stitched — and pretty tightly — in most of the seams. But he was a bishop ; and could only examine the glaciers to an ejDisco- pic extent ; and guess, the best he could, after that. His guesses are nearly always splendid ; but he must needs some- times reason as well as guess ; and he reasons himself with beautiful plausibility, ingenuity, and learning, up to the con- clusion — which he announces as positive — that it always freezes on the Alps, even in summer. James Forbes was the first who ascertained the fallacy of this episcopal- position ; and who announced — to our no small astonishment — that it always thawed on the Alps, even in winter. 16. Not superficially of course, nor in all places. But in- ternally, and in a great many places. And you will find it is an ascertained fact — the first great one of which we owe the discovery to him — that all the year round, you must reason on the masses of aqueous deposit on the Alps as, practically, in a state of squash. Not freezing ice or snow, nor dry ice or snow, but in many places saturated with, — everywhere affected by, — moisture ; and always subject, in enormous masses, to the conditions of change which affect ice or snow at the freez- ing-point, and not below it. Even James Forbes himself scarcely, I think, felt enough the importance of this element of his own discoveries, in all calculations of glacier motion. He sometimes speaks of his glacier a little too simply as if it 36 DEUCALION, were a stream of undiminishing substance, as of treacle or tar, moving under the action of gravity only ; and scarcely enough recognizes the influence of the subsiding languor of its faint- ing mass, as a constant source of motion ; though nothing can be more accurate than his actual account of its results on the surface of the Mer de Glace, in his fourth letter to Professor Jameson. 17. Let me drive the notion well home in your own minds, therefore, before going farther. You may permanently secure it, by an experiment easily made by each one of you for your- selves this evening, and that also on the minute and easily tenable scale which is so approved at the Eoyal Institution ; for in this particular case the material conditions may indeed all be represented in very small compass. Pour a little hot water on a lump of sugar in your teaspoon. You will imme- diately see the mass thaw, and subside by a series of, in minia- ture, magnificent and appalling catastrophes, into a miniature glacier, which you can pour over the edge of your teaspoon into your saucer ; and if you will then add a little of the brown sugar of our modern commerce — of a slightly sandy character, — you may watch the rate of the flinty erosion upon the soft silver of the teaspoon at your ease, and with Professor Earn- say 's help, calculate the period of time necessary to wear a hole through the bottom of it. I think it would be only tiresome to you if I carried the in- quiry farther by progressive analysis. You will, I believe, permit, or even wish me, rather to state summarily what the facts are : — their proof, and the process of their discovery, you will find incontrovertible and finally given in this volume, classical, and immortal in scientific literature — which, twenty- five years ago, my good master Dr. Buckland ordered me, in his lecture-room at the Ashmolean, to get, — as closing all question respecting the nature and cause of glacier movement, — James Forbes's ' Travels in the Alps.' 18. The entire mass of snow and glacier, (the one passing gradually and by infinite modes of transition into the other, over the whole surface of the Alps,) is one great accumulation of ice-cream, poured upon the tops, and flowing to the bot- OF ICE- CREAM. 37 fcoms, of the mountains, under precisely the same special con- dition of gravity and coherence as the melted sugar poured on the top of a bride-cake ; but on a scale which induces forms and accidents of course peculiar to frozen water, as distin- guished from frozen syrup, and to the scale of Mont Blanc and the Jungfrau, as compared to that of a bride-cake. Instead ©f an inch thick, the ice-cream of the Alps will stand two hun- dred feet thick, — no thicker, anywhere, if it can run off; but will lie in the hollows like lakes, and clot and cling about the less abrupt slopes in festooned wreaths of rich mass and sweep- ing flow, breaking away, where the steepness becomes intolera- ble, into crisp precipices and glittering cliffs. 19. Yet never for an instant motionless — never for an instant without internal change, through all the gigantic mass, of the relations to each other of every crystal grain. That one which you break now from its wave-edge, and which melts in your hand, has had no rest, day nor night, since it faltered down from heaven when you were a babe at the breast ; and the white cloud that scarcely veils yonder summit — seven-colored in the morning sunshine — has strewed it with pearly hoar- frost, which will be on this spot, trodden by the feet of others, in the day when you also will be trodden under feet of men, in your grave. 20. Of the infinite subtlety, the exquisite constancy of this fluid motion, it is nearly impossible to form an idea in the least distinct. We hear that the ice advances two feet in the clay ; and wonder how such a thing can be possible, unless the mass crushed and ground down everything before it. But think a little. Two feet in the day is a foot in twelve hours, ■ — only an inch in an hour, (or say a little more in the daytime, as less in the night,) — and that is maximum motion in mid- glacier. If your Geneva watch is an inch across, it is three inches round, and the minute-hand of it moves three times faster than the fastest ice. Fancy the motion of that hand so slow that it must take three- hours to get round the little dial. Between the shores of this vast gulf of hills, the long wave of hastening ice only keeps pace with that lingering arrow, in its central crest ; and that invisible motion fades away upwards 38 DEUCALION. through forty years of slackening stream, to the pure light of dawn on yonder stainless summit, on which this morning's snow lies — motionless. 21. And yet, slow as it is, this infinitesimal rate of current is enough to drain the vastest gorges of the Alps of their snow, as clearly as the sluice of a canal-gate empties a lock. The mountain basin included between the Aiguille Verte, the Grandes Jorasses, and the Mont Blanc, has an area of about thirty square miles, and only one outlet, little more than a quarter of a mile wide : yet, through this the contents of the entire basin are drained into the valley of Chamounix with perfect steadiness, and cannot possibly fill the basin beyond a certain constant height above the point of overflow. Overflow 7 , I say, deliberately ; distinguishing always the motion of this true fluid from that of the sand in an hour- glass, or stones slipping in a heap of shale. But that the nature of this distinction may be entirely conceived by you, I must ask you to pause with some attention at this word, to 'flow,' — which attention may perhaps be more prudently asked in a separate chapter. CHAPTER IV. LABITUR, ET LABETUIt. {Lecture given at London Institution, continued, with added Illustrations.) 1. Of course — we all know what flowing means. Well, it is to be hoped so ; but I'm not sure. Let us see. The sand of the hour-glass, — do you call the motion of that flowing ? No. It is only a consistent and measured fall of many unat- tached particles. Or do you call the entrance of a gas through an aperture, out of a full vessel into an empty one, flowing ? No. That is expansion — not flux. Or the draught through the keyhole ? No — is your answer, LABITUR, ET LABETUR. 38 still. Let us take instance in water itself. The spring of a fountain, or of a sea breaker into spray. You don't call that flowing ? No. Nor the fall of a fountain, or of rain ? No. Well, the rising of a breaker, — the current of water in the hollow shell of it, — is that flowing ? No. After it has broken — rushing up over the shingle, or impatiently advancing on the sand ? You begin to pause in your negative. Drooping back from the shingle then, or ebbing from the sand ? Yes ; flowing, in some places, certainly, now. You see how strict and distinct the idea is in our minds. Will you accept — I think you may, — this definition of it? Flowing is " the motion of liquid or viscous matter over solid matter, under the action of gravity, without any other impel- ling force." 2. Will you accuse me, in pressing this definition on you, of wasting time in mere philological nicety ? Permit me, in the capacity which even the newspapers allow to me, — that of a teacher of expression, — to answer you, as often before now, that philological nicety is philosophical nicety. See the im- portance of it here. I said a glacier flowed. But it remains a question whether it does not also spring, — whether it can rise as a fountain, no less than descend as a stream. For, broadly, there are two methods in which either a stream or glacier moves. The first, by withdrawing a part of its mass in front, the vacancy left by which, another part supplies from behind. That is the method of a continuous stream, — perpetual de- duction,* by what precedes, of what follows. The second method of motion is when the mass that is behind, presses, or is poured in upon, the masses before. That is the way in which a cataract falls into a pool, or a fountain into a basin. Now, in the first case, you have catenary curves, or else * " Ex quo ilia admirabilis a majoribus aquae facta deductio est."-* Cic. de Div., 1, 44. 40 DEUCALION. curves of traction, going down the stream. In the second case, you have irregularly concentric curves, and ripples of impulse and compression, succeeding each other round the pool. 3. Now the Mer de Glace is deduced down its narrow channel, like a river ; and the Glacier des Bossons is de- duced down its steep ravine ; and both were once injected into a pool of ice in the valley below, as the Glacier of the Ehone is still. Whereupon, observe, if a stream falls into a basin — level-lipped all round — you know when it runs over it must be pushed over — lifted over. But if ice is thrown into a heap in a plain, you can't tell, without the closest observa- tion, how violently it is pushed from behind, or how softly it is diffusing itself in front ; and I had never set my eyes or wits to ascertain where compression in the mass ceased, and diffusion began, because I thought Forbes had done every- thing that had to be done in the matter. But in going over his work again I find he has left just one thing to be still ex- plained ; and that one chances to be left to me to show you this evening, because, by a singular and splendid Nemesis, in the obstinate rejection of Forbes's former conclusively simple experiments, and in the endeavour to substitute others of his own, Professor Tyndall has confused himself to the extreme point of not distinguishing these two conditions of deductive and impulsive flux. His incapacity of drawing, and ignorance of perspective, prevented him from constructing his diagrams either clearly enough to show him his own mistakes, or pret- tily enough to direct the attention of his friends to them ; — and they luckily remain to us, in their absurd immortality. 4. Forbes poured viscous substance in layers down a trough ; let the stream harden ; cut it into as many sections as were required ; and showed, in permanence, the actual conditions of such viscous motion. Eager to efface the memory of these conclusive experiments, Professor Tyndall ( c Glaciers of the Alps, 5 page 383) substituted this literally ' superficial ' one of his own. He stamped circles on the top of a viscous current ; found, as it flowed, that they were drawn into ovals ; but had not wit to consider, or sense to LABITUR, ET LABETUR. 41 D E see, whether the area of the circle was enlarged or diminished — or neither — during its change in shape. He jumped, like the rawest • schoolboy, to the conclusion that a circle, becoming an oval, must neces- sarily be compressed ! You don't compress a globe of glass when you 1 blow it into a soda-water bottle, do you? 5. But to reduce Professor Tyn- dall's problem into terms. Let A F, Fig. 3, be the side of a stream of any substance whatever, and a /the middle of it ; and let the particles at the middle move twice as fast as the particles at the sides. Now we cannot study all the phenomena of fluid motion in one diagram, nor any one phenomenon of fluid motion but by progressive diagrams ; and this first one only shows the changes of form which would take place in a substance which moved with uniform increase of rapidity from side to centre. No fluid substance would so move ; but you can only trace the geometrical facts step by step, from uniform increase to accelerated in- crease. Let the increase of rapidity, therefore, first be supposed uniform. Then, while the point A moves to B, the point a moves to taining, I suppose, the first serviceable description of agates- cent structure yet extant.* 6. Hitherto, however, notwithstanding all that has been ac- complished, nobody can tell us how a common flint is made. Nobody ever made one ; nobody has ever seen one naturally coagulate, or naturally dissolve ; nobody has ever watched their increase, detected their diminution, or explained the exact share which organic bodies have in their formation. The splendid labours of Mr. Bowerbank have made us ac- quainted with myriads of organic bodies which have provoked siliceous concretion, or become entangled in it : but the beau- tiful forms which these present have only increased the dif- ficulty of determining the real crystalline modes of siliceous structure, unaffected by organic bodies. 7. Crystalline modes, I say, as distinguished from crystalline laws. It is of great importance to mineralogy that we should carefully distinguish between the laws or limits which deter- mine the possible angles in the form of a mineral, and the modes, or measures, in which, according to its peculiar nature or circumstances, it conducts itself under these restrictions. Thus both cuprite and fluor are under laws which enforce cubic or octohedric angles in their crystals ; but cuprite can arrange its cubes in fibres finer than those of the softest silk, while fluor spar only under rare conditions distinctly elongates its approximate cube into a parallelopiped. Again, the prismatic crystals of Wavellite arrange them- selves invariably in spherical or reniform concretions ; but the rhombohedral crystals of quartz and hematite do so only under particular conditions, the study of which becomes a quite distinct part of their lithology. * I must, however, refer the reader to the valuable summary of work hitherto done on this subject by Professor Rupert Jones, (Proceedings of Geologist's Association, Vol. IV., No. 7,) for examination of these questions of priority. FIRE AND WATER. 99 8. This stellar or radiant arrangement is one essential con- dition in the forms and phenomena of agate and chalcedony ; and Mr. Clifton "Ward has shown in the paper to which I have just referred, that it is exhibited under the microscope, as a prevalent condition in their most translucent substance, and on the minutest scale. Now all siliceous concretions, distinguishing themselves from the mass of the surrounding rocks, are to be arranged under two main classes ; briefly memorable as knots and nuts ; the latter, from their commonly oval form, have been usually described by mineralogists as, more specially, 'almonds.' ' Knots ' are concretions of silica round some central point or involved substance, (often organic) ; such knots being usu- ally harder and more solid in the centre than at the outside, and having their fibres of crystallization, if visible, shot out- wards like the rays of a star, forming pyramidal crystals on the exterior of the knot. 9. 'Almonds 9 are concretions of silica formed in cavities of rocks, or, in some cases, probably by their own energy pro- ducing the cavities they enclose ; the fibres of crystallization, if visible, being directed from the outside of the almond-shell towards its interior cavity. 10. These two precisely opposite conditions are severally represented best by a knot of sound black flint in chalk, and by a well-formed hollow agate in a volcanic rock. I have placed in the Sheffield Museum a block of black flint, formed round a bit of Inoceramus shell ; and an almond-shell of agate, about six times as big as a cocoa nut, which will satisfactorily illustrate these two states. Bat between the two, there are two others of distinctly gelatinous silica, and distinctly crystalline silica, filling pores, cavities, and veins, in rocks, by infiltration or secretion. And each of these states will be found passing through infinite gradations into some one of the three others, so that separate account has to be given of every step in the transitions before we can rightly understand the main types. 11. But at the base of the whole subject lies, first, the clear understanding of the way a knot of solid crystalline 100 LEU C ALIO JS\ substance — say, a doclecahedral garnet — forms itself out of a rock-paste, say greenstone trap, without admitting a hairs- breadth of interstice between the formed knot and enclosing paste ; and, secondly, clear separation in our thoughts, of the bands or layers which are produced by crystalline segregation, from those produced by successively accumulating substance. But the method of increase of crystals themselves, in an ap- parently undisturbed solution, has never yet been accurately described ; how much less the phenomena resulting from influx of various elements, and changes of temperature and pressure. The frontispiece to the third number of i Deu- calion ' gives typical examples of banded structure resulting from pure crystalline action ; and the three specimens, 1. A. 21, 22, and 23, at Sheffield, furnish parallel examples of ex- treme interest. But a particular form of banding in flint, first noticed and described by Mr. S. P. Woodward,* is of more interest than any other in the total obscurity of its origin ; and in the extreme decision of the lines by which, in a plurality of specimens, the banded spaces are separated from the homogeneous ones, indicating the first approach to the conditions which produce, in more perfect materials, the forms of, so-called ' brecciated ' agates. Together with these, a certain number of flints are to be examined which present every appearance of having been violently fractured and re- cemented. "Whether fractured by mechanical violence, by the expansive or decomponent forces of contained minerals, or by such slow contraction and re-gelation as must have taken place in most veins through masses of rock, w r e have to ascertain by the continuance of such work as my friend has here begun. Letter I.f — Introductory. 12. " I am beginning to be perplexed about the number of flints, containing problems and illustrations, and wondering to what extent my inquiries will be of any use to you. * ' Geological Magazine,' 1864, vol. i., p. 145, pi. vii. and viii. | I shall put my own notes on these and any future communications I may insert, in small print at the bottom of the pages ; and with letter- FIRE AND WA TEH. 101 " I intended at first to collect only what was really beauti- ful in itself — ' crystalline '! but how the subject widens, and how the arbitrary divisions do run into one another ! What a paltry shifting thing our classification is ! One is sometimes tempted to give it all up in disgust, and I have a shrewd sus- picion that all scientific classification (except for mutual aid to students) is absurd and pedantic : (a) varieties, species, genera, classes, orders, have most of them more in common than of divergence, — ' a forming spirit ' everywhere, for use and beauty. "It is (to me) impossible to separate purely mineral and chemical siliceous bodies in chalk, (b) from those which are partly formed by the silicate-collecting sponges, which seem to have given them their forms. "Who is to say that the radiations and accretions of a crystal are not life, but that the same arrangements in a leaf or a tree are life ? — that the clouds which float in their balanced changeableness are not as much guided and defined as the clouds of the chalcedony, or the lenses of the human eye which perceives them ? " I think the following facts are plain : " 1. The chalk bands do go through the flint. " 2. Fissures in flints are constantly repaired by fresh deposits of chalcedony and silex. " 3. Original sponge matter is preserved (c) and obliterated by siliceous deposit, in extent and degree varying infinitely, and apparently proportioned to the amount of iron present — i.e., the iron preserves original form, unless when combined with sulphur enough to crystallize, when all the original structure disappears. references — a, b, etc. ; but the notes of the authors themselves will be put at the end of their papers, in large print, and with number-ref- erences— 1, 2, etc. {a) All, at least, is imperfect ; and most of it absurd in the attempt to be otherwise. (b) It may be doubtful if any such exist in chalk ; but, if they exist, they will eventually be distinguishable. (c) Q. The form or body of it only ; is the matter itself ever pre- served ? 102 DEUCALION. "4. Amygdaloids seem to be formed by a kind of inde* pendent or diverse arrangement of molecules, caused hj slight admixture of foreign minerals." Letter II. — Memoranda made at MantelVs Quarry, Cuckfield, on the banding noticed in the beds and nodules of the sili- ceous calciferous sandstone there, Slst May, 1876. Nos. L and II. Ovate, concentric, ferruginous bandings ; the centre apparently (1) free from banding. III. Bands arranged at acute angles. These bands are not caused by fracture, but apparently by the intersection, at an acute angle, of the original lines of deposit, (d) IV. In this specimen the newly fractured surfaces show no bandings, but the weathered surface develops the banding. V. Ditto — i.e. bands parallel ; much more ferruginous and consequently more friable when exposed to weathering. May not something be learnt regarding the laws of banding in agates, flints, etc., from observing the arrangement of banding in rocks composed mainly of siliceous matter ? (e) May not some of the subtler influences which regulate the growth of trees in their lines of annual increase (magnetic probably) have some effect in the arrangement of minerals in solution ? — nay, even of the higher vital processes, such as the deposition of osseous matter in teeth and bones ? (/) Letter III. — Memoranda respecting banded chalk. I. In the banded lines (ferruginous) noticed above and be- low the horizontal fissures beneath the cliff at the Hope Gap, Seaford, it is evident that these lines are not markings of Note 1, page 121. (d) These angular concretions require the closest study ; see the seg- ments of spheres in the plate given in the last number. {e) More, I should say, from the agates, respecting the laws of band- ing in rocks : see the plate to the present number. When we can ex- plain the interruptions of the bands on such scale as this, we may begin to understand some of those in larger strata. if) Yes, certainly ; but in such case, the teeth and bones act by mineral law ; not the minerals by teeth and bone law. FIRE AND WATER. 103 original deposition, but are caused by successive infiltrations of water containing iron in solution, (g) II. Concentric markings of the same nature are observable in places where — a. Iron pyrites are decomposing, and the iron in solution is being successively infiltrated into the surrounding chalk rock. b. From dropping of ferruginous springs through crevices on horizontal surfaces. c. This is observable also on surfaces of tabular flint. III. Very peculiar contorted bandings, (similar to the so- called contorted-rocks,) are observable in certain places, notably in the face of the chalk-pit on the east side of Gold- stone Bottom. This chalk-pit, or quarry, is remarkable — 1. For the contorted bandings in the chalk rock which are not markings of original deposition, being quite independent of original stratification, (h) 2. For the excessive shattering and Assuring observable. 3. For the fact that these cracks and fissures have been re- filled with distinctive and varying substances, as with flint, clay, Websterite, and intermediate admixtures of these sub- stances. 4. For veins of flint, formerly horizontal, which show visi- ble signs of disjDlacenient by subsidence. 5. For the numerous fissures in these veins of tabular flint being stained by iron, which apparently aids in the further process of splitting up and of widening the minute crevices in the flint. The iron also appears to be infiltrated at varying depths into the body of unfractured flint. Qy. Has not ordinary flint the power or property of absorb- ing ferruginous fluid ? (g) Questionable. Bands are almost always caused by concretion, or separation, not infiltration. However caused, tlie essential point, in the assertion of which this paper has so great value, is their distinction from strata. (h) A most important point. It is a question with me whether the greater number of minor contortions in Alpine limestones may not have been produced in this manner. When once the bands are arranged by segregation, chemical agencies will soon produce mechanical separation, as of original beds. 104 DEUCALION. Letter IV. — Memoranda respecting brecciate flint. "June 7, 1876. " I hasten to report the result of my fresh inquiry respect- ing the specimen I first sent to you as 'breccia/ but which you doubted. " The site is the embouchure of the little tidal river Cuck- mere, about two miles east of Seaford. I found a block at about the same spot (about three hundred yards east of the coastguard station, and about three quarters of the distance west of the river's mouth). "The rocks are here covered with sand, or with a bed of the old valley alluvium, not yet removed by wave action. Travelling westward, the transported blocks of breccia gradually increase in size, (a pretty sure augury that they were derived from a western source). The whole coast is subject to a very rapid degradation and consequent encroach- ment of the sea, the average in some places being from twenty- five to thirty feet yearly. At a spot a hundred yards east of the coastguard station, blocks of one or two tons were visible. The denuded chalk rock is of chalk, seamed and fissured ; the cliff of the same nature ; but all the flints, and especially the tabular veins, are splintered and displaced to an unusual extent. " Farther westward yet, the blocks of breccia weigh several tons, the cement being itself fissured, and in some places con- sisting of angular fragments stained with iron. From one mass I extracted a hollow circular flint split into four or five pieces, the fragments, although displaced, re-cemented in juxtaposition, (i) " At the Hope Gap, the whole cliff becomes a fractured mass, the fissures being refilled, sometimes with calcareous cement, sometimes with clay, and in other places being hollow. " From the sides of an oblique fissure filled with clay I extracted two pieces of a nodular flint, separated from each (i) I am not prepared to admit, yet, that any of these phenomena are owing to violence. We shall see. FIRE AND WATER 105 other by a two-inch seam of clay : when replaced (the clay having been removed) the two fitted exactly. An examin- ation of the rocks shows that the fissures, which run in all directions, are largest when nearly horizontal, dipping slightly seawards. " The upper and lower portions of some of these horizontal fissures are banded with iron stains, evidently derived from iron-water percolating the seams. "If I am right, therefore, the mystery seems to be ex- plained thus : (k) — " L Rain water, charged with carbonic acid, falling on the hills behind, trickles past the grass and humus beneath, through the cracks in the chalk, dissolving the carbonate of lime into a soluble bi-carbonate. Falling downwards, it escapes seaw r ards through the horizontal fissures, widening them by its solvent power. " II. The weight of the superincumbent mass by slow, cer- tain, irregular pressure, descends, maintaining the contact of surfaces, but still ever sinking at intervals, varied by the re- sisting forces of weight and pressure. "III. This process is probably accelerated by the inflow and reflow of salt water at the ebb and flow of tide (into the fissures). "IV. At certain periods, probably in the summer, (as soluble bi-carbonate of lime becomes less soluble as temper- ature increases,) a portion becomes redeposited as a hard semi-crystalline calcareous cement. " V. This cement appears, in some instances, to be slightly siliceous, and may have a tendency, by the mutual attraction of siliceous matter, to form solid layers of tabular flint. "VI. If these deductions be correct, it is probable that the great results involved in the sinking of limestone hills, and the consequent encroachment of the sea, may be traced (step (W) I think this statement of Mr. Willett s extremely valuable ; and see no reason to doubt its truth, as an explanation of the subsidence or chalk and limestone in certain localities. I do not hitherto receive it as any explanation of fracture in Hints. I believe Dover Cliffs might sink to Channel bottom without splitting a flint, unless bedded. 106 DEUCALION. by step) to the springs in valleys 'which run among the hills ; ' thence to the rain and dewdrops ; higher up to the mists and clouds ; and so onward, by solar heat, to the ocean, where at last again they find their rest." Letter V. — Final Abstract. "June 13, 1876. "In addition to the heat derived from summer and at- mospheric changes, there will be a considerable amount of heat evolved from the friction produced between the sides of fissures when slipping and subsidence occur, and from the crushing down of flint supports when weight overcomes re- sistance. " After heavy rainfall — 1. Fissures are filled. 2. Solution is rapid. 3. Hydraulic pressure increases. 4. Fissures are widened. " After a period of dry weather — 1. Solution is diminished. 2. Hydraulic pressure relieved. 3. Subsidence and flint-crushing commence, or progress more rapidly. 4. Heat is evolved. 5. Carbonic acid discharged. 6. Semi-crystalline carbonate of lime is deposited around. a. Fragments of crushed flint, (at rest at intermitting intervals between motion of rocks). b. Angular fragments of original chalk rock. c. Angular fractured pieces of old cement. "I have a dawning suspicion that siliceous deposits (as chalcedony, etc.) are made when the temperature falls, for reasons which I must postpone to a future paper." THIRTY YEARS SINCE. 107 (1) Probably the same arrangement exists (concentric), but has not been made visible because the iron has not been oxydized. CHAPTER X. 'thirty years since.' Village of Simplon, 2d September, 1876. 1. I am writing in the little one-windowed room opening from the salle-a-manger of the Hotel de la Poste ; but under some little disadvantage, being disturbed partly by the invo- cation, as it might be fancied, of calamity on the heads of nations, by the howling of a frantic wind from the Col ; and partly by the merry clattering of the knives and forks of a hungry party in the salon doing their best to breakfast ade- quately, while the diligence changes horses. In that same room, — a little earlier in the year, — two-and- thirty years ago, my father and mother and I were sitting at one end of the long table in the evening : and at the other end of it, a quiet, somewhat severe-looking, and pale, English (as we supposed) traveller, with his wife ; she, and my mother, working ; her husband carefully completing some mountain outlines in his sketch-book. 2. Those days are become very dim to me ; and I forget which of the group spoke first. My father and mother were always as shy as children ; and our busy fellow-traveller seemed to us taciturn, slightly inaccessible, and even Al- pestre, and, as it were, hewn out of mountain flint, in his serene labour. Whether some harmony of Scottish accent struck my father's ear, or the pride he took in his son's accomplishments prevailed over his own shyness, I think we first ventured word across the table, with view of informing the grave draughtsman that we also could draw. Whereupon my own sketch-book was brought out, the pale traveller politely per- missive. My good father and mother had stopped at the .108 DEUCALION. Simplon for me, (and now, feeling miserable myself in the thin air, I know what it cost them,) because I wanted to climb the high point immediately w T est of the Col, thinking thence to get a perspective of the chain joining the Fletschhorn to the Monte Bosa. I had been drawing there the best part of the afternoon, and had brought down with me careful studies of the Fletschhorn itself, and of a great pyramid far eastward, whose name I did not know, but, from its bearing, supposed it must be the Matterhorn, which I had then never seen. 3. I have since lost both these drawings ; and if they were given away, in the old times when I despised the best I did, because it was not like Turner, and any friend has preserved them, I wish they might be returned to me ; for they would be of value in Deucalion, and of greater value to myself ; as having won for me, that evening, the sympathy and help of James Forbes. For his eye grew keen, and his face attentive, as he examined the drawings ; and he turned instantly to me as to a recognized fellow- workman, — though yet young, no less faithful than himself. He heard kindly what I had to ask about the chain I had been drawing ; only saying, with a slightly proud smile, of my peak supposed to be the Matterhorn,* " No, — and when once you have seen the Matterhorn, you will never take anything else for it ! " He told me as much as I w r as able to learn, at that time, of the structures of the chain, and some pleasant general talk followed ; but I knew nothing of glaciers then, and he had his evening's work to finish. And I never saw him again. I wonder if he sees me now, or guided my hand as I cut the leaves of M. Violet-le-Duc's ' Massif du Mont Blanc ' this morn- ing, till I came to page 58, — and stopped ! I must yet go back, for a little while, to those dead days. 4. Failing of Matterhorn on this side of the valley of the Ehone, I resolved to try for it from the other ; and begged my father to wait yet a day for me at Brieg. No one, then, had ever heard of the Bell Alp ; and few Eng- lish knew even of the Aletsch glacier. I laid my plans from * It was the Weisshorn. THIRTY YEARS SINGE. 109 the top of the Simplon Col ; and was up at four, next day ; in a cloudless morning, climbing the little rock path which as- cends directly to the left, after crossing the bridge over the Ehone, at Brieg ; path which is quite as critical a little bit of walking as the Ponts of the Mer de Glace ; and now, encum- bered with the late fallen shatterings of a flake of gneiss of the shape of an artichoke leaf, and the size of the stern of an old ship of the line, which has rent itself away, and dashed down like a piece of the walls of Jericho, leaving exposed, underneath, the undulatory surfaces of pure rock, which, I am under a very strong impression, our young raw geologists take for real " mutton ed " glacier tracks.* I took this path because I wanted first to climb the green wooded mass of the hill rising directly over the valley, so as to enfilade the entire profiles of the opposite chain, and length of the valley of the Rhone, from its brow. By midday I had mastered it, and got up half as high again, on the barren ridge above it, commanding a little tarn ; whence, in one panorama are seen the Simplon and Saas Alps on the south, with the Matterhorn closing the avenue of the valley of St. Nicolas ; and the Aletsch Alps on the north, with all the lower reach of the Aletsch glacier. This panorama I drew carefully; and slightly coloured afterwards, in such crude way as I was then able ; and fortunately not having lost this, I place it in the Sheffield Museum, for a perfectly trustworthy witness to the extent of snow on the Breithorn, Fletschhorn, and Montague de Saas, thirty years ago. My drawing finished, I ran round and down obliquely to the Bell Alp, and so returned above the gorge of the Aletsch torrent — making some notes on it afterwards used in c Mod- ern Painters,' many and many such a day of foot and hand labour having been needed to build that book, in which my friends, nevertheless, I perceive, still regard nothing but what they are pleased to call its elegant language, and are entirely indifferent, with respect to that and all other books they read, whether the elegant language tells them truths or lies. * I saw this wisely suggested in a recent number of the ' Alpine Journal.' 110 DEUCALION. That book contains, however, (and to-day it is needful that I should not be ashamed in this confidence of boasting) the first faithful drawings ever given of the Alps, not only in Eng- land, but in Europe ; and the first definitions of the manner in which their forms have been developed out of their crys- talline rocks. 6. 'Definitions' only, observe, and descriptions; but no * explanations.' I knew, even at that time, far too much of the Alps to theorize on them ; and having learned, in the thirty years since, a good deal more, with the only consequence of finding the facts more inexplicable to me than ever, laid M. Violet-le-D uc's book on the seat of the carriage the day be- fore yesterday, among other stores and preparations for pass- ing the Simplon, contemplating on its open first page the splendid dash of its first sentence into space, — " La croute terrestre, refroidie au moment du plissement qui a forme le massif du Mont Blanc," — with something of the same amaze- ment, and same manner of the praise, which our French allies are reported to have rendered to our charge at Balaclava : — u (Test magnifique ; — mais ce n'est pas" — la geologie. 7. I soon had leisure enough to look farther, as the steam- ing horses dragged me up slowly round the first ledges of pines, under a drenching rain which left nothing but their nearest branches visible. Usually, their nearest branches, and the wreaths of white clouds braided among them, would have been all the books I cared to read ; but both curiosity and vanity were piqued by the new utterances, prophetic, appar- ently, in claimed authority, on the matters timidly debated by me in old time. I soon saw that the book manifested, in spite of so great false-confidence, powers of observation more true in their scope and grasp than can be traced in any writer on the Alps since De Saussure. But, alas, before we had got up to Berisal, I had found also more fallacies than I could count, in the author's first statements of physical law ; and seen, too surely, that the poor Frenchman's keen natural faculty, and quite splendid zeal and industry, had all been wasted, through the wretched THIRTY YEARS SINCE. Ill national vanity which made him interested in Mont Blanc only 'since it became a part of France/ and had thrown him totally into the clique of Agassiz and Desor, with results in which neither the clique, nor M. Violet, are likely, in the end, to find satisfaction. 8. Too sorrowfully weary of bearing with the provincial tem- per, and insolent errors, of this architectural restoration of the Gothic globe, I threw the book aside, and took up my Carey's Dante, which is always on the carriage seat, or in my pocket — not exactly for reading, but as an antidote to pesti- lent things and thoughts in general ; and store, as it were, of mental quinine,— a few lines being usually enough to recover me out of any shivering marsh fever fit, brought on among foulness or stupidity. It opened at a favourite old place, in the twenty-first canto of the Paradise, (marked with an M. long ago, when I was reading Dante through to glean his mountain descriptions): — - u 'Twixt either shore Of Italy, nor distant from thy land," etc.; and I read on into the twenty-third canto, down to St. Bene- dict's ff. There, all things are, as they have ever been; Our ladder reaches even to that clime, Whither the patriarch Jacob saw it stretch Its topmost round, when it appeared to him With angels laden. But to mount it now None lifts his foot from earth ; and hence my rule Is left a profitless stain upon the leaves, The walls, for abbey reared, turned into dens ; The cowls, to sacks choked up with musty meal. * * * * His convent, Peter founded without gold Or silver ; I, with prayers and fasting, mine; And Francis, his, in meek humility. And if thou note the point whence each proceeds, Then look what it hath erred to, thou shalt find The white turned murky. Jordan was turned back, And a less wonder than the refluent sea May, at God's pleasure, work amendment here." 112 DEUCALION. 9. I stopped at this, (holding myself a brother of the third order of St. Francis,) and began thinking how long it would take for any turn of tide by St. George's work, when a ray of light came gleaming in at the carriage window, and I saw, where the road turns into the high ravine of the glacier gal- leries, a little piece of the Breithorn snowfield beyond. Somehow, I think, as fires never burn, so skies never clear, while they are watched ; so I took up my Dante again, though scarcely caring to read more ; and it opened, this time, not at an accustomed place at all, but at the " I come to aid thy wish," of St. Bernard, in the thirty-first canto. Not an accustomed place, because I always think it very unkind of Beatrice to leave him to St. Bernard ; and seldom turn expressly to the passage : but it has chanced lately to become of more signifi- cance to me, and I read on eagerly, to the " So burned the peaceful oriflamme/' when the increasing light became so strong that it awaked me, like a new morning ; and I closed the book again, and looked out. We had just got up to the glacier galleries, and the last films of rain were melting into a horizontal bar of blue sky which had opened behind the Bernese Alps. I watched it for a minute or two through the alternate arch and pier of the glacier galleries, and then as we got on the open hill flank again, called to Bernardo * to stop. 10. Of all views of the great mountains that I know r in Switzerland, I think this, of the southern side of the Bernese range from the Simplon, in general the most disappointing — for two reasons : the first, that the green mass of their foun- dation slopes so softly to the valley that it takes away half the look of their height ; and the second, that the greater peaks are confused among the crags immediately above the Aletsch glacier, and cannot, in quite clear weather, be recognized as more distant, or more vast. But at this moment, both these disadvantages were totally conquered. The whole valley was full of absolutely impenetrable wreathed cloud, nearly all pure * Bernardo Bergonza, of the Hotel d'ltalie, Arona, in whom any friend of mine will find a glad charioteer ; and they cannot anywhere find an abler or honester one. THIRTY TEARS SINCE. 113 white, only the palest grey rounding the changeful domes of it ; and beyond these domes of heavenly marble, the great Alps stood up against the blue, — not wholly clear, but clasped and entwined with translucent folds of mist, traceable, but no more traceable, than the thinnest veil drawn over St. Catherine's or the Virgin's hair by Lippi or Luini ; and rising as they were withdrawn from such investiture, into faint oriflammes, as if borne by an angel host far distant ; the peaks themselves strewn with strange light, by snow fallen but that moment, — the glory shed upon them as the veil fled ; — and intermittent waves of still gaining seas of light increasing upon them, as if on the first day of creation. " A present, vous pouvez voir l'hotel sur le Bell Alp, bati par Monsieur Tyndall." The voice was the voice of the driver of the supplementary pair of horses from Brieg, who, just dismissed by Bernardo, had been for some minutes considering how he could best rec- ommend himself to me for an extra franc. I not instantly appearing favourably stirred by this infor- mation, he went on with increased emphasis, "Monsieur le professeur Tyndall." The poor fellow lost his bonnemain by it altogether — not out of any deliberate spite of mine ; but because, at this sec- ond interruption, I looked at him, with an expression (as I suppose) so little calculated to encourage his hopes of my gene- rosity that he gave the matter up in a moment, and turned away, with his horses, down the hill ; — I partly not caring to be further disturbed, and being besides too slow — as I always am in cases where presence of mind is needful — in calling him back again. 11. For, indeed, the confusion into which he had thrown my thoughts was all the more perfect and diabolic, because it consisted mainly in the stirring up of every particle of personal vanity and mean spirit of contention which could be concen- trated in one blot of pure black ink, to be dropped into the midst of my aerial vision. Finding it totally impossible to look at the Alps any more, for the moment, I got out of the carriage, sent it on to th8 8 Ill DEUCALION. Simplon village ; and began climbing, to recover my feelings and wits, among the mossy knolls above the convent. They were drenched with the just past rain ; glittering now in perfect sunshine, and themselves enriched by autumn into wreaths of responding gold. The vast hospice stood desolate in the hollow behind them; the first time I had ever passed it with no welcome from either monk, or dog. Blank as the fields of snow above, stood now the useless walls ; and for the first time, unredeemed by asso- ciation ; only the thin iron cross in the centre of the roof re- maining to say that this had once been a house of Christian Hospitallers. 12. Desolate this, and dead the office of this, — for the pres- ent, it seems; and across the valley, instead, "1 hotel sur le Bell Alp, bati par Monsieur Tyndall," no nest of dreamy monks, but of philosophically peripatetic or perisaltatory ' puces des glaces.' For, on the whole, that is indeed the dramatic aspect and relation of them to the glaciers ; little jumping black things, who appear, under the photographic microscope, active on the ice- waves, or even inside of them ; — giving to most of the great views of the Alps, in the windows at Geneva, a more or less animatedly punctuate and pulicarious character. Such their dramatic and picturesque function, to any one with clear eyes ; their intellectual function, however, being more important, and comparable rather to a symmetrical suc- cession of dirt-bands, — each making the ice more invisible than the last ; for indeed, here, in 1876, are published, with great care and expense, such a quantity of accumulated rub- bish of past dejection, and moraine of finely triturated mis- take, clogging together gigantic heaped blocks of far- travelled blunder, — as it takes away one's breath to approach the shadow of. 13. The first in magnitude, as in origin, of these long-sus- tained stupidities, — the pierre-a-Bot, or Frog-stone, par ex- cellence, of the Neuchatel clique, — is Charpentier's Dilatation Theory, revived by M. Violet, not now as a theory, but an assured principle ! — without, however, naming Charpentier THIRTY TEARS SINCE. 115 as the author of it ; and of course without having read a word of Forbes's demolition of it. The essential work of Deucalion is construction, not demolition ; but when an avalanche of old rubbish is shot in our way, I must, whether I would or no, clear it aside before I can go on. I suppose myself speaking to my Sheffield men ; and shall put so much as they need know of these logs upon the line, as briefly as possible, before them. 14. There are three theories extant, concerning glacier-mo- tion, among the gentlemen who live at the intellectual ' Hotel des Neuchatelois.' These are specifically known as the Slid- ing, — Dilatation, — and Kegelation, theories. When snow lies deep on a sloping roof, and is not supported below by any cornice or gutter, you know that when it thaws, and the sun has warmed it to a certain extent, the whole mass slides off into the street. That is the way the scientific persons who hold the ' Sliding theory/ suppose glaciers to move. They assume, therefore, two things more ; namely, first that all mountains are as smooth as house-roofs ; and, secondly, that a piece of ice a mile long and three or four hundred feet deep will slide gently, though a piece a foot deep and a yard long slides fast, — in other words, that a paving-stone will slide fast on another paving-stone, but the Eossberg fall at the rate of eighteen inches a day. There is another form of the sliding theory, which is that glaciers slide in little bits, one at a time ; or, for example, that if you put a railway train on an incline, with loose fastening to the carriages, the first carriage will slide first, as far as it can go, and then stop ; then the second start, and catch it up, and wait for the third ; and so on, till when the last has come up, the first will start again. Having once for all sufficiently explained the 'Sliding theory ' to you, I shall not trouble myself any more in Deuca- lion about it. 15. The next theory is the Dilatation theory. The scien- tific persons who hold that theory suppose that whenever a shower of rain falls on a glacier, the said rain freezes inside of it ; and that the glacier being thereby made bigger, 116 DEUCALION. stretches itself uniformly in one direction, and never in any other ; also that, although it can only be thus expanded in cold and wet weather, such expansion is the reason that it always goes fastest In hot and dry weather. There is another form of the Dilatation theory, which is that the glacier expands by freezing its own meltings. 16. Having thus sufficiently explained the Dilatation theory to you, I shall not trouble myself in Deucalion farther about it ; noticing only, in bidding it goodbye, the curious want of power in scientific men, when once they get hold of a false notion, to perceive the commonest analogies implying its correction. One would have thought that, with their ther- mometer in their hand to measure congelation with, and the idea of expansion in their head, the analogy between the tube of the thermometer, and a glacier channel, and the ball of the thermometer, and a glacier reservoir, might, some sunshiny day, have climbed across the muddily-fissured glacier of their wits : — and all the quicker, that their much-studied Mer de Glace bears to the great reservoirs of ice above it precisely the relation of a very narrow tube to a very large bail. The vast c instrument ' seems actually to have been constructed by Nature, to show to the dullest of savants the difference be- tween the steady current of flux through a channel of drain- age, and the oscillatory vivacity of expansion which they constructed their own tubular apparatus to obtain ! 17. The last popular theory concerning glaciers is the Eegelation theory. The scientific persons who hold that theory, suppose that a glacier advances by breaking itself spontaneously into small pieces ; and then spontaneously sticking the pieces together again ; — that it becomes continu- ally larger by a repetition of this operation, and that the enlargement (as assumed also by the gentlemen of the dilata- tion party), can only take place downwards. You may best conceive the gist of the Eegelation theory by considering the parallel statement, which you may make to your scientific young people, that if they put a large piece of barley sugar on the staircase landing, it will walk downstairs by alternately cracking and mending itself. THIRTY YEARS SINCE. 117 I shall not trouble myself farther, in Deucalion, about the Regelation theory. 18. M. Violet-le-Duc, indeed, appears to have written his book without even having heard of it ; but he makes most dextrous use of the two others, fighting, as it were, at once with sword and dagger ; and making his glaciers move on the Sliding theory when the ground is steep, and on the Dilatation theory when it is level. The woodcuts at pages 65, 66, in which a glacier is represented dilating itself up a number of hills and down again, and that at page 99, in which it defers a line of boulders, which by unexplained supernatural power have been deposited all across it, into moraines at its side, cannot but remain triumphant among monuments of scientific B Fig. 5. error, — bestowing on their author a kind of St. Simeon- Stylitic pre-eminence of immortality in the Paradise of Fools. 19. Why I stopped first at page 58 of this singular volume, I see there is no room to tell in this number of Deucalion ; stili less to note the interesting repetitions by M. Violet-le-Duc of the Tyndall-Agassiz demonstration that Forbes' assertion of the plasticity of ice in large pieces, is now untenable, by reason of the more recent discovery of its plasticity in little ones. I have just space, however, for a little woodcut from the ' Glaciers of the Alps/ (or ' Forms of Water,' I forget which, and it is no matter,) in final illustration of the Tyndalh Agassiz quality of wit. 20, Fig. 5, a, is Professor Tyndall's illustration of the effect 118 DEUCALION. of sunshine on a piece of glacier, originally of the form shown by the dotted line, and reduced by solar power on the south side to the beautifully delineated wave in the shape of a wedge. It never occurred to the scientific author that the sunshine would melt some of the top, as well as of the side, of his parallelopiped ; nor that, during the process, even on the shady side of it, some melting would take place in the sum- mer air. The figure at b represents three stages of the dimi- nution which would really take place, allowing for these other somew T hat important conditions of the question ; and it shows, what may farther interest the ordinary observer, how rectan- gular portions of ice, originally produced merely by fissure in its horizontal mass, may be gradually reduced into sharp, axe- edged ridges, having every appearance of splintery and vitre- ous fracture. In next Deucalion I hope to give at last some account of my experiments on gelatinous fracture, made in the delightful laboratory of my friend's kitchen, with the aid of her infinitely conceding, and patiently collaborating, cook. CHAPTER XX OF SILICA IN LAVAS. 1. The rocks through whose vast range, as stated in the ninth chapter, our at first well-founded knowledge of their igneous origin gradually becomes dim, and fades into theory, may be logically divided into these four following groups. I. True lavas. Substances which have been rapidly cooled from fusion into homogeneous masses, showing no clear traces of crystallization. II. Basalts.* Rocks in which, without distinct separation of their elements, a disposition towards crystalline structure manifests itself. * I use this word as on the whole the best for the vast class of rocks I wish to include ; but without any reference to columnar desiccation I consider, in this arrangement, only internal structure. OF SILICA IN LAVAS. 119 III. Porphyries. Eocks in which one or more mineral ele- ments separate themselves in crystalline form from a homo- geneous paste. IV. Granites. Eocks in which all their elements have taken crystalline form. 2. These, I say, are logical divisions, very easily tenable. But Nature laughs at logic, and in her infinite imagination of rocks, defies all Kosmos, except the mighty one which we, her poor puppets, shall never discern. Our logic will help us but a little way ; — so far, however, we will take its help. 3. And first, therefore, let us ask what questions impera- tively need answer, concerning indisputable lavas, seen by living human eyes to flow incandescent out of the earth, and thereon to cool into ghastly siags. On these I have practically burnt the soles of my boots, and in their hollows have practically roasted eggs ; and in the lee of them, have been wellnigh choked with their stench ; and can positively testify respecting them, that they were in many parts once fluid under power of fire, in a very fine and soft flux ; and did congeal out of that state into ropy or cel- lular masses, variously tormented and kneaded by explosive gas ; or pinched into tortuous tension, as by diabolic tongs ; and are so finally left by the powers of Hell, to submit them- selves to the powers of Heaven, in black or brown masses of adamantine sponge without water, and horrible honeycombs without honey, interlaid between drifted banks of earthy flood, poured down from merciless clouds whose rain was ashes. The seas that now beat against these, have shores of black sand ; the peasant, whose field is in these, ploughs with his foot, and the wind harrows. 4. Now of the outsides of these lava streams, and unaltered volcanic ashes, I know the look well enough ; and could sup- ply Sheffield with any quantity of characteristic specimens, if their policy and trade had not already pretty nearly buried them, and great part of England besides, under such devil's ware of their own production. But o* the insides of these lava streams, and of the recognized iterations of volcanic 120 DEUCALION. tufa, I know nothing. And, accordingly, I want authentic an* swer to these following questions, with illustrative specimens. 5. a. In lavas which have been historically hot to perfect fusion, so as to be progressive, on steep slopes, in the man- ner of iron out of a furnace in its pig-furrows ; — in such per- fect lavas, I say — what kind of difference is there between the substance at the surface and at the extremest known depths, after cooling ? It is evident that such lavas can only accumu- late to great depths in infernal pools or lakes. Of such lakes, which are the deepest known ? and of those known, where are the best sections ? I want for Sheffield a series of speci- mens of any well-fused lava anywhere, showing the gradations of solidity or crystalline consolidation, from the outside to extreme depth. b. On lavas which have not been historically hot, but of which there is no possible doubt that they were once fluent, (in the air,) to the above-stated degree, what changes are traceable, produced, irrespectively of atmospheric action, by lapse of time ? "What evidence is there that lavas, once cool to their centres, can sustain any farther crystalline change, or re-arrangement of mineral structure? c. Ill lavas either historically or indisputably once fluent, what forms of silica are found ? I limit myself at present to the investigation of volcanic silica: other geologists will in time take up other minerals ; but I find silica enough, and more than enough, for my life, or at least for what may be left of it. Now I am myself rich in specimens of Hyalite, and Auvergne stellar and guttate chalcedonies ; but I have no notion what- ever how these, or the bitumen associated with them, have been developed ; and I shall be most grateful for a clear ac- count of their locality, — possible or probable mode of produc- tion in that locality, — and microscopic structure. Of pure quartz, of opal, or of agate, I have no specimen connected with what I should call a truly ' living ' lava ; one, that is to say, which has simply cooled down to its existing form from the fluid state ; but I have sent to the Sheffield Museum a piece of Hyalite, on a living lava, so much like a living wasp's OF SILICA IN LaVAS. nest, and so incredible for a lava at all to the general observer, that I want forthwith some help from my mineralogical friends, in giving account of it. 6. And here I must, for a paragraph or two, pass from defi- nition of flinty and molten minerals, to the more difficult definition of flinty and molten hearts ; in order to explain why the Hyalite which I have just sent to the men of Sheffield, for their first type of volcanic silica,* is not at all the best Hyalite in my collection. This is because I practically find a certain quantity of selfishness necessary to live by ; and having no manner of saintly nature in me, but only that of ordinary men, — (which makes me all the hotter in temper when I can't get ordinary men either to see what I know they can see if they look, or do what I know they can do if they like,) — I get some- times weary of giving things away, letting my drawers get into disorder, and losing the powers of observation and thought which are connected with the complacency of possession, and the pleasantness of order. Whereupon I have resolved to bring my own collection within narrow limits ; but to constitute it resolutely and irrevocably of chosen and curious pieces, for my own pleasure ; trusting that they may be afterwards cared for by some of the persons who knew me, when I myself am troubled with care no more.f 7. This piece of Hyalite, however, just sent to Sheffield, though not my best, is the most curiously definite example I ever saw. It is on a bit of brown lava, which looks, as afore- said, a little way off, exactly like a piece of a wasp's nest : seen closer, the cells are not hexagonal, but just like a cast of a spoonful of pease ! the spherical hollows having this of nota- ble in them, that they are only as close to each other as they can be, to admit of their being perfectly round : therefore, neces- * I give tlie description of these seven pieces of Hyalite at Sheffield, in Deucalion, because their description is necessary to explain certain general principles of arrangement and nomenclature. f By the way, this selfish collection is to be primarily of stones that will icash. Of petty troubles, none are more fretting than the effect of dust on minerals that can neither be washed nor brushed. Hence, my specialty of liking for silica, felspar, and the granitic or gneissic rocks. 122 DEUCALION. sarily, with little spaces of solid stone between them. I have not the slightest notion how such a lava can be produced. It is like an oolite with the yolks of its eggs dropped out, and not in the least like a ductile substance churned into foam by expansive gas. 8. On this my sterious bit of gaseous wasp's nest, the Hya- lite seems to have been dropped, like drops of glass from a melt- ing glass rod. It seems to touch the lava just as little as it can ; sticks at once on the edges of the cells, and laps over without run- ning into, much less filling them. There is not any appearance, and I think no possibility, of exudation having taken place ; the silica cannot but, I think, have been deposited ; and it is stuck together just as if it had fallen in drops, which is what I mean by calling Hyalite characteristically 6 guttate 5 ; but it shows, nevertheless, a tendency to something like crystalliza- tion, in irregularities of surface like those of glacier ice, or the kind of old Venetian glass which is rough, and apparently of lumps coagulated. The fracture is splendidly vitreous, — the substance, mostly quite clear, but in parts white and opaque. 9. Now although no other specimen that I have yet seen is so manifestly guttate as this, all the Irpalites I know agree in approximate conditions ; and associate themselves with forms of chalcedony which exactly resemble the droppings from a fine wax candle. Such heated waxen effluences, as they con- geal, will be found thrown into flattened coats ; and the chal- cedonies in question on the under surface precisely resemble them ; while on the upper they become more or less crystalline, and, in some specimens, form lustrous stellar crystals in the centre. 10. Now, observe, this chalcedony, capable of crystallization, differs wholly from chalcedony properly so called, which may indeed be covered with crystals, but itself remains consistently smooth in surface, as true Hyalite does, also. Not to be teazed with too many classes, however, I shall ar- range these peculiar chalcedonies with Hyalite ; and, accord- ingly, I send next to the Sheffield Museum, to follow this first Hyalite, an example of the transition from Hyalite to dropped chalcedony, (x. h. 2,) being an Indian volcanic chai- OF SILICA IN LA VAS. 123 cedony, translucent, aggregated like Hyalite, and showing a concave fracture where a ball of it has been broken out. 11. Next, (i. h. 3,) pure dropped chalcedony. I do not like the word ' dropped ' in this use, — so that, instead, I shall call this in future wax chalcedony ; then (i. h. 4) the same form, with crystalline surface, — this I shall henceforward call sugar chalcedony ; and, lastly, the ordinary stellar form of Auvergne, star chalcedony (i. h. 5). These five examples are typical, and perfect in their kind : next to them (i. h. 6) I place a wax chalcedony formed on a porous rock, (volcanic ash ?) which has at the surface of it small circular concavities, being also so irregularly coagulate thoughout that it suggests no mode of deposition whatever, and is peculiar, in this also, that it is thinner in the centre than at the edges, and that no vestige of its substance occurs in the pores of the rock it overlies. Take a piece of porous broken brick, drop any tallowy com- position over four or five inches square of its surface, to the depth of one-tenth of an inch ; then drop more on the edges till you have a rampart round, the third of an inch thick ; and you w r ill have some likeness of this piece of stone : but how Nature held the composition in her fingers, or composed it to be held, I leave you to guess, for I cannot. 12. Next following, I place the most singular example of ail (i. h. 7). The chalcedony in i. h. 6 is apparently dropped on the ashes, and of irregular thickness ; it is difficult to un- derstand how it was dropped, but once get Nature to hold the candle, and the thing is done. But here, in i. h. 7, it is no longer apparently dropped, but apparently boiled ! It rises like the bubbles of a strongly boil- ing liquid ; — but not from a liquid mass ; on the contrary, (except in three places, presently to be described,) it coats the volcanic ash in perfectly even thickness — a quarter of an inch, and no more, nor less, everywhere, over a space five inches square ! and the ash, or lava, itself, instead of being porous throughout the mass, w r ith the silica only on the surface, is, filled with chalcedony in every cavity ! Now this specimen completes the transitional series from 124 DEUCALION. hyalite to perfect chalcedony ; and with these seven speci- mens, in order, before us, we can define some things, and question of others, with great precision. 13. First, observe that all the first six pieces agree in two conditions, — varying, and coagulated, thickness of the deposit. But the seventh has the remarkable character of equal, and therefore probably crystalline, deposition everywhere. Secondly. In the first six specimens, though the coagula- tions are more or less rounded, none of them are regularly spherical. But in the seventh, though the larger bubbles (so to call them) are subdivided into many small ones, every un- interrupted piece of the surface is a portion of a sphere, as in true bubbles. Thirdly. The sugar chalcedony, i. h. 4, and stellar chal- cedony, i. h. 5, show perfect power of assuming, under favour- able conditions, prismatic crystalline form. But there is no trace of such tendency in the first three, or last two, of the seven examples. Nor has there ever, so far as I know, been found prismatic true hyalite, or prismatic true chalcedony. Therefore w r e have here essentially three different minerals, passing into each other, it is true ; but, at a certain point, changing their natures definitely, so that hyalite, becoming wax chalcedony, gains the power of prismatic crystallization ; and wax chalcedony, becoming true chalcedony, loses it again ! And now I must pause, to explain rightly this term 1 pris- matic,' and others which are now in use, or which are to be used, in St. George's schools, in describing crystallization. 14. A prism, (the sawn thing,) in Newton's use of the word, is a triangular pillar with fiat top and bottom. Putting two or more of these together, we can make pillars of any number of plane sides, in any regular or irregular shape. Crystals, therefore, which are columnar, and thick enough to be dis- tinctly seen, are called ' prismatic' 2. But crystals which are columnar, and so delicate that they look like needles, are called ' acicular,' from acus, a needle. 3. When such crystals become so fine that they look like bail- or down, and lie in confused directions, the mineral composed of them is called 6 plumose.' Plate V. — Structure of Lake Agate. OF SILICA IN LAVAS. 125 4. And when they adhere together closely by their sides, the mineral is called 1 fibrous/ 5. When a crystal is flattened by the extension of two of its planes, so as to look like a board, it is called ' tabular ' ; but people don't call it a ' tabula/ 6c But when such a board becomes very thin, it is called a 'lamina/ and the mineral composed of many such plates, laminated. 7. When laminae are so thin that, joining with others equally so, they form fine leaves, the mineral is c foliate.' 8. And when these leaves are capable of perpetual subdivision, the mineral is ' micaceous.' 15. Now, so far as i know their works, mineralogists hith- erto have never attempted to show cause why some minerals rejoice in longitude, others in latitude, and others in plati- tude. They indicate to their own satisfaction, — that is to say, in a manner totally incomprehensible by the public, — all the modes of expatiation possible to the mineral, by cardinal points on a sphere : but why a crystal of ruby likes to be short and fat, and a crystal of rutile, long and lean ; why amianth should bind itself into bundles of threads, cuprite weave itself into tissues, and silver braid itself into nests. — ■ the use, in fact, that any mineral makes of its opportunities, and the cultivation which it gives to its faculties, — of all this, my mineralogical authorities tell me nothing. Industry, in- deed, is theirs to a quite infinite degree, in pounding, decoct- ing, weighing, measuring, but they have remained just as un- conscious as vivisecting physicians that all this was only the anatomy of dust, — not its history. But here at last, in Cumberland, I find a friend, Mr. Clifton Ward, able and willing to begin some true history of mineral substance, and far advanced already in preliminary discovery ; and in answer to my request for help, taking up this first hy- alitic problem, he has sent me the drawings — engraved, I regret to say, with little justice to their delicacy;* — in Plate V. * But not by my fault, for I told the engraver to do his best ; and took more trouble with the plate than with any of my own. 126 DEUCALION. 16. This plate represents, in Figure 1, the varieties of structure in an inch vertical section of a lake-agate ; and ic Figures 2, 3, 4, and 5, still farther magnified portions of the layers so numbered in Figure 1. Figures 6 to 9 represent the structure and effect of polar- ized light in a lake-agate of more distinctly crystalline struct- ure ; and Figures 10 to 13, the orbicular concretions of vol- canic Indian chalcedony. But before entering farther on the description of these definitely concretionary bands, I think it will be desirable to take note of some facts regarding the larger bands of our Westmoreland mountains, which become to me, the more I climb them, mysterious to a point scarcely tolerable ; and only the more so, in consequence of their re- cent more accurate survey. 17. Leaving their pebbles, therefore, for a little while, I will ask my readers to think over some of the conditions of their crags and pools, explained as best I could, in the follow- ing lecture, to the Literary and Scientific Society of the town of Kendal. For indeed, beneath the evermore blessed Kendal- green of their sweet meadows and moors, the secrets of hill- structure remain, for all the work spent on them, in colour- less darkness ; and indeed, " So dark, Hal,, that thou could'st not see thine hand." CHAPTER XH. YEWDALE AND ITS STREAMLETS. Lecture delivered before the Members of the Literary and Scientific Institution, Kendal, 1st October, 1877. 1. I fear that some of my hearers may think an apology due to them for having brought, on the first occasion of my being honoured by their audience, a subject before them which they may suppose unconnected with my own special work, past or present. But the truth is, I knew mountains long before I knew pictures ; and these mountains of yours, before any TEWDALE AND ITS STREAMLETS. 127 other mountains. From this town, of Kendal, I went out, a child, to the first joyful excursions among the Cumberland lakes, which formed my love of landscape and of painting : and now, being an old man, I find myself more and more glad to return — and pray you to-night to return with me — from shadows to the reality. I do not, however, believe that one in a hundred of our youth, or of our educated classes, out of directly scientific circles, take any real interest in geology. And for my own part, I do not wonder, — for it seems to me that geology tells us nothing really interesting. It tells us much about a world that once was. But, for my part, a world that only was, is as little interesting as a world that only is to be. I no more care to hear of the forms of mountains that crumbled away a million of years ago to leave room for the town of Kendal, than of forms of mountains that some future day may swallow up the town of Kendal in the cracks of them. I am only in- terested — so ignoble and unspeculative is my disposition — in knowing how God made the Castle Hill of Kendal, for the Baron of it to build on, and how he brought the Kent through the dale of it, for its people and flocks to drink of. 2. And these things, if you think of them, you will find are precisely what the geologists cannot tell you. They never trouble themselves about matters so recent, or so visible ; and w^hile you may always obtain the most satisfactory in- formation from them respecting the congelation of the whole globe out of gas, or the direction of it in space, there is really not one who can explain to you the making of a pebble, or the running of a rivulet. May I, however, before pursuing my poor little inquiry into these trifling matters, congratulate those members of my audience who delight more in literature than science, on the possession, not only of dales in reality, but of dales in name. Consider, for an instant or two, how much is involved, how much indicated, by our possession in English of the six quite distinct words— vale, valley, dale, dell, glen, and dingle ;— consider the gradations of character in scene^ and fineness of observation in the inhabitants, implied by that six-foil cluster DEUCALION. of words ; as compared to the simple ' thai ' of the Germans, c valle I of the Italians, and ' vallee ' of the French, shortening into 'vaT merely for ease of pronunciation, but having no variety of sense whatever ; so that, supposing I want to trans- late, for the benefit of an Italian friend, Wordsworth's * Rev- erie of Poor Susan/ and come to u Green pastures she views in the midst of the dale," and look for 4 dale' in my Italian dictionary, I find "valle lunga e stretta tra poggi aiti," and can only convey Mr. Wordsworth's meaning to my Italian lis- tener by telling him that "la povera Susanna vede verdi prati, nel mezzo della valle lunga e stretta tra poggi alti " ! It is worth while, both for geological and literary reasons, to trace the essential differences in the meaning and proper use of these words. 3. * Vale ' signifies a large extent of level land, surrounded by hills, or nearly so ; as the Vale of the White Horse, or Vale of Severn. The level extent is necessary to the idea ; while the next word, 6 valley,' means a large hollow among hills, in which there is little level ground, or none. Next comes ' dale,' which signifies properly a tract of level land on the borders of a stream, continued for so great a distance as to make it a district of importance as a part of the inhabited country ; as Ennerdale, Langdale, Liddesdale. ' Dell ' is to dale, what valley is to vale ; and implies that there is scarcely any level land beside the stream. ' Dingle ' is such a recess or dell clothed with wood ; * and ' glen ' one varied with rocks. The term 'ravine,' a rent chasm among rocks, has its necessary parallel in other languages. Our richness of expression in these particulars may be traced to the refinement of our country life, chiefly since the fifteenth century ; and to the poetry founded on the ancient character of the Border peasantry ; mingling agricultural with shepherd life in almost equal measure. I am about to endeavour, then, to lay before you this even- * Connected partly, I doubt not, with Ingle, or Inglewood,— "brush- wood to burn, (hence Justice Inglewood in ' Hob Roy '). I have still omitted 'clough,' or cleugh, given by Johnson in relation to 'dingle,' and constant in Scott, from ' Gander-cleugh ' to 4 Buc(k)- cleugh.' T E WD ALE AND ITS STREAMLETS. 129 ing the geological laws which have produced the 'dale/ properly so called, of which I take — for a sw T eet and near ex- ample — the green piece of meadow land through which flows, into Coniston Water, the brook that chiefly feeds it. 4. And now, before going farther, let me at once vindicate myself from the blame of not doing full justice to the earnest continuance of labour, and excellent subtlety of investigation, by which Mr. Aveline and Mr. Clifton Ward have presented you with the marvellous maps and sections of this district, now in course of publication in the Geological Survey. Es- pecially let me, in the strongest terms of grateful admiration, refer to the results which have been obtained by the micro- scopic observations of minerals instituted by Mr. Sorby, and carried out indefatigably by Mr. Clifton Ward, forming the first sound foundations laid for the solution of the most secret problems of geology. 5. But while I make this most sincere acknowledgment of what has been done by these gentlemen, and by their brother geologists in the higher paths of science, I must yet in all humility lament that this vast fund of gathered knowledge is every bit of it, hitherto, beyond you and me. Dealing only with infinitude of space and remoteness of time, it leaves us as ignorant as ever we were, or perhaps, in fancying ourselves wiser, even more ignorant, of the things that are near us and around, — of the brooks that sing to us, the rocks that guard us, and the fields that feed. 6. To-night, therefore, I am here for no other purpose than to ask the simplest questions ; and to win your interest, if it may be, in pleading with our geological teachers for the an- swers which as yet they disdain to give. Here, in your long winding dale of the Kent, — and over the hills, in my little nested dale of the Yew, — will you ask the geologist, with me, to tell us how their pleasant depth was opened for us, and their lovely borders built. For, as yet, this is all that we are told concerning them, by accumulated evidence of geology, as collected in this summary at the end of the first part of Mr. Clifton Ward's volume on the geology of the lakes : — 130 DEUCALION. " The most ancient geologic records in the district indicate marine conditions with a probable proximity of land. Sub- marine volcanoes broke out during the close of this period, followed by an elevation of land, with continued volcanic eruptions, of which perhaps the present site of Keswick was one of the chief centres. Depression of the volcanic district then ensued beneath the sea, with the probable cessation of volcanic activity ; much denudation was effected ; another slight volcanic outburst accompanied the formation of the Coniston Limestone, and then the old deposits of Skiddaw Slate and volcanic material were buried thousands of feet deep beneath strata formed in an upper Silurian sea. Next followed an immensely long period of elevation, accompanied by disturbance and alteration of the rocks, and by a prodigious amount of marine and atmospheric denudation. A subse- quent depression, to a considerable extent, marked the coming on of the Carboniferous epoch, heralded however, in all like- lihood, by a period of more or less intense cold. Then for succeeding ages, the district elevated high above the surround- ing seas of later times, underwent that large amount of sub- aerial denudation which has resulted in the formation of our beautiful English Lake-country." 7. The only sentence in this passage of the smallest service to us, at present, is that stating the large amount of ' sub- aerial denudation ' which formed our beautiful country. Putting the geological language into simple English, that means that your dales and hills were produced by being < rubbed down in the open air/ — rubbed down, that is to say, in the manner in which people are rubbed down after a Turkish bath, so as to have a good deal of their skin taken off them. But observe, it would be just as rational to say that the beauty of the human form was owing to the immemorial and continual use of the flesh-brush, as that we owe the beauty of our mountains to the mere fact of their having been rubbed away. No quantity of stripping or denuding will give beauty when there is none to denude ; — you cannot rub a statue out of a sandbank, or carve the Elgin frieze with rottenstone for a chisel, and chance to drive it. YE WD ALE AND ITS STREAMLETS. 131 8. We have to ask then, first, what material there was here to carve ; and then what sort of chisels, and in what work- man's hand, were used to produce this large piece of precious chasing or embossed work, which we call Cumberland and Weste-more-land. I think we shall get at our subject most clearly, however, by taking a somewhat wider view of it than our own dales permit, and considering what ' sub-aerial denudation ' means, on the surface of the world, instead of in "Westmoreland only. 9. Broadly, therefore, we have, forming a great part of that surface, vast plains or steppes, like the levels of France, and lowlands of England, and prairies of America, composed mostly of horizontal beds of soft stone or gravel. Nobody in general talks of these having been rubbed down ; so little, indeed, that I really do not myself know what the notions of geologists are on the matter. They tell me that some four- and-twenty thousand feet or so of slate — say, four miles thick of slate — must have been taken off the top of Skiddaw to grind that into what it is ; but I don't know in the least how much chalk or freestone they think has been ground off the East Cliff at Brighton, to flatten that into what it is. They tell me that Mont Blanc must have been three times as high as he is now, when God, or the affinity of atoms, first made him ; but give me no idea whatever how much higher the shore of the Adriatic was than it is now, before the lagoon of Venice was rubbed out of it. 10. Collecting and inferring as best I can, it seems to me they mean generally that all the mountains were much higher than they are now, and all the plains lower ; and that what has been scraped off the one has been heaped on to the other : but that is by no means generally so ; and in the de- gree in which it is so, hitherto has been unexplained, and has even the aspect of being inexplicable. I don't know what sort of models of the district you have in the Museum, but the kind commonly sold represent the entire mountain surface merely as so much sandheap washed into gutters. It is totally impossible for your youth, while these false impressions are conveyed by the cheap tricks of 132 DEUCALION. geographical manufacture, to approach the problems of moun- tain form under any sense of their real conditions : while even advanced geologists are too much in the habit of think- ing that every mountain mass may be considered as a heap of homogeneous clay, which some common plough has fretted into similar clods. But even to account for the furrows of a field you must ask for plough and ploughman. How much more to account for the furrows of the adamantine rock. Shall one plough there with oxen ? I will ask you, therefore, to-night, to approach this question in its first and simplest terms, and to examine the edge of the weapon which is supposed to be still at work. The streamlets of the dale seem yet in many places to be excavating their glens as they dash down them, — or deepening the pools under their cascades. Let us in such simple and daily visible matters consider more carefully what are the facts. 11. Towards the end of July, this last summer, I was saun- tering among the fern, beside the bed of the Yewdale stream, and stopped, as one does instinctively, at a place where the stream stopped also, — bending itself round in a quiet brown eddy under the root of an oak tree. How many thousand thousand times have I not stopped to look down into the pools of a mountain stream, — and yet never till that day had it occurred to me to ask how the pools came there. As a matter of course, I had always said to myself, there must be deep places and shallow ones, — and where the water is deep there is an eddy, and where it is shallow there is a ripple, — and what more is there to say about it? However, that day, having been of late in an interrogative humour about everything, it did suddenly occur to me to ask why the water should be deep there, more than anywhere else. This pool was at a bend of the stream, and rather a wide part of it ; and it seemed to me that, for the most part, of the deep pools I recollected had been at bends of streams, and in rather wide parts of them ; — with the accompanying condition of slow circular motion in the water ; and also, mostly under steep banks. YE WD ALE AND ITS STREAMLETS. 133 12. Gathering my fifty years' experience of brooks, this seemed to me a tenable generalization, that on the whole, where the bank was steepest, and one was most likely to tum- ble in, one was least likely to get out again. And that gloomily slow and sullen motion on the surface, as if the bubbles were unwillingly going round in a mill, — this also I recollected as a usual condition of the deeper water, — so usual, indeed, that (as I say) I never once before had reflected upon it as the least odd. Whereas now, the thought struck me as I looked, and struck me harder as I looked longer, If the bubbles stay at the top, why don't the stones stay at the bottom ? If, when I throw in a stick here in the back eddy at the surface, it keeps spinning slowly round and round, and never goes down-stream — am I to expect that when I throw a stone into the same eddy, it will be immediately lifted by it out of the hole and carried away ? And yet unless the water at the bottom of the hole has this power of lifting stones out of it, why is the hole not filled up ? 13. Coming to this point of the question, I looked up the beck, and down. Up the beck, above the pool, there was a shallow rapid over innumerable stones of all sizes : and down the beck, just below the pool, there was a ledge of rock, against which the stream had deposited a heap of rolled shingle, and over the edges of which it flowed in glittering tricklets, so shallow that a child of four years old might have safely waded across ; and between the loose stones above in the steep rapid, and the ledge of rock below — which seemed put there ex- pressly for them to be lodged against — here was this deep, and wide, and quiet, pool. So I stared at it, and stared ; and the more I stared, the Jess I understood it. And if you like, any of you may easily go and stare too, for the pool in question is visible enough from the coach-road, from Mr. Sly's Waterhead Inn, up to Til- berthwaite. You turn to the right from the bridge at Mr. Bowness's smithy, and then in a quarter of a mile you may look over the roadside wall into this quiet recess of the stream, and consider of many things. For, observe, if there were any- thing out of the way in the pool — I should not send you to 134 DEUCALION. look at it. I mark it only for one of myriads such in every mountain stream that ever trout leaped or ripple laughed in. And beside it, as a type of ail its brother deeps, these fol- lowing questions may be wisely put to yourselves. 14. First— How are any of the pools kept clear in a stream that carries shingle ? There is some power the water has got of lifting it out of the deeps hitherto unexplained — unthought of. Coming down the rapid in a rage, it drops the stones, and leaves them behind ; coming to the deep hole, where it seems to have no motion, it picks them up and carries them away in its pocket. Explain that. 15. But, secondly, beside this pool let us listen to the wide murmuring geological voice, telling us — "To sub-aerial denu- dation you owe your beautiful lake scenery " ! — Then, presum- ably, Yewdale among the rest ? — Therefore we may look upon Yewdale as a dale sub-aerially denuded. That is to say, there was once a time w T hen no dale was there, and the process of denudation has excavated it to the depth you see. 16. But now I can ask, more definitely and clearly, With what chisel has this hollow been hewn for us ? Of course, the geologist replies, by the frost, and the rain, and the decom- position of its rocks. Good ; but though frost may break up, and the rain wash down, there must have been somebody to cart away the rubbish, or still you would have had no Yewdale. Well, of course, again the geologist answers, the streamlets are the carters ; and this stream past Mr. Bow- ness's smithy is carter-in-chief. 17. How many cartloads, then, may we suppose the stream has carried past Mr. Bowness's, before it carted away all Yew- dale to this extent, and cut out all the northern side of Weth- erlam, and all that precipice of Yewdale Crag, and carted all the rubbish first into Coniston Lake, and then out of it again, and so down the Crake into the sea ? Oh, the geologists re- ply, we don't mean that the little Crake did all that. Of course it was a great river full of crocodiles a quarter of a mile long ; or it was a glacier five miles thick, going ten miles an hour ; or a sea of hot water fifty miles deep, — or, — some- thing of that sort. Well, I have no interest, myself, in any* YE WD ALE AND ITS STREAMLETS. 135 thing of that sort : and 1 want to know, here, at the side of my little puzzler of a pool, whether there's any sub-aerial denudation going on still, and whether this visible Crake, though it can only do little, does anything. Is it carrying stones at all, now, past Mr. Bowness's ? Of course, reply the geologists ; don't you see the stones all along it, and doesn't it bring down more every flood ? Well, yes ; the delta of Coniston Waterhead may, perhaps, within the memory of the oldest inhabitant, or within the last hundred years, have ad- vanced a couple of yards or so. At that rate, those two streams, considered as navvies, are proceeding with the works in hand ;— to that extent they are indeed filling up the lake, and to that extent sub-aerially denuding the mountains. But now, I must ask your attention very closely : for I have a strict bit of logic to put before you, which the best I can do will not make clear without some helpful effort on your part. 18. The streams, we say, by little and little, are filling up the lake. They did not cut out the basin of that. Something else must have cut out that, then, before the streams began their work. Could the lake, then, have been cut out all by itself, and none of the valleys that lead to it ? Was it punched into the mass of elevated ground like a long grave, before the streams were set to work to cut Yewdale down to it? 19. You don't for a moment imagine that. Well, then, the lake and the dales that descend with it, must have been cut out together. But if the lake not by the streamlets, then the dales not by the streamlets ? The streamlets are the conse- quence of the dales then, — not the causes ; and the sub-aerial denudation to which you owe your beautiful lake scenery, must have been something, not only different from what is going on now, but, in one half of it at least, contrary to what is going on now. Then, the lakes which are now being filled up, were being cut down ; and as probably, the mountains now being cut down, were being cast up. 20. Don't let us go too fast, however. The streamlets are now, we perceive, filling up the big lake. But are they not, then, also filling up the little ones ? If they don't cut Conis- ton water deeper, do you think they are cutting Mr. Marshall's 136 DEUCALION. tarns deeper ? If not Mr. Marshall's tarns deeper, are they cutting their own little pools deeper ? This pool by which we are standing — we have seen it is inconceivable how it is not filled up, — much more it is inconceivable that it should be cut deeper down. You can't suppose that the same stream which is filling up the Coniston lake below Mr. Browness's, is cutting out another Coniston lake above Mr. Browness's? The truth is that, above the bridge as below it, and from their sources to the sea, the streamlets have the same function, and are filling, not deepening, alike lake, tarn, pool, channel, and valley. 21. And that being so, think how you have been misled by seeking knowledge far afield, and for vanity's sake, instead of close at home, and for love's sake. You must go and see Niagara, must you ? — and you will brick up and make a foul drain of the sweet streamlet that ran past your doors. And all the knowledge of the waters and the earth that God meant for you, flowed with it, as water of life. Understand, then, at least, and at last, to-day, Niagara is a vast Exception — and Deception. The true cataracts and falls of the great mountains, as the dear little cascades and leaplets of your own rills, fall where they fell of old ; — that is to say, wherever there's a hard bed of rock for them to jump over. They don't cut it away — and they can't. They do form pools beneath in a mystic way,— they excavate them to the depth which will break their fall's force— and then they excavate no more.* We must look, then, for some other chisel than the stream- let ; and therefore, as we have hitherto interrogated the waters at their work, we will now interrogate the hills, in their patience. 22. The principal flank of Yewdale is formed by a steep range of crag, thrown out from the greater mass of Wether- lam, and known as Yewdale Crag. It is almost entirely composed of basalt, or hard volcanic ash ; and is of supreme interest among the southern hills of * Else, every pool would become a well, of continually increasing depth. YE WD ALE AND ITS STREAMLETS. 137 the lake district, as being practically the first rise of the great mountains of England, out of the lowlands of England. And it chances that my own study window being just op- posite this crag, and not more than a mile from it as the bird flies, I have it always staring me, as it were, in the face, and asking again and again, when I look up from writing any of my books, — " How did / come here ? " I wrote that last sentence hurriedly, but leave it — as it was written ; for, indeed, however well I know the vanity of it, the question is still sometimes, in spite of my best effort, put to me in that old form by the mocking crags, as by a vast couchant Sphinx, tempting me to vain labour in the inscruta- ble abyss. But as I regain my collected thought, the mocking question ceases, and the divine one forms itself, in the voice of vale and streamlet, and in the shadowy lettering of the engraven rock. " Where wast thou when I laid the foundation of the earth? — declare, if thou hast understanding." 23. How Yewdale Crags came there, I, for one, will no more dream, therefore, of knowing, than the wild grass can know, that shelters in their clefts. I will only to-night ask you to consider one more mystery in the things they have suffered since they came. You might naturally think, following out the idea of 1 sub- aerial denudation 9 that the sudden and steep rise of the crag- above these softer strata was the natural consequence of its greater hardness ; and that in general the district was only the remains of a hard knot or kernel in the substance of the island, from which the softer superincumbent or surrounding material had been more or less rubbed or washed away.* 24. But had that been so, one result of the process must have been certain — that the hard rocks would have resisted * The most wonderful piece of weathering, in all my own district, is on & projecting mass of intensely hard rock on the eastern side of Goat's Water. It was discovered and shown to me by my friend the Rev. F. A. Malleson ; and exactly resembles deer> ripple-marking, though noth- ing in the grain of the rock indicates its undulatory structure, 138 DEUCALION. more than the soft ; and that in some distinct proportion and connection, the hardness of a mountain would be conjecture able from its height, and the whole surface of the district more or less manifestly composed of hard bosses or ridges, with depressions between them in softer materials. Nothing is so common, nothing so clear, as this condition, on a small scale, in every " weathered rock. Its quartz, or other hard knots and veins, stand out from the depressed surface in raised w T alls, like the divisions between the pits of Dante's eighth circle, — and to a certain extent, Mr. Ward tells us, the lava dykes, either by their hardness or by their decomposition, produce walls and trenches in the existing surface of the hills. But these are on so small a scale, that on this map they cannot be discernibly indicated ; and the quite amazing fact stands out here in unqualified and indisputable decision, that by whatever force these forms of your mountains were hewn, it cut through the substance of them, as a sword-stroke through flesh, bone, and marrow, and swept away the masses to be removed, with as serene and indiscriminating power as one of the shot from the Devil's great guns at Shoeburyness goes through the oak and the iron of its target. 25. It is with renewed astonishment, whenever I take these sections into my hand, that I observe the phenomenon itself; and that I remember the persistent silence of geological teachers on this matter, through the last forty years of their various discourse. In this shortened section, through Bow- fell to Brantwood, you go through the summits of three first- rate mountains down to the lowland moors : you find them built, or heaped ; barred, or bedded ; here with forged basalt, harder than flint, and tougher than iron, — there, with shiver- ing shales that split themselves into flakes as fine as puft- paste, and as brittle as shortbread. And behold, the hewing tool of the Master Builder sweeps along the forming lines, and shapes the indented masses of them, as a draper's scis- sors shred a piece of striped sarsnet ! 26. Now do but think a little of the wonderfulness in this. If the process of grinding was slow, why don't the hard rocks project ? If swift, what kind of force must it have been ? and Fig.l. Slates of Bull Cra£ and Maiden Moox. (GEOL^ SURVEY.) Fig. 3. Pie-Pa,ste. Compression modified l)y elevatory forces. Fi£. 4. Pie Paste. Compression, restricted to tine lower Strata under a ri^id upper one. Plate VI. * LATERAL COMPRESSION>OF STRATA Fig.l. Ideal. Figs 2.3 & 4- Practical. YE WD ALE AND ITS STREAMLETS. 139 Why do the rocks it tore show no signs of rending ? Nobody supposes it was indeed swift as a sword or a cannon-ball ; but if not, why are the rocks not broken ? Can you break an oak plank and leave no splinters, or cut a bed of basalt a a thousand feet thick like cream-cheese ? But you suppose the rocks were soft when it was done. Why don't they squeeze, then ? Make Dover cliffs of baker's dough, and put St. Paul's on the top of them, — won't they give way somewhat, think you ? and will you then make Causey Pike of clay, and heave Scaw- fell against the side of it ; and yet shall it not so much as show a bruise ? Yet your modern geologists placidly draw the folded beds of the Skiddaw and Causey Pike slate, first, without observ- ing whether the folds they draw are possible folds in anything ; and, secondly, without the slightest suggestion of sustained pressure, or bruise, in any part of them. 27. I have given in my diagram, (Plate VI, Fig. 1,) the section attributed, in that last issued by the Geological Sur- vey, to the contorted slates of Maiden Moor, between Causey Pike and the erupted masses of the central mountains. Now, for aught I know, those contortions may be truly represented ; —but if so, they are not contortions by lateral pressure. For, first, they are impossible forms in any substance what- ever, capable of being contorted ; and, secondly, they are doubly impossible in any substance capable of being squeezed. Impossible, I say, first in any substance capable of being contorted. Fold paper, cloth, leather, sheets of iron, — what you will, and still you can't have the folded bed at the top double the length of that at the bottom. But here, I have meas- ured the length of the upper bed, as compared with that of the lower, and it is twenty miles, to eight miles and a half. Secondly, I say, these are impossible folds in any substance capable of being squeezed, for every such substance will change its form as well as its direction under pressure. And to show you how such a substance does actually behave, and contort itself under lateral pressure, I have prepared the sec- tions Figures 2, 3, and 4. DEUCALION. 28. I have just said, you have no business to seek knowl- edge far afield, when you can get it at your doors. But more than that, you have no business to go outside your doors for it, when you can get it in your parlour. And it so hap- pens that the two substances which, while the foolish little king was counting out his money, the wise little queen was eating in the parlour, are precisely the two substances be- side which wise little queens and kings, and everybody else, may also think, in the parlour, — Bread, and honey. For whatever bread, or at least dough, will do under pressure, ductile rocks, in their proportion, must also do under pres- sure ; and in the manner that honey will move, poured upon a slice of them, — in that manner, though in its own measure, ice will move, poured upon a bed of them. Eocks, no more than piecrust, can be rolled out without squeezing them thinner ; and flowing ice can no more excavate a valley, than flowing treacle a teaspoon. 29. I said just now, Will you dash Scawfell against Causey Pike? I take, therefore, from the Geological Survey the section of the Skiddaw slates, which continue the mass of Causey Pike under the Vale of Newlands, to the point where the volcanic mass of the Scawfell range thrusts itself up against them, and laps over them. They are represented, in the section, as you see, (Plate VI., Fig. 1 ;) and it has always been calmly as- sumed by geologists that these contortions were owing to lateral pressure. But I must beg you to observe that since the uppermost of these beds, if it were straightened out, would be more than twice the length of the lower ones, you could only obtain that elongation by squeezing the upper bed more than the lower, und making it narrower where it is elongated. Now, if this were indeed at the surface of the ground, the geologists might i>ay the upper bed had been thrown up because there was less weight on it. But, by their own accounts, there were five miles thick of rocks on the top of all this when it was bent. So you could not have made one bed tilt up, and another stay down ; and the structure is evidently an impossible one. YE WD ALE AND ITS STREAMLETS. 141 30. Nay, answer the surveyors, impossible or not, it is there, t partly, in pausing, myself doubt its being there. This looks to me an ideal, as well as an impossible, undulation. But if it is indeed truly surveyed, then assuredly, whatever it may be owing to, it is not owing to lateral pressure. That is to say, it may be a crystalline arrangement assumed under pressure, but it is assuredly not a form assumed by ductile substance under mechanical force. Order the cook to roll out half a dozen strips of dough, and to stain three of them with cochineal. Put red and white alternately one above the other. Then press them in any manner you like ; after pressure, a wetted carving knife will give you quite un- questionable sections, and you see the results of three such experiments in the lower figures of the plate. 31. Figure 2 represents the simplest possible case. Three white and three red dough-strips were taken, a red one upper- most, (for the pleasure of painting it afterwards) ! They were left free at the top, enclosed at the sides, and then reduced from a foot to six inches in length, by pressure from the right. The result, you see, is that the lower bed rises into sharpest gables ; the upper ones are rounded softly. But in the geological section it is the upper bed that rises, the lower keeps down ! The second case is much more interesting. The pastes were arranged in the same order, but bent up a little, to begin with, in two places, before applying the pres- sure. The result was, to my own great surprise, that at these points of previous elevation, the lower bed first became quite straight by tension as it rose, and then broke into transverse faults. 32. The third case is the most interesting of all. In this case, a roof of slate was put over the upper bed, allowing it to rise to some extent only, and the pressure was applied to the two lower beds only.* The upper bed of course exuded backwards, giving these fiame-like forms, of which afterwards * Here I had to give the left-hand section, as it came more neatly. The wrinkled mass on the left colored brown represents the pushing piece of wood, at the height to which it was applied. 142 DEVCALIOK I got quite lovely complications by repeated pressures. Thes$ I must reserve for future illustration, concluding to-night, if you will permit me, with a few words of general advice to the younger members of this society, formed as it has been to trace for itself a straight path through the fields of literature, and over the rocks of science. 33. First. — Whenever you write or read English, write it pure, and make it pure if ill written, by avoiding all unnec- essary foreign, especially Greek, forms of words yourself, and translating them when used by others. Above all, make this a practice in science. Great part of the supposed scientific knowledge of the day is simply bad English, and vanishes the moment you translate it. There is a farther very practical reason for avoiding all vulgar Greek-English. Greece is now a kingdom, and will I hope remain one, and its language is now living. The ship- chandler, within six doors of me on the quay at Venice had indeed a small English sign — calling himself Ship-Chandler ; but he had a large and practically more serviceable, Greek one, calling himself a " TrpofjurjOtTTrjs twv ttXohdv." Now when the Greeks want a little of your science, as in very few years they must, if this absurd practice of using foreign languages for the clarification of scientific principle still holds, what you, in compliment to Greece, call a ( Dinotherium,' Greece, in compliment to you, must call a £ Nastybeastium,' — and you know that interchange of compliments can't last long. 34. II. Observe generally that all knowledge, little or much, is dangerous, in which your progress is likely to be broken short by any strict limit set to the powers of mortals : while it is precisely that kind of knowledge which provokes vulgar curiosity, because it seems so far away ; and idle am- bition, because it allows any quantity of speculation, without proof. And the fact is that the greater quantity of the knowledge which modern science is so saucy about, is only an asses' bridge, which the asses all stop at the top of, and which, moreover, they can't help stopping at the top of ; for they have from the beginning taken the wrong road, and so come to a broken bridge — a Ponte Kotto over the River of YE WD ALE AND ITS STREAMLETS. 143 Death, by which the Pontifex Maximus allows them to pasa no step farther. 35. For instance, — having invented telescopes and photog- raphy, you are all stuck up on your hobby-horses, because you know how big the moon is, and can get pictures of the volcanoes in it ! But you never can get any more than pictures of these, while in your own planet there are a thousand volcanoes which you may jump into, if you have a mind to ; and may one day perhaps be blown sky high by, whether you have a mind or not. The last time the great volcano in Java was in erup- tion, it threw out a stream of hot water as big as Lancaster Bay, and boiled twelve thousand people. That's what I call a volcano to be interested about, if you want sensational science. 36. But if not, and you can be content in the wonder and the power of Nature, without her terror, — here is a little bit of a volcano, close at your very doors — Yewdale Crag, which I think will be quiet for our time, — and on which the anagallis tenella, and the golden potentilla, and the sundew, grow together among the dewy moss in peace. And on the cellular surface of one of the blocks of it, you may find more beauty, and learn more precious things, than with telescope or pho- tograph from all the moons in the milky way, though every drop of it were another solar system. I have a few more serious words to say to the fathers, and mothers, and masters, who have honored me with their pres- ence this evening, with respect to the influence of these far- reaching sciences on the temper of children. 37. Those parents who love their children most tenderly, cannot but sometimes dwell on the old Christian fancy, that they have guardian angels. I call it an old fancy, in defer- ence to your modern enlightenment in religion ; but I assure you nevertheless, in spite of all that illumination, there re- mains yet some dark possibility that the old fancy may be true : and that, although the modern apothecary cannot ex- hibit to you either an angel, or an imp, in a bottle, the spiritual Dowers of heaven and bell are no less now 3 than 144 DEUCALION. heretofore, contending for the souls of your children ; and contending with you — for the privilege of their tutorship. 88. Forgive me if I use, for the few minutes I have yet to speak to you, the ancient language, — metaphorical, if you will, of Luther and Fenelon, of Dante and Milton, of Goethe and Shakspeare, of St. John and St. Paul, rather than your modern metaphysical or scientific slang : and if I tell you, what in the issue of it you will find is either life-giving, or deadly, fact, — that the fiends and the angels contend with you daily for the spirits of your children : the devil using to you his old, his hitherto immortal, bribes, of lust and pride ; and the angels pleading with you, still, that they may be allowed to lead your babes in the divine life of the pure and the lowly. To enrage their lusts, and chiefly the vilest lust of money, the devils would drag them to the classes that teach them how to get on in the world ; and for the better pluming of their pride, provoke their zeal in the sciences which will assure them of their being no God in nature but the gas of their own graves. And of these powers you may discern the one from the other by a vivid, instant, practical test. The devils always will exhibit to you what is loathsome, ugly, and, above all, dead ; and the angels, what is pure, beautiful, and, above all, living. 39. Take an actual, literal instance. Of all kiiown quadru- peds, the unhappiest and vilest, yet alive, is the uloth, having this farther strange devilry in him, that what activity he is capable of, is in storm, and in the night. Well, the devil takes up this creature, and makes a monster of it, — gives it legs as big as hogsheads, claws stretched like the roots of a tree, shoulders like a hump of crag, and a skull as thick as a paving-stone. From this nightmare monster he takes what poor faculty of motion the creature, though wretched, has in its minuter size ; and shows you, instead of the clinging climber that scratched and scrambled from branch to branch among the rattling trees as they bowed in storm, only a vast heap of stony bones and staggering clay, that drags its meat down to its mouth out of the forest ruin. This creature the YE WD ALE AND ITS STREAMLETS. 145 fiends delight to exhibit to you, but are permitted by the nobler powers only to exhibit to you in its death.* 40. On the other hand, as of all quadrupeds there is none so ugly or so miserable as the sloth, so, take him for all in all, there is none so beautiful, so happy, so wonderful as the squirrel. Innocent in all his ways, harmless in his food, play- ful as a kitten, but without cruelty, and surpassing the fan- tastic dexterity of the monkey, with the grace and the bright- ness of a bird, the little dark-eyed miracle of the forest * The Mylodon. An old sketch, (I think, one of Leech's) in Punch, of Paterfamilias improving Master Tom s mind among the models on the mud-bank of the lowest pond at Sydenham, went to the root of the matter. For the effect, on Master Tom's mind of the living squirrel, compare the following account of the most approved modes of squirrel- hunting, by a clerical patron of the sport, extracted for me by a cor- respondent, from 'Rabbits: how to rear and manage them; with Chapters on Hares, Squirrels, etc.' S. O. Beefcon, 248, Strand, W. C. " It may be easily imagined that a creature whose playground is the top twigs of tall trees, where no human climber dare venture, is by no means easy to capture — especially as its hearing is keen, and its vision remarkably acute. Still, among boys living in the vicinity of large woods and copses, squirrel-hunting is a favorite diversion, and none the less so because it is seldom attended by success. 1 The only plan.* says the Rev. Mr. Wood, ' is to watch the animal until it has ascended an isolated tree, or, by a well-directed shower missiles, to drive it into such a place of refuge, and then to form a ring round the tree so as to intercept the squirrel, should it try to escape by leaping to the ground and running to another tree. The best climber is then sent in chase of the squirrel, and endeavours, by violently shaking the branches, to force the little animal to loose its hold and fall to the earth. But it is by no means an easy matter to shake a squirrel from a branch, especially as the little creature takes refuge on the topmost and most slender boughs, which even bend under the weight of its own small body, and can in no way be trusted with the weight of a human being. By dint, how- ever, of perseverance, the squirrel is at last dislodged, and comes to th<» ground as lightly as a snow-flake. Hats, caps, sticks, and all available missiles are immediately flung at the luckless animal as soon as it touches the ground, and it is very probably struck and overwhelmed by a cap. The successful hurler flings himself upon the cap, and tries to seize the squirrel as it lies under his property. All his companions gather round him, and great is the disappointment to find the cap empty, and to see the squirrel triumphantly scampering up some tree where ft would be useless to follow it.' " 146 DEUCALION. glances from branch to branch more like a sunbeam than a living creature : it leaps, and darts, and twines, where it will ; — a chamois is slow to it ; and a panther, clumsy : grotesque as a gnome, gentle as a fairy, delicate as the silken plumes of the rush, beautiful and strong like the spiral of a fern, — it haunts you, listens for you, hides from you, looks for you, loves you, as if the angel that walks with your children had made it himself for their heavenly plaything. And this is what you do, to thwart alike your child's angel, and his God, — you take him out of the woods into the town, — you send him from modest labour to competitive schooling, — you force him out of the fresh air into the dusty bone- house, — you show him the skeleton of the dead monster, and make him pore over its rotten cells and wire-stitched joints, and vile extinct capacities of destruction, — and when he is choked and sickened with useless horror and putrid air, you let him — regretting the waste of time — go out for once to play again by the woodside ; — and the first squirrel he sees, he throws a stone at ! Carry, then, I beseech you, this assured truth away with you to-night. All true science begins in the love, not the dis- section, of your fellow-creatures ; and it ends in the love, not the analysis, of God. Your alphabet of science is in the nearest knowledge, as your alphabet of science is in the near- est duty. " Behold, it is nigh thee, even at the doors." The Spirit of God is around you in the air that you breathe, — His glory in the light that you see ; and in the fruitfulness of the earth, and the joy of its creatures, He has written for you, day by day, His revelation, as He has granted you, day by day, your daily bread. CHAPTER XIII OF STELLAR SILICA. 1. The issue of this number of Deucalion has been so long delayed, first by other work, and recently by my illness, that 1 think it best at once to begin Mr. Ward's notes on Plate V. ; OF STELLAR SILICA. 147 reserving their close, with full explanation of their importance and bearing, to the next following number. Greta Bank Cottage, Keswick, June 13, 1876. My dear Sir, — I send you a few notes on the microscopic structure of the three specimens I have had cut. In them I have stated merely what I have seen. There has been much which I did not expect, and still more is there that I don't understand. I am particularly sorry I have not the time to send a whole series of coloured drawings illustrating the various points ; but this summer weather claims my time on the mountain- side, and I must give up microscopic work until winter comes round again. The minute spherulitic structure — especially along the fine brown lines — was quite a surprise, and I shall hope on some future occasion to see more of this subject. Believe me, yours very truly, J. Clifton Ward. P.S. — There seems to be a great difference between the microscopic structure of the specimens now examined and that of the filled-up vesicles in many of my old lavas here, so far as my limited examination has gone. specimen a. No. 1 commences at the end of the section farthest from A in specimen. 1. Transparent zone with irregular curious cavities (not liquid), and a few mossy-looking round spots (brownish). Polarization. Indicating an indefinite semi-crystalline struct- ure. (See note at page 148.) 2. Zone with minute seed -like bodies of various sizes (nar- row brownish bands in the specimen of darker and lighter tints). a. Many cavities, and of an indefinite oval form in general. b. The large spherulites (2) are very beautiful, the outer 148 DEUCALION. zone (radiate) of a delicate greenish-yellow, the nucleus of $ brownish-yellow, and the intermediate zone generally clear. c. A layer of densely packed bodies, oblong or oval in form. d. Spherulites generally similar to b, but smaller, much more stained of a brownish-yellow, and with more defined nuclei. Polarization. The spherulites show a clearly radiate polari- zation, with rotation of a dark cross on turning either of the prisms ; the intermediate ground shows the irregular semi- crystalline structure. 3. Clear zone, with little yellowish, dark, squarish specks. Polarization. Irregular, semi-crystalline. 4. Row of closely touching spherulites with large nucleus and defined margin, rather furry in character (3). Margins and nuclei brown ; intermediate space brownish-yellow. Polarization. Eadiate, as in the spherulites 2 b. (This is a short brown band which does not extend down through the whole thickness of the specimen.) 5. Generally clear ground, with a brownish cloudy appear- ance in parts. Polarization, Indefinite semi-crystalline. 6 a. On a hazy ground may be seen the cloudy margins of separately crystalline spaces. Polarization. Definite semi-crystalline.** 6 b. A clear band with very indefinite polarization. 7. A clearish zone with somewhat of a brown mottled ap- pearance (light clouds of brown colouring matter). Polarization. Indefinite semi-crystalline. 8. Zone of brownish bodies (this is a fine brown line, about the middle of the section in the specimen). * By 1 indefinite semi-crystalline ' is meant the breaking up of the ground under crossed prisms with sheaves (5) of various colours not clearly margined. By ' definite semi-crystalline ' is meant the breaking up &f the ground under crossed prisms with a mosaic (4) of various colours clearly mar- gined. By ' semi-crystalline ' is meant the interference of crystalline spaces with one another, so as to prevent a perfect crystalline form being assumed. OF STELLAR SILICA. 149 a. Yellowish-brown nucleated disks. b. Smaller, scattered, and generally non-nucleated disks. c. Generally non-nucleated. Polarization. The disks are too minute to show separate polarization effects, but the ground exhibits the indefinite semi-crystalline. 9. Ground showing indefinite semi-crystalline polarization. 10. Irregular line of furry-looking yellowish disks. 11. Zone traversed by a series of generally parallel and faint lines of a brownish-yellow. These are apparently lines produced by colouring matter alone, — at any rate, not by visible disks of any kind. Polarization. Tolerably definite, and limited by the cross lines (6). 12. Dark-brown flocculent-looking matter, as if growing out from a well-defined line, looking like a moss-growth. 13. Defined crystalline interlocked spaces. Polarization. Definite semi-crystalline. 14. Generally, not clearly defined spaces ; central part rather a granular look (spaces very small). Polarization. Under crossed prisms breaking up into toler- ably definite semi-crystalline spaces. SPECIMEN B. B 1. In the slice taken from this side there seems to be frequently a great tendency to spherulitic arrangement, as shown by the polarization phenomena. In parts of the white quartz where the polarization appearance is like that of a mosaic pavement, there is even a semi-spherulitic structure. In other parts there are many spherulites on white and yel- lowish ground. Between the many parallel lines of a yellowish colour the polarization (7) effect is that of fibrous coloured sheaves. Here (8) there is a central clear band (b) ; between it and (a) a fine granular line with some larger granules (or very minute spherulites). The part (a) is carious, apparently with g}f$s cavities. On the other side of the clear band, at c, are half- formed and adherent spherulites ; the central (shaded) parts 150 DEUCALION. are yellow, and the outer coat, the intermediate portion clearish. B 2. The slice from this end of the specimen shows the same general structure. The general tendency to spherulitic arrangement is well seen in polarized light, dark crosses frequently traversing the curved structures. Here (in Fig. 9) the portion represented on the left was situated close to the other portion, where the point of the arrow terminates, both crosses appearing together and revolv- ing in rotation of one of the prisms. specimen c. The slice from this specimen presents far less variety than in the other cases. There are two sets of structural lines — those radiate (10), and those curved and circumferential (11). The latter structure is exceedingly fine and delicate, and not readily seen, even with a high power, owing to the fine radii not being marked out by any colour, the whole section being very clear and white. A more decidedly nucleated structure is seen in part 12. In (13) is a very curious example of a somewhat more glassy portion protruding in finger-like masses into a radiate, clear, and largely spherical portion. 2. These notes of Mr. Clifton Ward's contain the first ac- curate statements yet laid before mineralogists respecting the stellar crystallization of silica, although that mode of ita formation lies at the very root of the structure of the greater mass of amygdaloidal rocks, and of all the most beautiful phenomena of agates. And indeed I have no words to express the wonder with which I see work like that done by Cloize- aux in the measurement of quartz angles, conclude only in the construction of the marvellous diagram, as subtle in exe- cution as amazing in its accumulated facts,* without the least reference to the conditions of varying energy which produce the spherical masses of chalcedony ! He does not even use the classic name of the mineral, but coins the useless one, Gey- * Facing page 8 of the 'Manuel de Mineralogie. ' OF STELLAR SILICA. 151 serite, for the absolutely local condition of the Iceland sinter. 3. And although, in that formation, he went so near the edge of Mr. Clifton Ward's discovery as to announce that " leur masse se compose ellememe de spheres enchassees dans une sorte de pate gelatin euse," he not only fails, on this sug- gestion, to examine chalcedonic structure generally, but ar- rested himself finally in the pursuit of his inquiry by quietly asserting, "ce genre de structure n'a jamais ete recontre jus- qu'ici sur aucune autre variete de silice naturelle ou artifici- elle," — the fact being that there is no chalcedonic mass whatever, which does not consist of spherical concretions more or less perfect, enclosed in a " pate gelatineuse." 4. In Professor Miller's manual, which was the basis of Cloizeaux's, chalcedony is stated to appear to be a mixture of amorphous with crystalline silica ! and its form taken no ac- count of. Malachite might just as well have been described as a mixture of amorphous with crystalline carbonate of copper ! 5. I will not, however, attempt to proceed farther in this difficult subject until Mr. Clifton Ward has time to continue his own observations. Perhaps I may persuade him to let me have a connected series of figured examples, from pure stellar quartz down to entirely fluent chalcedony, to begin the next volume of Deucalion with ; — but I must endeav- our, in closing the present one, to give some available sum- mary of its contents, and clearer idea of its purpose ; and will only trespass so far on my friend's province as to lay before him, together with my readers, some points noted lately on another kind of semi-crystallization, which bear not merely on the domes of delicate chalcedony, and pyramids of microscopic quartz, but on the far-seen chalcedony of the Dome du Goute, and the prismatic towers of the Cervin and dark peak of Aar. 152 DEUCALION. CHAPTER XIV. SCHISMA MONTI UM. 1. The index closing this volume of Deucalion, drawn up by myself, is made as short as possible, and classifies the con- tents of the volume so as to enable the reader to collect all notices of importance relating to any one subject, and to col- late them with those in my former writings. That they need such assemblage from their desultory occurrence in the previ- ous pages, is matter of sincere regret to me, but inevitable, since the writing of a systematic treatise was incompatible with the more serious work I had in hand, on greater subjects. The f Laws of Fesole ' alone might well occupy all the hours I can now permit myself in severe thought. But any student of intelligence may perceive that one inherent cause of the divided character of this book, is its function of advance in parallel columns over a wide field ; seeing that, on no fewer than four subjects, respecting which geological theories and assertions have long been alike fantastic and daring, it has shown at least the necessity for revisal of evidence, and, in two cases, for reversal of judgment. 2. I say " it has shown," fearlessly ; for at my time of life, every man of ordinary sense, and probity, knows what he has done securely, and what perishabl} r . And during the last twenty years, none of my words have been set down untried ; nor has any opponent succeeded in overthrowing a single sen- tence of them. 3. But respecting the four subjects above alluded to. (denu- dation, cleavage, crystallization, and elevation, as causes of mountain form,) proofs of the uncertainty, or even falseness, of current conceptions have been scattered at intervals through my writings, early and late, from ' Modern Painters ' to the ' Ethics of the Dust : ' and, with gradually increasing wonder at the fury of so-called ' scientific ' speculation, I have insisted, year by year, on the undeait with, and usually undreamt of, 8CII1SMA MONTIUM. 153 difficulties which lay at the threshold of secure knowledge in such matters ; — trusting always that some ingenuous young reader would take up the work I had no proper time for, and follow out the investigations of which the necessity had been indicated. But I waited in vain ; and the rough experiments made at last by myself, a year ago, of which the results are represented in Plate VI. of this volume, are actually the first of which there is record in the annals of geology, made to as- certain the primary physical conditions regulating the forms of contorted strata. The leisure granted me, unhappily, by the illness which has closed my relations with the University of Oxford, has permitted the pursuit of these experiments a little farther ; but I must defer account of their results to the fol- lowing volume, contenting myself with indicating, for conclu- sion of the present one, to what points of doubt in existing theories they have been chiefly directed. 4. From the examination of all mountain ground hitherto well gone over, one general conclusion has been derived, that wherever there are high mountains, there are hard rocks. Earth, at its strongest, has difficulty in sustaining itself above the clouds ; and could not hold itself in any noble height, if knitted infirmly. 5. And it has farther followed, in evidence, that on the flanks of these harder rocks, there are yielding beds, which appear to have been, in some places, compressed by them into wrinkles and undulations ; — in others, shattered, and thrown up or down to different levels. My own interest was excited, very early in life,* by the forms and fractures in the mountain groups of Savoy ; and it happens that the undulatory action of the limestone beds on each shore of the Lake of Annecy, * I well yet remember my father's rushing up to the drawing-room at Heme Hill, with wet and flashing eyes, with the proof in his hand of the first sentences of his son's writing ever set in type, — * Enquiries on the Causes of the Colour of the Water of the Rhone,' (Magazine of Natu- ral History, September, 1834 ; followed next month by ' Facts and Considerations on the Strata of Mont Blanc, and on some Instances of Twisted Strata observable in Switzerland.' I was then fifteen.) M^ mother and I eagerly questioning the cause of his excitement, — u It's-~ it's — only $Hkt" said he ! Alas ! how much the ■ only ' meant ! 154 DEUCALION. and the final rupture of their outmost wave into the precipice of the Saleve, present examples so clear, and so imposing, of each condition of form, that I have been led, without there- fore laying claim to any special sagacity, at least into clearer power of putting essential questions respecting such phenom- ena than geologists of far wider experience, who have confused or amused themselves by collecting facts indiscriminately over vast spaces of ground. I am well convinced that the reader will find more profit in following my restricted steps ; and satisfying, or dissatisfying himself, with precision, respecting forms of mountains which he can repeatedly and exhaustively examine. 6. In the uppermost figure in Plate VII., I have enlarged and coloured the general section given rudely above in Figure 1, page 12, of the Jura and Alps, with the intervening plain. The central figure is the southern, and the lowermost figure, which should be conceived as joining it on the right hand, the northern, series of the rocks composing our own Lake dis- trict, drawn for me with extreme care by the late Professor Phillips, of Oxford. I compare, and oppose, these two sections, for the sake of fixing in the reader's mind one essential point of difference among many resemblances ; but that they may not, in this comparison, induce any false impressions, the system of col- our which I adopt in this plate, and henceforward shall ob- serve, must be accurately understood. 7. At pages 93-94 above, I gave my reasons for making no endeavour, at the Sheffield Museum, to certify the ages of rocks. For the same reason, in practical sections I concern myself only with their nature and position ; and colour granite pink, slate purple, and sandstone red, without inquir- ing whether the granite is ancient or modern, — the sand triaa or pliocene, and the slate Wenlock or Caradoc ; but with this much only of necessary concession to recognized method, as to colour with the same tint all rocks which unquestionably belong to the same great geological formation, and vary their mineralogical characters within narrow limits. Thus, since, in characteristic English sections, chalk may most convert 8CH18MA MONTIUM. 155 iently be expressed by leaving it white, and some of the upper beds of the Alps unquestionably are of the same pe- riod, I leave them white also, though their general colour may be brown or grey, so long as they retain cretaceous or marly consistence ; but if they become metamorphic, and change into clay slate or gneiss, I colour them purple, what- ever their historical relations may be. 8. ilnd in all geological maps and sections given in 'Deu- calion,' I shall limit myself to the definition of the twelve fol- lowing formations by the twelve following colours. It is enough for any young student at first to learn the relations of these great orders of rock and earth : — once master of these, in any locality, he may split his beds into any com- plexity of finely laminated chronology he likes ;— and if I have occasion to split them for him myself, I can easily ex- press their minor differences by methods of engraving. But, primarily, let him be content in the recognition of these twelve territories of Demeter, by this following colour her- aldry : — 9. 1. Granite will bear in the field, 2. Gneiss and mica-slate — 3. Clay-slate 4. Mountain limestone 5. Coal measures and millstone grit 6. Jura limestone 7. Chalk 8. Tertiaries forming hard rock 9. Tertiary sands and clays 10. Eruptive rocks, not de- finitely volcanic 11. Eruptive rocks, defi- nitely volcanic, but at rest 12. Volcanic rocks, active Rose-red. Rose-purple. Violet-purple, Blue. Grey. Yellow. White. Scarlet. Tawny. Green. Green, spotted red. Black, spotted red. 10. It will at once be seen by readers of some geological experience, that approximately, and to the degree possible, 150 DEUCALION-. these colours are really characteristic of the several forma* tions ; and they may be rendered more so by a little care in modifying the tints. Thus the 'scarlet' used for the tertia- ries may be subdued as much as we please, to what will be as near a sober brown as we can venture without confusing it with the darker shades of yellow ; and it may be used more pare to represent definitely red sandstones or conglomerates : while, again, the old red sands of the coal measures may be extricated from the general grey by a tint of vermilion which will associate them, as mineral substances, with more recent sand. Thus in the midmost section of Plate VII. this colour is used for the old red conglomerates of Kirby Lonsdale. And again, keeping pure light blue for the dated mountain limestones, which are indeed, in their emergence from the crisp turf of their pastures, grey, or even blue in shade, to the eye, a deeper blue may be kept for the dateless limestones which are associated with the metamorphic beds of the Alps ; as for my own Coniston Silurian limestone, which may be nearly as old as Skiddaw. 11. The colour called c tawny/ I mean to be as nearly that of ripe wheat as may be, indicating arable land, or hot prai- rie ; while, in maps of northern countries, touched with points of green, it may pass for moorland and pasture : or, kept in the hue of pale vermilion, it may equally well repre- sent desert alluvial sand. Finally, the avoidance of the large masses of fierce and frightful scarlet which render modern geological maps intolerable to a painter's sight, (besides in- volving such geographical incongruities as the showing Ice- land in the colour of a red-hot coal ;) and the substitution over all volcanic districts, of the colour of real greenstone, or serpentine, for one which resembles neither these, nor the general tones of dark colour either in lava or cinders, will certainly render all geological study less injurious to the eye- sight, and less harmful to the taste. 12. Of the two sections in Plate VII., the upper one is ar- ranged from Stucler, so as to exhibit in one view the principal phenomena of Alpine structure according to that geologist. The cleavages in the central granite mass are given 3 however SCHISM A MONTI UM. 157 on my own responsibility, not his. The lower section was, as aforesaid, drawn for me by my kind old friend Professor Phillips, and is, I doubt not, entirely authoritative. In all great respects, the sections given by Studer are no less so ; but they are much ruder in drawing, and can be received only as imperfect summaries — perhaps, in their abstraction, occasionally involving some misrepresentation of the complex facts. For my present purposes, however, they give me all the data required. 13. It will instantly be seen, on comparing the two groups of rocks, that although nearly similar in succession, and both suggesting the eruptive and elevatory force of the granitic central masses, there is a wdde difference in the manner of the action of these on the strata lifted by them. In the Swiss section, the softer rocks seem to have been crushed aside, like the ripples of water round any submersed object rising to the surface. In the English section, they seem to have undergone no such torsion, but to be lifted straight, as they lay, like the timbers of a gabled roof. It is true that, on the larger scale of the Geological Survey, contortions are shown at most of the faults in the Skiddaw slate ; but, for the reasons already stated, I believe these contortions to be more or less conven- tionally represented ; and until I have myself examined them, will not modify Professor Phillips 1 drawing by their intro- duction. Some acknowledgment of such a structure is indeed given by him observably in the dark slates on the left in the lower- most section ; but he has written under these undulatory lines " quartz veins," and certainly means them, so far as they are structural, to stand only for ordinary gneissitic contortion in the laminated mass, and not for undulating strata. 14. Farther. No authority is given me by Studer for dividing the undulatory masses of the outer Alps by any kind of cleavage-lines. Nor do I myself know examples of fissile structure in any of these mountain masses, unless where they are affected by distinctly metamorphic action, in the neigh- bourhood of the central gneiss or mica-schist. On the con- trary, the entire courses of the Cumberland rock, from Kirby 158 DEUCALION. Lonsdale to Carlisle, are represented by Professor Phillips as traversed by a perfectly definite and consistent cleavage throughout, dipping steeply south, in accurately straight par- allel lines, and modified only, in the eruptive masses, by a vertical cleavage, characterizing the pure granite centres, 15. I wish the reader to note this with especial care, be- cause the cleavage of secondary rock has been lately attrib- uted, with more appearance of reason than modern scientific theories usually possess, to lateral pressure, acting in a direc- tion perpendicular to the lamination. It seems, however, little calculated to strengthen our confidence in such an explanation, to fiud the Swiss rocks, which appear to have been subjected to a force capable of doubling up leagues of them backwards and forwards like a folded map, wholly without any resultant schistose structure ; and the English rocks, which seem only to have been lifted as a raft is raised on a wave, split across, for fifty miles in succession, by foliate structures of the most perfect smoothness and precision. 16. It might indeed be alleged, in deprecation of this ob- jection, that the dough or batter of which the Alps were com- posed, mostly calcareous, did not lend itself kindly to lamina- tion, while the mud and volcanic ashes of Cumberland were of a slippery and unctuous character, easily susceptible of re- arrangement under pressure. And this view receives strong support from the dextrous experiment performed by Professor Tyndall in 1856, and recorded, as conclusive, in 1872,* where- in, first warming some wax, then pressing it between two pieces of glass, and finally freezing it, he finds the congealed mass delicately laminated ; and attributes its lamination to the " lateral sliding of the particles over each other." * But with his usual, and quite unrivalled, incapacity of following out any subject on the two sides of it, he never tells us, and never seems to have asked himself, how far the wax was flat- tened, and how far, therefore, its particles had been forced to slide ; — nor, during the sixteen years between his first and final record of the experiment, does he seem ever to have used * « Forms of Water,' King and Co., 1872, p. 190. SCHISMA MONTIUM. 159 any means of ascertaining whether, under the observed con- ditions, real compression of the substance of the wax had taken place at all ! For if not, and the form of the mass was only altered from a lump to a plate, without any increase of its density, a less period for reflection than sixteen years might surely have suggested to Professor Tyndall the necessity, in applying his result to geological matters, of providing moun- tains which were to be squeezed m one direction, with room for expansion in another. 17. For once, however, Professor Tyndall is not without fellowship in his hesitation to follow the full circumference of this question. Among the thousands of passages I have read in the works even of the most careful and logical geolo- gists, — even such as Humboldt and De Saussure, — I remem- ber not one distinct statement * of the degree in which they supposed the lamination of any given rock to imply real in- crease of its density, or only the lateral extension of its mass. 18. And the student must observe that in many cases lateral extension of mass is precisely avoided by the very positions of rocks which are supposed to indicate the pressure * As these sheets are passing through the press, I receive the follow- ing most important note from Mr. Clifton Ward : ' ' With regard to the question whether cleavage is necessarily followed by a reduction in hulk of the body cleaved, the following cases may help us to form an opinion. Crystalline volcanic rocks (commonly called trap), as a rule, are not cleaved, though the beds, uncrystalline in character, above and below them, may be. When, however, a trap is highly vesicular, it is sometimes well cleaved. May we not, therefore, suppose that in a rock, wholly crystalline, the particles are too much interlocked to take up new positions ? In a purely fragmentary rock, however, the particles seem to have more freedom of motion ; their motion under pressure leads to a new and more parallel arrangement of particles, each being slightly flattened or pulled out along the planes of new arrangement. This, then, points to a diminution of bulk at any rate in a direction at right angles to the planes of cleavage. The tendency to new arrangement of particles under pressure poin ts to accommodation under altered circum- stances of space. In rocks composed of fragments, the interspaces, being for the most part larger than the intercrystalline spaces of a trap rock, more freely allow of movement and new arrangement." 160 DEUCALION. sustained. In Mr. Woodward's experiment with sheets o! paper, for instance, (above quoted, p. 16,*) there is neither increase of density nor extension of mass, in the sheets of paper. They remain just as thick as they were, — just as long and broad as they were. They are only altered in direction, and no more compressed, as they bend, than a flag is com- pressed by the wind that waves it. In my own experiments with dough, of course the dough was no more compressible than so much water would have been. Yet the language of the geologists who attribute cleavage to pressure might usu- ally leave their readers in the notion that clay can be re- duced like steam ; and that we could squeeze the sea down to half its depth by first mixing mud with it ! Else, if they really comprehended the changes of form rendered necessary by proved directions of pressure, and did indeed mean that the paste of primitive slate had been ' flattened out \ (in Pro- fessor Tyndall's words) as a cook flattens out her pastry-crust with a rolling-pin, they would surely sometimes have asked themselves, — and occasionally taken the pains to tell their scholars, — where the rocks in question had been flattened to. Yet in the entire series of Swiss sections (upwards of a hundred) given by Studer in his Alpine Geology, there is no hint of such a difficulty having occurred to him ; — none, of his having observed any actual balance between diminution of bulk and alteration of form in contorted beds ; — and none, showing any attempt to distinguish mechanical from crystalline foliation. The cleavages are given rarely in any section, and always imperfectly. 19. In the more limited, but steadier and closer, work of Professor Phillips on the geology of Yorkshire, the solitary notice of "that very obscure subject, the cleavage of slate " is contained in three pages, (5 to 8 of the first chapter,) de- scribing the structure of a single quarry, in which the author does not know, and cannot eventually discover, whether the * There is a double mistake in the thirteenth line from the top in that page. I meant to have written, 4 'from a length of four inches into the length of one inch,"— but I believe the real dimensions should have been " a foot crushed into three inches. " SCHISMA MONTIUM. 161 rock is stratified or not ! I respect, and admire, the frankness of the confession ; but it is evident that before any affirmation of value, respecting cleavages, can be made by good geolo- gists, they must both ascertain many laws of pressure in viscous substances at present unknown ; and describe a great many quarries with no less attention than was given by Pro- fessor Phillips to this single one. 20. The experiment in wax, however, above referred to as ingeniously performed by Professor Tyndall, is not adduced in the "Forms of Water" for elucidation of cleavage in rocks, but of riband structure in ice — (of which more presently). His first display of it, however, was I believe in the lecture delivered in 1856 at the Royal Institution, — this, and the other similar experiments recorded in the Appendix to the ' Glaciers of the Alps/ being then directed mainly to the confusion of Professor Sedgwick, in that the Cambridge geologist had — with caution — expressed an opinion that cleavage was a result of crystallization under polar forces. 21. Of that suggestion Professor Tyndall complimentarily observed that " it was a bold stretch of analogies," and con- descendingly — that "it had its value, — it has drawn attention to the subject. " Presently, translating this too vulgarly in- telligible statement into his own sublime language, he declares of the theory in debate that it, and the like of it, are " a dynamic power wdiich operates against intellectual stagnation." How a dynamic power differs from an undynamic one, — (and, presumably, also, a potestatic dynamis from an unpotestatic one ;) and how much more scientific it is to say, instead of — that our spoon stirs our porridge, — that it " operates against the stagnation " of our porridge, Professor Tyndall trusts the reader to recognize with admiration. But if any stirring, or skimming, or other operation of a duly dynamic character, could have clarified from its scum of vanity the pease-porridge of his own wits, Professor Tyndall would have felt that men like the Cambridge veteran, — one of the very few modern men of science who possessed real genius, — stretch no analogies farther than they will hold ; and, in this particular case, there were two facts, familiar to Sedgwick, and with which Pro- 102 DEUCALION. fessor Tyndall manifesis no acquaintance, materially affecting every question relating to cleavage structure. 22. The first, that all slates whatever, among the older rocks, are more or less metamorphic ; and that all metamorphism implies the development of crystalline force. Neither the chiastolite in the slate of Skiddaw, nor the kyanite in that of St. Gothard, could have been formed without the exertion, through the whole body of the rock, of crystalline force, which, extracting some of its elements, necessarily modifies the structure of the rest. The second, that slate-quarries of commercial value, fortunately rare among beautiful mountains, owe their utility to the unusual circumstance of cleaving, over the quarry able space, practically in one direction only. But such quarryable spaces extend only across a few fathoms of crag, and the entire mass of the slate mountains of the world is cloven, not in one, but in half a dozen directions, each sep- arate and explicit ; and requiring, for their production on the pressure theory, the application of half a dozen distinct press- ures, of which none shall neutralize the effect of any other ! That six applications of various pressures at various epochs, might produce six cross cleavages, may be conceived without unpardonable rashness, and conceded without perilous cour- tesy ; but before pursuing the investigation of this hexfoiled subject, it would be well to ascertain w T hether the cleavage of any rock w r hatever does indeed accommodate itself to the cal- culable variations of a single pressure, applied at a single time. 23. Whenever a bed of rock is bent, the substance of it on the concave side must be compressed, and the substance of it on the convex side, expanded. The degree in which such change of structure must take place may be studied at ease in one's arm-chair with no more apparatus than a stick of sealing-wax and a candle ; and as soon as I am shown a bent bed of any rock with distinct lamination on its concave side, traceably gradated into distinct crevassing on its convex one, I will admit without farther debate the connection of foliation with pressure. 24. In the meantime, the delicate experiments by the con- SCH1SMA MONTIUM. 1G3 duct of which Professor Tyndall brought his audiences into what he is pleased to call "contact with facts" (in olden times we used to say ' grasp of facts ' ; modern science, for its own part prefers, not unreasonably, the term ' contact,' expressive merely of occasional collision with them,) must remain incon- clusive. But if in the course of his own various ' contact with facts ' Professor Tyndall has ever come across a bed of slate squeezed between tw r o pieces of glass — or anything like them — I will thank him for a description of the locality. All me tani orphic slates have been subjected assuredly to heat — probably to pressure ; but (unless they were merely the shaly portions of a stratified group) the pressure to which they have been subjected was that of an irregular mass of rock ejected in the midst of them, or driven fiercely against them ; and their cleavage — so far as it is indeed produced by that pressure, must be such as the iron of a target shows round a shell ; — and not at all representable by a film of candle-droppings. 25. It is further to be observed, — and not without increas- ing surprise and increasing doubt, — that the experiment was shown, on the first occasion, to explain the lamination of slate, and, on the second, to explain the riband structure of ice. But there are no ribands in slate, and there is no lamination in ice. There are no regulated alternations of porous with solid substance in the one ; and there are no constancies of fracture by plane surfaces in the other ; moreover — and this is to be chiefly noted, — slate lamination is always straight ; glacier banding always bent. The structure of the pressed w r ax might possibly explain one or other of these phenomena ; but could not possibly explain both, and does actually explain neither. 26. That the arrangement of rock substance into fissile folia does indeed take place in metamorphic aluminous masses un- der some manner of pressure, has, I believe, been established by the investigations both of Mr. Sorby and of Mr. Clifton Ward. But the reasons for continuity of parallel cleavage through great extents of variously contorted beds ; — for its al- most uniform assumption of a high angle ; — for its as uniform non-occurrence in horizontal laminae under vertical i>ressure, 164 DEUCALIOK however vast ; — for its total disregard of the forces causing upheaval of the beds ; — and its mysteriously deceptive har- monies with the stratification, if only steep enough, of neigh- bouring sedimentary rocks, remain to this hour, not only un- assigned, but unsought. 27. And it is difficult for me to understand either the con- tentment of geologists with this state of things, or the results on the mind of ingenuous learners, of the partial and more or less contradictory information hitherto obtainable on the subject. The section given in the two low r er figures of Plate VII. was drawn for me, as I have already said, by my most affectionately and reverently remembered friend, Professor Phillips, of Oxford. It goes through the entire crest of the Lake district from Lancaster to Carlisle, the first emergent rock-beds being those of mountain limestone, A to B, not steeply inclined, but lying unconformably on the steeply in- clined flags and grit of Furness Fells, B to C. In the depres- sion at C lies Coniston Lake ; then follow the masses of Con- iston Old Man and Scawfell, C to D, sinking to the basin of Derwentwater just after the junction, at Grange, of their vol- canic ashes with the Skiddaw slate.. Skiddaw himself, and Carrock Fell, rise between D and E ; and above E, at Cald- beck, again the mountain limestone appears in unconformable bedding, declining under the Trias of the plain of Carlisle, at the northern extremity of which a few rippled lines do service for the waves of Solway. 28. The entire ranges of the greater mountains, it will be seen, are thus represented by Professor Phillips as consisting of more or less steeply inclined beds, parallel to those of the Furness shales ; and traversed by occasional cleavages at an opposite angle. But in the section of the Geological Survey, already referred to, the beds parallel to the Furness shales reach only as far as Wetherlam, and the central mountains are represented as laid in horizontal or slightly basin-shaped swirls of ashes, traversed by ejected trap, and divided by no cleavages at all, except a few vertical ones indicative of the Tilberthwaite slate quarries. 29. I think it somewhat hard upon me, now that I am sixty S CIIIS MA MONTIUM. 165 years old, and short of breath in going up hills, to have to compare, verify for myself, and reconcile as I may, these en- tirely adverse representations of the classical mountains of England : — no less than that I am left to carryforward, in my broken leisure, the experiments on viscous motion instituted by James Forbes thirty years ago. For the present, however, I choose Professor Phillips's section as far the most accurately representative of the general aspect of matters, to my present judgment; and hope, with Mr. Clifton Ward's good help, to give more detailed drawings of separate parts in the next vol- ume of Deucalion. 30. I am prepared also to find Professor Phillips's drawing in many respects justifiable, by my own former studies of the cleavage structure of the central Alps, which, in all the cases I have examined, I found to be a distinctly crystalline lami- nation, sometimes contorted according to the rock's own humour, fantastically as Damascus steel ; but presently after- wards assuming inconceivable consistency with the untroubled repose of the sedimentary masses into whose company it had been thrust. The junction of the contorted gneiss through which the gorge of Trient is cleft, with the micaceous marble on which the tower of Martigny is built, is a transition of this kind within reach of the least adventurous traveller ; and the junction of the gneiss of the Montanvert with the porous limestone which underlies it, is certainly the most interesting, and the most easily explored, piece of rock-fellowship in Europe. Yet the gneissitic lamination of the Montanvert has been attributed to stratification by one group of geologists, and to cleavage by another, ever since the valley of Chamouni was first heard of, and the only accurate drawings of the beds hitherto given are those published thirty years ago in 'Modern Painters/ I had hoped at the same time to con- tribute some mite of direct evidence to their elucidation, by sinking a gallery in the soft limestone under the gneiss, sup- posing the upper rock hard enough to form a safe roof ; but a decomposing fragment fell, and so nearly ended the troubles, with the toil, of the old miner who was driving the tunnel, that I attempted no farther inquiries in that practical manner, 166 DEUCALIOJST. 31. The narrow bed, curved like a sickle, and coloured ver- milion, among the purple slate, in the uppermost section oi Plate VII, is intended to represent the position of the sin- gular band of quartzite and mottled schists, ("bunte schie- fer,") which, on the authority of Studer's section at page 178 of his second volume, underlies, at least for some thousands of feet, the granite of the Jungfrau ; and corresponds, in its relation to the uppermost cliff of that mountain, with the subjacence of the limestone of Les Tines to the aiguilles of Chamouni. I have coloured it vermilion in order to connect it in the student's mind with the notable conglomerates of the Black Forest, through which their underlying granites pass into the Trias ; but the reversed position which it here as- sumes, and the relative dominance of the central mass of the Bernese Alps, if given by Studer with fidelity, are certainly the first structural phenomena which the geologists of Ger- many should benevolently qualify themselves to explain to the summer society of Interlachen. The view of the Jungfrau from the Castle of Manfred is probably the most beautiful natural vision in Europe ; but, for all that modern science can hitherto tell us, the construction of it is supernatural, and explicable only by the Witch of the Alps. 32. In the meantime I close this volume of Deucalion by noting firmly one or two letters of the cuneiform language in which the history of that scene has been written. There are five conditions of rock cleavage w T hich the stu- dent must accustom himself to recognize, and hold apart in his mind with perfect clearness, in all study of mountain form. I. The Wave cleavage : that is to say, the condition of structure on a vast scale which has regulated the succession of summits. In almost all chains of mountains not volcanic, if seen from a rightly chosen point, some law of sequence will manifest itself in the arrangement of their eminences. On a small scale, the declining surges of pastoral mountain, from the summit of Helvellyn to the hills above Kendal, seen from any point giving a clear profile of them, on Wetherlam or the Old Man of Coniston, show a quite rhythmic, almost formal, order of ridged waves, with their steepest sides to the low SCHISMA MONTIUM. 167 lands ; for which the cause must be sought in some internal structure of the rocks, utterly untraceable in close section. On vaster scale, the succession of the aiguilles of Chamouni, and of the great central aiguilles themselves, from the dome of Mont Blanc through the Jorasses, to the low peak of the aiguille de Trient, is again regulated by a harmonious law of alternate cleft and crest, which can be studied rightly only from the far-distant Jura. The main directions of this vast mountain tendency might always be shown in a moderately good model of any given district, by merely colouring all slopes of ground inclined at a greater angle than thirty degrees, of some darker colour than the rest. No slope of talus can maintain itself at a higher angle than this, (compare * Modern Painters/ vol. iv., p. 318 ;) and therefore, while the mathematical laws of curva- ture by aqueous denudation, which were first ascertained and systematized by Mr. Alfred Tylor, will be found assuredly to regulate or modify the disposition of masses reaching no steeper angle, the cliffs and banks which exceed it, brought into one abstracted group, will always display the action of the wave cleavage on the body of the yet resisting rocks. 33. II. The Structural cleavage. This is essentially determined by the arrangement of the plates of mica in crystalline rocks, or — where the mica is ob- scurely formed, or replaced by other minerals — by the sinu- osities of their quartz veins. Next to the actual bedding, it is the most important element of form in minor masses of crag ; but in its influence on large contours, subordinate al- ways to the two next following orders of cleavage. 34. IIL The Asphodeline cleavage ; — the detachment, that is to say, of curved masses of crag more or less concentric, like the coats of an onion. It is for the most part transverse to the structural cleavage, and forms rounded domes and bending billows of smooth contour, on the flanks of the great foliated mountains, which look exactly as if they had been worn for ages under some river of colossal strength. It is far and away the most important element of mountain form in granitic and metamorphic districts. 168 DEUCALION. 35. IV. The Frontal cleavage. This shows itself only on the steep escarpments of sedimentary rock, when the cliff has been produced in all probability by rending elevatory force. It occurs on the faces of nearly ail the great precipices in Savoy, formed of Jura limestone, and has been in many cases mis- taken for real bedding. I hold it one of the most fortunate chances attending the acquisition of Brantwood, that I have within three hundred yards of me, as I write, jutting from beneath my garden wall, a piece of crag knit out of the Furness shales, showing frontal cleavage of the most definite kind, and enabling me to examine the conditions of it as per- fectly as I could at Bonneville or Annecy. 36. V. The Atomic cleavage. This is the mechanical fracture of the rock under the hammer, indicating the mode of coherence between its particles, irre- spectively of their crystalline arrangements. The conchoidal fractures of flint and calcite, the raggedly vitreous fractures of quartz and corundum, and the earthy transverse fracture of clay slate, come under this general head. And supposing it proved that slaty lamination is indeed owing either to the lat- eral expansion of the mass under pressure, or to the filling of vacant pores in it by the flattening of particles, such a formation ought to be considered, logically, as the ultimate degree of fineness in the coherence of crushed substance ; and not properly a ' structure/ I should call this, therefore, also an ' atomic ' cleavage. 37. The more or less rectilinear divisions, known as ' joints/ and apparently owing merely to the desiccation or contraction of the rock, are not included in the above list of cleavages, which is limited strictly to the characters of separation in- duced either by arrangements of the crystalline elements, or by violence in the methods of rock elevation or sculpture. 38. If my life is spared, and my purposes hold, the second volume of Deucalion will contain such an account of the hills surrounding me in this district, as shall be, so far as it is car- ried, trustworthy down to the minutest details in the exposi- tion of their first elements of mountain form. And I am even fond enough to hope that some of the youths of Oxford, edu- SCHISMA MONTIUM. 169 cated in its now established schools of Natural History and Art, may so securely and consistently follow out such a piece of home study by the delineation of the greater mountains they are proud to climb, as to redeem, at last, the ingenious nineteenth century from the reproach of having fostered a mountaineering club, which was content to approve itself in competitive agilities, without knowing either how an aiguille stood, or how a glacier flowed ; and a Geological Society, which discoursed with confidence on the catastrophes of chaos, and the processes of creation, without being able to tell a builder how a slate split, or a lapidary how a pebble was coloured, APPENDIX. When I began Deucalion, one of the hopes chiefly connected with it was that of giving some account of the work done by the real masters and fathers of Geology. I must not conclude this first volume without making some reference, (more espe- cially in relation to the subjects of inquiry touched upon in its last chapter,) to the modest life and intelligent labour of a most true pioneer in geological science, Jonathan Otley. Mr. Clifton Ward's sketch of the good guide's life, drawn up in 1877 for the Cumberland Association for the Advancement of Literature and Science, supplies me with the following par- ticulars of it, deeply — as it seems to me — instructive and im- pressive. He was born near Ambleside, at Nook House, in Loughrigg, January 19th, 1766. His father was a basket-maker ; and it is especially interesting to me, in connection with the resolved retention of Latin as one of the chief elements of education in the system I am arranging for St. George's schools, to find that the Westmoreland basket-maker was a good Latin scholar ; and united Oxford and Cambridge discipline for his son with one nobler than either, by making him study Latin and mathematics, while, till he was twenty-five, he worked as his father's journeyman at his father's handicraft. "He also cleaned all the clocks and watches in the neighbourhood, and showed himself very skilful in engraving upon copper-plates, seals and coin." In 1791 he moved to Keswick, and there lived sixty-five years, and died, ninety years old and upwards. I find no notice in Mr. Ward's paper of the death of the father, to whose good sense and firmness the boy owed so much. There was yet a more wof ul reason for his leaving his 172 DEUCALION. birthplace. He was in love with a young woman named Anno Youdale, and had engraved their names together on a silver coin. But the village blacksmith, Mr. Bowness, was also a suitor for the maiden's hand ; and some years after, Jonathan's niece, Mrs. "Wilson, asking him how it was that his name and Anne Youdale's were engraved together on the same coin, he replied, " Oh, the blacksmith beat me." * He never married, but took to mineralogy, watchmaking, and other consolatory pursuits, with mountain rambling — alike discursive and at- tentive. Let me not omit what thanks for friendly help and healthy stimulus to the earnest youth may be due to another honest Cumberland soul, — Mr. Crosthwaite. Otley was stand- ing one day (before he removed to Keswick) outside the Crosthwaite Museum, f when he was accosted by its founder, and asked if he would sell a curious stick he held in his hand. Otley asked a shilling for it, the proprietor of the Museum stipulating to show him the collection over the bargain. From this time congenial tastes drew the two together as firm and staunch friends. He lived all his life at Keswick, in lodgings, — recognized as " Jonathan Otley's, up the steps," — paying from five shil- lings a week at first, to ten, in uttermost luxury ; and being able to give account of his keep to a guinea, up to October 18, 1852, — namely, board and lodging for sixty-one years and one week, £1325 ; rent of room extra, fifty-six years, £164 10a *I doubt tlie orthography of the fickle maid's name, but all authority of antiquaries obliges me to distinguish it from that of the valley. I do so, however, still under protest — as if I were compelled to write Lord Lonsdale, ' Lownsdale,' or the Marquis of Tweeddale, 4 Twaddle,' or the victorious blacksmith, ' Beauness.' The latter's family still retain the forge by Elter Water— an entirely distinct branch, I am told, from our blacksmith's of the Dale : see above, pp. 133, 134. f In that same museum, my first collection of minerals — fifty specimens —total price, if I remember rightly, five shillings— was bought for me, by my father, of Mr. Crosthwaite. No subsequent possession has had so much influence on my life. I studied Turner at his own gallery, and in Mr. Windus's portfolios ; but the little yellow bit of " copper ore from Coniston," and the "Garnets" (I never could see more than one!) from Borrowdale, were the beginning of science to me which never could have been otherwise acquired. APPENDIX. 173 Total keep and roof overhead, for the sixty usefullest of his ninety years, £1489 10s. Thus housed and fed, he became the friend, and often the teacher, of the leading scientific men of his clay, — Dr. Dalton the chemist, Dr. Henry the chemist, Mr. Farey the engineer, Airy the Astronomer Royal, Professor Phillips of Oxford, and Professor Sedgwick of Cambridge. He was the first accurate clescriber and accurate map-maker of the Lake district ; the founder of the geological divisions of its rocks, — which were accepted from him by Sedgwick, and are now finally con- firmed ; — and the first who clearly defined the separation be- tween bedding, cleavage, and joint in rock, — hence my en- forced notice of him, in this place. Mr. Ward's Memoir gives examples of his correspondence with the men of science above named : both Phillips and Sedgwick referring always to him in any question touching Cumberland rocks, and becoming gradually his sincere and affectionate friends. Sedgwick sate by his death-bed. I shall have frequent occasion to refer to his letters, and to avail myself of his work. But that work was chiefly crowned in the example he left — not of what is vulgarly praised as weilt-help, (for every noble spirit's watchword is "God us ayde") — but of the rarest of mortal virtues, self-possession, " In your patience, possess ye your souls." I should have dwelt at greater length on the worthiness both of the tenure and the treasure, but for the bitterness of my conviction that the rage of modern vanity must destroy in our scientific schoolmen, alike the casket, and the possession. DEUCALION. VOL. H. CHAPTEK I LIVING WAVES. 1. The opening of the second volume of Deucalion with a Lecture on Serpents may seem at first a curiously serpentine mode of advance towards the fulfilment of my promise that the said volume should contain an account of the hills sur- rounding me at Coniston, (above, vol. i., p. 168, § 38). But I am obliged now in all things to follow in great part the leadings of circumstance : and although it was only the fortui- tous hearing of a lecture by Professor Huxley which induced me to take up at present the materials I had by me respecting snake motion, I believe my readers will find their study of undulatory forces dealt through the shattered vertebrae of rocks, very materially enlivened, if not aided, by first observ- ing the transitions of it through the adjusted vertebrae of the serpent. I w r ould rather indeed have made this the matter of a detached essay, but my distinct books are far too numerous already ; and, if I could only complete them to my mind, would in the end rather see all of them fitted into one colu- brine chain of consistent strength, than allowed to stand in any broken or diverse relations. There are, however, no indications in the text of the lecture itself of its possible use in my geological work. It was written as briefly and clearly as I could, for its own immediate purpose : and is given here, as it was delivered, with only the insertion of the passages I was forced to omit for want of time. 2. The lecture, as it stands, was, as I have just said, thrown 176 DEUCALION, together out of the materials I had by me ; most of them for a considerable time ; and with the help of such books as I chanced to possess, — chiefly, the last French edition of Cuvier, — Dr. Russell's Indian Serpents, — and Bell's British Reptiles. Not until after the delivery of the lecture for the second time, was I aware of the splendid w r ork done recently by Dr Gun- ther, nor had I ever seen drawings of serpents for a moment comparable, both in action and in detail of scale, to those by Mr. Ford which illustrate Dr. Gunther's descriptions ; or, in colour, and refinement of occasional action, to those given in Dr. Fayrer's Thanatophidia of India. The reader must there- fore understand that anything generally said, in the following lecture, of modern scientific shortcoming, or error, is not to be understood as applying to any publication by either of these two authors, who have, I believe, been the first naturalists to adopt the artistically and mathematically sound method of delineation by plan and profile ; and the first to represent serpent action in true lines, whether of actual curve, or induced perspective. What follows, then, is the text of what I read, or, to the best of my memory, spoke, at the London Institution. 3. In all my lectures on Natural History at Oxford I virtu- ally divided my subject always into three parts, and asked my pupils, first, to consider what had been beautifully thought about the creature ; secondly, what was accurately known of it ; thirdly, what was to be wisely asked about it. First, you observe, what w r as, or had been, beautifully thought about it ; the effect of the creature, that is to say, [luring past ages, on the greatest human minds. This, it is especially the business of a gentleman and a scholar to know. It is a king's business, for instance, to know the meaning of the legend of the basilisk, the King of Serpents, who killed with a look, in order that he may not himself become like a basilisk. But that kind of knowledge would be of small use to a viper-catcher. Then the second part of the animal's history is — what is truly known of it, which one usually finds to be extremely little. LIVING WAVES. 177 And the third part of its history will be — what remains to be asked about it — what it now behoves us, or will be profit- able to us, to discover. 4. It will perhaps be a weight off jour minds to be assured that I shall waive to-night the first part of the subject alto- gether except so far as thoughts of it may be suggested to you by Mr. Severn's beautiful introductory diagram, * and by the references I have to make to it, though shown for the sake of the ivy, not the Eve, — its subject being already explained in my Florentine Guide to the Shepherd's Tower. But I will venture to detain you a few moments while I point out how, in one great department of modern science, past traditions may be used to facilitate, where at present they do but en- cumber, even the materialistic teaching of our own day. 5. When I was furnishing Brantwood, a few years ago, I indulged myself with two bran-new globes, brought up to all the modern fine discoveries. I find, however, that there's so much in them that I can see nothing. The names are too many on the earth, and the stars too crowded in the heaven. And I am going to have made for my Coniston parish school a series of drawings in dark blue, with golden stars, of one constellation at a time, such as my diagram No. 2, with no names written to the stars at all. For if the chil- dren don't know their names without print on their diagram, they won't know them without print on the sky. Then there must be a school-manual of the constellations, which will have the legend of each told as simply as a fairy tale ; and the names of the chief stars given on a map of them, correspond- ing to the blue diagram, — both of course drawn as the stars- are placed in the sky ; or as they would be seen on a concave celestial globe, from the centre of it. The having to look down on the stars from outside of them is a difficult position for children to comprehend, and not a very scientific one, even when comprehended. 6. But to do all this rightly, I must have better outlines than those at present extant. The red diagram, No. 3, which * The Creation of Eve, bas-relief from the tower of Giotto. The photograph may he obtained from Mr, Ward. 178 DEUCALION. has I hope a little amused you, more than frightened, is an enlargement of the outline given on my new celestial globe, to the head of the constellation Draco. I need not tell you that it is as false to nature as it is foolish in art ; and I want you to compare it with the uppermost snake head in No. 4, because the two together will show you in a moment what long chapters of ' Modern Painters ' were written to explain, — how the real faculty of imagination is always true, and goes straight to its mark : but people with no imagination are always false, and blunder or drivel about their mark. That red head was drawn by a man who didn't know a snake from a sausage, and had no more imagination in him than the chopped pork of which it is made. Of course he didn't know that, and with a scrabble of lines this way and the other, gets together what he thinks an invention — a knot of gratui- tous lies, which you contentedly see portrayed as an instrument of your children's daily education. While — two thousand and more years ago — the people who had imagination enough to believe in Gods, saw also faithfully what was to be seen in snakes ; and the Greek workman gives, as you see in this en- largement of the silver drachma of Phsestus, with a group of some six or seven sharp incisions, the half-dead and yet dread- ful eye, the flat brow, the yawning jaw, and the forked tongue, which are an abstract of the serpent tribe for ever and ever. And I certify you that all the exhibitions they could see in all London would not teach your children so much of art as a celestial globe in the nursery, designed with the force and the simplicity of a Greek vase. 7. Now, I have done alike with myths and traditions; and perhaps I had better forewarn yon, in order, what I am next coining to. For, after my first delivery of this lecture, one of my most attentive hearers, and best accustomed pupils, told me that he had felt it to be painfully unconnected, — with much resultant difficulty to the hearer in following its inten- tion. This is partly inevitable when one endeavours to get over a great deal of ground in an hour ; and indeed I have been obliged, as I fastened, the leaves together, to cut out sundry sentences of adaptation or transition— and run my LIVING WAVES. 179 bits of train all into one, without buffers. But the actual di- visions of what I have to say are clearly jointed for all that ; and if you like to jot them down from the leaf I have put here at my side for my own guidance, these are the heads of them : — I. Introduction— Imaginary Serpents. II. The Names of Serpents. III. The Classification of Serpents. IV. The Patterns of Serpents. V. The Motion of Serpents. VI. The Poison of Serpents. VII. Caution, concerning their Poison. VIII. The Wisdom of Serpents. IX. Caution, concerning their Wisdom. It is not quite so bad as the sixteenthly, seventeenthly, and to conclude, of the Duke's chaplain, to Major Dalgetty ; but you see we have no time to round the corners, and must get through our work as straightly as we may. We have got done already with our first article, and begin now with the names of serpents ; of which those used in the great languages, ancient and modern, are all significant, and therefore instructive, in the highest degree. 8. The first and most important is the Greek 'ophis,' from which you know the whole race are called, by scientific people, ophidia. It means the thing that sees all around ; and Milton is thinking of it w r hen he makes the serpent, looking to see if Eve be assailable, say of himself, " Her husband, for I view far round, not near." Satan says that, mind you, in the per- son of the Serpent, to whose faculties, in its form, he has re- duced himself. As an angel, he would have known whether Adam was near or not : in the serpent, he has to look and see. This, mind you further, however, is Miltonic fancy, not Mosaic theology ; — it is a poet and a scholar who speaks here, — by no means a prophet. 9. Practically, it has never seemed to me that a snake could see far round, out of the slit in his eye, which is drawn large 180 DEUCALION. for you in my diagram of the rattlesnake ;* but either he oi the puffadder, I have observed, seem to see with the backs of their heads as well as the fronts, whenever I am drawing them. You will find the question entered into at some length in my sixth lecture in the 4 Eagles Nest' ; and I endeavoured to find out some particulars of which I might have given you assurance to-night, in my scientific books ; but though I found pages upon pages of description of the scales and wrinkles about snakes' eyes, I could come at no account what- ever of the probable range or distinctness in the sight of them ; and though extreme pains had been taken to exhibit, in sundry delicate engravings, their lachrymatory glands and ducts, I could neither discover the occasions on which rattle- snakes wept, nor under what consolations they dried their eyes. 10. Next for the word dracon, or dragon. We are accus- tomed to think of a dragon as a winged and clawed creature ; but the real Greek dragon, Cadmus's or Jason's, was simply a serpent, only a serpent of more determined vigilance than the ophis, and guardian therefore of fruit, fountain, or fleece. In that sense of guardianship, not as a protecter, but as a sentinel, the name is to be remembered as well fitted for the great Greek lawgiver. The dragon of Christian legend is more definitely malig- nant, and no less vigilant. You will find in Mr. Anderson's supplement to my ' St. Mark's Rest,' " The Place of Dragons," a perfect analysis of the translation of classic into Christian tradition in this respect. 11. III. Anguis. The strangling thing, passing into the French ' angoisse ' and English ' anguish ' ; but we have never taken this Latin word for our serpents, because we have none of the strangling or constrictor kind in Europe. It is always used in Latin for the most terrible forms of snake, and has been, with peculiar infelicity, given by scientific people to the most innocent, and especially to those which can't strangle * See the careful drawing of the eye of Daboia Rtissellii, Thanato LIVING WAVES. ISl anything. The 1 Anguis fragilis ' breaks like a tobacco-pipe ; but imagine how disconcerting such an accident would be to a constrictor ! 12. IV. Coluber, passing into the French, \ couleuvre/ a grandly expressive word. The derivation of the Latin one is uncertain, but it will be wise and convenient to reserve it for the expression of coiling. Our word 'coil/ as the French ' cueillir,' is from the Latin ' colligere,' to collect ; and we shall presently see that the way in which a snake £ collects • itself i3 no less characteristic than the way in which it diffuses itself. 13. V. Serpens. The winding thing. This is the great word which expresses the progressive action of a snake, dis- tinguishing it from all other animals ; or, so far as modifying the motion of others, making them in that degree serpents also, as the elongated species of fish and lizard. It is the principal object of my lecture this evening to lay before you the law of this action, although the interest attaching to other parts of my subject has tempted me to enlarge on them so as to give them undue prominence. 14. VI. Adder. This Saxon word, the same as nieder or nether, ' the grovelling thing,' was at first general for all ser- pents, as an epithet of degradation, * the deaf adder that stop- peth her ears/ Afterwards it became provincial, and has never been accepted as a term of science. In the most schol- arly late English it is nearly a synonym with 6 viper,' but that word, said to be a contraction for vivipara, bringing forth the young alive, is especially used in the New Testament of the Pharisees, who compass heaven and earth to make one prose- lyte. The Greek word used in the same place, echidna, is of doubtful origin, but always expresses treachery joined with malice. 15. VII. Snake. German, * schlange,' the crawling thing ; and with some involved idea of sliminess, as in a snail. Of late it has become partly habitual, in ordinary English, to use it for innocent species of serpents, as opposed to venomous ; but it is the strongest and best general term for the entire race ; which race, in order to define clearly, I must now entef 182 DEUCALION. into some particulars respecting classification, which I find little announced in scientific books. 16. And here I enter on the third division of my lecture, which must be a disproportionately long one, because it in- volves the statement of matters important in a far wider scope than any others I have to dwell on this evening. For although it is not necessary for any young persons, nor for many old ones, to know 3 even if they can know, anything about the origin or development of species, it is vitally necessary that they should know what a species is, and much more what a genus or (a better word) gens, a race, of animals is. 17. A gens, race, or kinship, of animals, means, in the truth of it, a group which can do some special thing nobly and well. And there are always varieties of the race which do it in dif- ferent styles, — an eagle flies in one style, a windhover in another, but both gloriously, — they are ' Gentiles' — gentle- men creatures, well born and bred. So a trout belongs to the true race, or gens, of fish : he can swim perfectly ; so can a dolphin, so can a mackerel : they swim in different styles in- deed, but they belong to the true kinship of swimming creatures. 18. Now between the gentes, or races, and between the species, or families, there are invariably links — mongrel creat- ures, neither one thing nor another, — but clumsy, blunder- ing, hobbling, misshapen things. You are always thankful when you see one that you are not it. They are, according to old philosophy, in no process of development up or down, but are necessary, though much pitiable, where they are. Thus between the eagle and the trout, the mongrel or need- ful link is the penguin. Well, if you ever saw an eagle or a windhover flying, I am sure you must have sometimes wished to be a windhover ; and if ever you saw a trout or a dolphin, swimming, I am sure, if it was a hot day, you wished you could be a trout. But did ever anybody wish to be a penguin ? So, again, a swallow is a perfect creature of a true gens ; and a field-mouse is a perfect creature of a true gens ; and between the two you have an accurate mongrel— the bat LIVING WAVES. 183 Well, surely some of you have wished, as you saw them glanc- ing and dipping over lake or stream, that you could for half an hour be a swallow : there have been humble times with myself when I could have envied a field-mouse. But did ever anybody wish to be a bat ? 19. And don't suppose that you can invert the places of the creatures, and make the gentleman of the penguin, and the mongrel of the windhover, — the gentleman of the bat, and mongrel of the swallow. All these living forms, and the laws that rule them, are parables, when once you can read ; but you can only read them through love, and the sense of beauty ; and some day I hope to plead with you a little, of the value of that sense, and the way you have been lately losing- it. But as things are, often the best way of explaining the nature of any one creature is to point out the other creatures with whom it is connected, through some intermediate form of degradation. There are almost always two or three, or more, connected gentes, and between each, some peculiar manner of decline and of reascent. Thus, you heard Professor Huxley explain to you that the true snakes were connected with the lizards through helpless snakes, that break like with- ered branches ; and sightless lizards, that have no need for eyes or legs. But there are three other great races of life, with which snakes are connected in other and in yet more mar- vellous ways. And I do not doubt being able to show you, this afternoon, the four quarters, or, as astrologers would say, the four houses, of the horizon of serpent development, in the modern view, or serpent relation, in the ancient one. In the first quarter, or house, of his nativity, a serpent is, as Profess- or Huxley showed you, a lizard that has dropped his legs off. But in the second quarter, or house, of his nativity, I shall show you that he is also a duck that has dropped her wings off. In the third quarter, I shall show you that he is a iish that has dropped his fins off. And in the fourth quarter of ascent, or descent, whichever you esteem it, that a serpent is a honeysuckle, with a head put on. 20. The lacertine relations having been explained to you in *the preceding lecture by Professor Huxley, I begin this even- 184 DEUCALION. ing with the Duck. I might more easily, and yet more sur- prisingly, begin with the Dove ; but for time-saving must leave your own imaginations to trace the transition, easy as you may think it, from the coo to the quack, and from the walk to the waddle. Yet that is very nearly one-half the jour- ney. The bird is essentially a singing creature, as a serpent is a mute one ; the bird is essentially a creature singing for love, as a puffadder is one puffing for anger ; and in the descent from the sound which fills that verse of Solomon's Song, " The time of the singing of birds is come, and the voice of the turtle is heard in our land," to the recollection of the last flock of ducks which you saw disturbed in a ditch, ex- pressing their dissatisfaction in that peculiar monosyllable which from its senselessness has become the English expres- sion for foolish talk,* you have actually got down half-way ; and in the next flock of geese whom you discompose, might imagine at first you had got the whole way, from the lark's song to the serpent's hiss. 21. But observe, there is a variety of instrumentation in hisses. Most people fancy the goose, the snake, and we our- selves, are alike in the manner of that peculiar expression of opinion. But not at all. Our own hiss, whether the useful and practical ostler's in rubbing down his horse, or that om- nipotent one which — please do not try on me just now ! — are produced by the pressure of our soft round tongues against our teeth. But neither the goose nor snake can hiss that way, for a goose has got no teeth, to speak of, and a serpent no tongue, to speak of. The sound which imitates so closely our lingual hiss is with them only a vicious and vindictive sigh, — the general disgust which the creature feels at the sight of us expressed in a gasp. Why do you suppose the puffadder is called puffy ? f Simply because he swells himself up to hiss, just as Sir Gorgius Midas might do to scold his footmen, and then actually and literally 'expires* with rage, * The substantive 1 quack ' in its origin means a person who quacks, ■ — i.e., talks senselessly; see Johnson. f In more graceful Indian metaphor, the 4 Father of Tumefaction. (Note from a friend.) LIVING WAVES. 185 sending all the air in bis body out at you in a biss. In a quieter way, the drake and gander do the same thing ; and we ourselves do the same thing under nobler conditions, of which presently. 22. But now, here's the first thing, it seems to me, we've got to ask of the scientific people, what use a serpent has for his tongue, since it neither wants it to talk with, to taste with, to hiss with, nor, so far as I know, to lick with,* and least of all to sting with,- — and yet, for people who do not know the creature, the little vibrating forked thread, flashed out of its mouth, and back again, as quick as lightening, is the most threatening part of the beast ; but what is the use of it ? Nearly every other creature but a snake can do all sorts of mischief with its tongue. A woman worries with it, a cha- meleon catches flies with it, a snail files away fruit with it, a hummingbird steals honey with it, a cat steals milk with it, a pholas digs holes in rocks with it, and a gnat digs holes in us with it ; but the poor snake cannot do any manner of harm with it whatsoever ; and what is his tongue forked for ? 23. I must leave you to find out that at your leisure ; and to enter at your pleasure into the relative anatomical questions respecting forms of palate, larynx, and lung, in the dove, the swan, the goose, and the adder, — not unaccompanied by ser- pentine extension and action in the necks of the hissing birds, which show you what, so to speak, Nature is thinking of. These mechanical questions are all — leather and prunella, or leather and catgut ; — the moral descent of the temper and meaning in the sound, from a murmur of affection to a gasp of fury, is the real transition of the creature's being. You will find in Kinglake's account of the charge of the Grays in the battle of Balaclava, accurate record of the human murmur of long-restrained rage, at last let loose ; and may reflect, also at your leisure, on the modes of political development which change a kindly Scot into a fiery dragon. 24. So far of the fall of the bird-angels from song to hiss : * I will not take on me to contradict, but I don't in the least believe, any of the statements about serpents licking their prey before they swallow it. ISO DEUCALIOSr. next consider for a minute or two the second phase of catas* trophe — from walk to waddle. Walk,— or, in prettier creatures still, the run. Think what a descent it is, from the pace of the lapwing, like a pretty lady's, — " Look, where Beatrice, like a lapwing, runs ; " or of the cream-coloured courser * of the African desert, whom you might yourselves see run, on your own downs, like a little racehorse, if you didn't shoot it the moment it alighted there, — to the respectable, but, to say the least, unimpressive, gait from which we have coined the useful word to ' w T addle.' Can you remember exactly how a duck does walk ? You can best fancy it by conceiving the body of a large barrel carried forward on two short legs, and rolling alternately to each side at every step. Once watch this method of motion attentively, and you will soon feel how near you are to dispensing with legs altogether, and getting the barrel to roll along by itself in a succession of zigzags. 25. Now, put the duck well under water, and he does dis- pense with his legs altogether. There is a bird who — my good friend, and boat-builder, Mr. Bell, tells me — once lived on Coniston Water, and some- times visits it yet, called the saw-bill duck, who is the link, on the ducky side, between the ducks and divers : his shape on the whole is a duck's, but his habits are a diver's, — that is to say, he lives on fish, and he catches them deep under water- swimming, under the surface, a hundred yards at a time. 26. W T e do not at all enough dwell upon this faculty in aquatic birds. Their feet are only for rowing — not for diving. Those little membranous paddles are no use whatever, once under water. The bird's full strength must be used in div- ing : he dives with his wings — literally flies under water with his wings ; — the great northern diver, at a pace which a well- manned boat can't keep up with. The stroke for progress, ob- serve, is the same as in the air ; only in flying under water, the bird has to keep himself down, instead of keeping himself up, and strikes up with the wing instead of down. Well, the great divers hawk at fish this way, and become themselves fish, or saurians, the wings acting for the time as true fins, or paddles * Cursorius isabellinus (Meyer), Gallicus (Gould). LIVING WAVES. 187 And at the same time, observe, the head takes the shape, and receives the weapons, of the fish-eating lizard. Magnified in the diagram to the same scale, this head of the saw-bill duck (No. 5) is no less terrible than that of the gavial, or fish-eating crocodile of the Ganges. The gavial passes, by the mere widening of the bones of his beak, into the true crocodile, — the crocodile into the serpentine lizard. I drop my duck's wings off through the penguin ; and its beak being now a saurian's, I have only to ask Professor Huxley to get rid of its feet for me, and my line of descent is unbroken, from the dove to the cobra, except at the one point of the gift of poison. 27. An important point, you say ? Yes ; but one which the anatomists take small note of. Legs, or no legs, are by no means the chief criterion of lizard from snake. Poison, or no poison, is a far more serious one. Why should the mere fact of being quadruped, make the creature chemically innocent ? Yet no lizard has ever been recognized as venomous. 28. A less trenchant, yet equally singular, law of distinc- tion is found in the next line of relationship we have to learn, that of serpents with fish. The first quite sweeping division of the whole serpent race is into water serpents and land serpents.* A large number, in- deed, like damp places ; and I suppose all serpents who ever saw water can swim ; but still fix in your minds the intense and broad distinction between the sand asp, which is so fond of heat that if you light a real fire near him he will instantly wriggle up to it and burn himself to death in the ashes, and the water hydra, who lives in the open, often in the deep sea, and * Br. Gunther's division of serpents, (' Reptiles of British India,' p. 166,) the most rational I ever saw in a scientific book, is into five main kinds : burrowing snakes, ground snakes, and tree snakes, on the land ; and fresh-water snakes and sea snakes, in the water. All the water snakes are viviparous ; and I believe all the salt-water ones venomous. Of the fresh-water snakes, Dr. Gunther strongly says, l< none are venomous," to my much surprise ; for I have an ugly recol- lection of the black river viper in the Zoological Gardens, and am nearly certain that Humboldt speaks of some of the water serpents of Brazil as dangerous. 188 DEUCALION. though just as venomous as the little fiery wretch, has the bo(fy flattened vertically at the tail so as to swim exactly as eels do. 29. Not that I am quite sure that even those who go often- est to Eel Pie Island quite know how eels do swim, and still less how they walk ; nor, though I have myself seen them doing it, can I tell you how they manage it. Nothing in ani- mal instinct or movement is more curious than the way young eels get up beside the waterfalls of the Highland streams. They get first into the jets of foam at the edge, to be thrown ashore by them, and then wriggle up the smooth rocks — heaven knows how. If you like, any of you, to put on greased sacks, with your arms tied down inside, and your feet tied together, and then try to wriggle up after them on rocks as smooth as glass, I think even the skilfulest members of the Alpine Club will agree with me as to the difficulty of the feat ; and though I have watched them at it for hours, I do not know how much of serpent, and how much of fish, is min- gled in the motion. But observe, at all events, there is no walking here on the plates of the belly : whatever motion is got at all, is by undulation of body and lash of tail : so far as by undulation of body, serpentine ; so far as by lash of tail, fishy. 30. But the serpent is in a more intimate sense still, a fish that has dropped its fins off. All fish poison is in the fins or tail, not in the mouth. There are no venomous sharks, no fanged pikes ; but one of the loveliest fishes of the south coast, and daintiest too when boiled, is so venomous in the fin, that when I was going eagerly to take the first up that came on the fishing-boat's deck with the mackerel line, in my first day of mackerel fishing, the French pilot who was with me caught hold of my arm as eagerly as if I had been going to lay hold of a viper. Of the common medusa, and of the sting ray, you know probably more than I do : but have any of us enough con- sidered this curious fact ; (have any of you seen it stated clearly in any book of natural history?) that throughout the whole fish race, — which, broadly speaking, pass the whole of their existence in one continual gobble, — you never find any LIVING WAVES. 189 poison put into the teeth ; and throughout the whole serpent- race, never any poison put into the horns, tail, scales, or skin ? 31. Besides this, I believe the aquatic poisons are for the most part black ; serpent poison invariably white ; and, finally, that fish poison is only like that of bees or nettles, numbing and irritating, but not deadly ; but that the moment the fish passes into the hydra, and the poison comes through the teeth, the bite is mortal. In these senses, and in many others, (which I could only trace by showing you the undulatory motion of fins in the seahorse, and of body in the sole,) the serpent is a fish without fins. 32. Now, thirdly, I said that a serpent was a honeysuckle with a head put on. You perhaps thought I was jesting ; but nothing is more mysterious in the compass of creation than the relation of flowers to the serpent tribe, — not only in those to which, in ' Proserpina/ I have given the name Draconidse, and in which there is recognized resemblance in their popular name, Snapdragon, (as also in the speckling of the Snake's- head Fritillary,) but much more in those carnivorous, insect- eating, and monstrous, insect-begotten, structures, to which your attention may perhaps iiave been recently directed by the clever caricature of the possible effects of electric light, which appeared lately in the ' Daily Telegraph.' But, seven hundred years ago, to the Florentine, and three thousand years ago, to the Egyptian and the Greek, the mystery of that bond was told in the dedication of the ivy to Dionysus, and of the dragon to Triptolemus. Giotto, in the lovely design which is to-night the only relief to your eyes, thought the story of temptation enough symbolized by the spray of ivy round the hazel trunk ; and I have substituted, in my definition, the honey- suckle for the ivy, because, in the most accurate sense, the honeysuckle is an 6 anguis ' — a strangling thing. The ivy stem increases with age, without compressing the tree trunk, any more than the rock, that it adorns ; but the woodbine retains, to a degree not yet measured, but almost, I believe, after a certain time, unchanged, the first scope of its narrow con- tortion ; and the growing wood of the stem it has seized is contorted with it, and at last paralyzed and killed. 190 DEUCALION. That there is any essential difference in the spirit of life which gives power to the tormenting tendrils, from that which animates the strangling coils, your recent philosophy denies, and I do not take upon me to assert. The serpent is a honeysuckle * with a head put on ; and perhaps some day, in the zenith of development, you may see a honeysuckle getting so much done for it. 33. It is, however, more than time for me now to ap- proach the main parts of our subject, the characteristics of perfect serpent nature in pattern, motion, and poison. First, the pattern — i.e., of their colours, and the arranged masses of them. That, the scientific people always seem to think a matter of no consequence ; but to practical persons like me, it is often of very primal consequence to know a viper when they see it, which they can't conveniently, except by the pat- tern. The scientific people count the number of scales be- tween its eyes and its nose, and inform you duly of the amount ; but then a real viper won't stand still for you to count the scales between his eyes and his nose ; whereas you can see at a glance, what to us Londoners, at least, should surely be an interesting fact — that it has a pretty letter H on the top of its head (Diag. No. 6). I am a true Cockney my- self, — born within ring of Bow ; and it is impressive to me thus to see such a development of our dropped Hs. Then, the wavy zigzag down the back, with the lateral spots — one to each bend, are again unmistakable ; and a pretty general type of the kind of pattern which makes the poets and the story-tellers, when they need one epithet only, speak always of the Spotted snake.' Not but that a thrush or a wood- pecker are much more spotty than any snakes, only they're a great deal more than that, while the snake can often only be known from the gravel he lies on by the comparative sym- metry of his spots. 34. But, whether spotted, zigzagged, or blotched with re- * Farther note was here taken of the action of the blossoms of the cranberry, myrtilla regina, etc., for more detailed account of which (useless in this place without the diagram) the reader is referred to the sixth number of 1 Proserpina. ' LIVING WAVES. 191 ticulated stains, this, please observe, is constant in their col- ours : they are always, in the deadly serpents, lurid, or dull. The fatal serpents are all of the French school of art, — French grey ; the throat of the asp, French blue, the bright- est thing I know in the deadly snakes. The rest are all gravel colour, mud colour, blue-pill colour, or in general, as I say, French high-art colour. You will find this pointed out long ago in one of the most important chapters of * Modern Painters,' and I need not dwell upon it now, except just to ask you to observe, not only that puffadders and rattlesnakes have no resemblance to tulips and roses, but that they never have even the variegated greens and blues of mackerel, or the pinks and crimsons of the char or trout. Fancy the difference it would make in our general conception of creation, if pea- cocks had grey tails, and serpents golden and blue ones ; or if cocks had only black spectacles on their shoulders, and cobras red combs on their heads, — if hummingbirds flew in suits of black, and water- vipers swam in amethyst ! * 35. I come now to the fifth, midmost, and chiefly important section of my subject, namely, the manner of motion in ser- pents. They are distinguished from all other creatures by that motion, which I tried to describe the terror of, in the * Queen of the Air' — calling the Serpent "a wave without wind, — a current, — but with no fall." A snail and a worm go on their bellies as much as a serpent, but the essential motion o! a serpent is undulation, — not up and down, but from side to * Had I possessed the beautiful volume of the Thauatophidia, above referred to, before giving my lecture, I should have quoted from it the instance of one water-viper, Hydrophis nigrocincta (q. purpureocincta ?), who does swim in amethyst, if the colouring of the plate may be trusted, rather than the epithet of its name. I should also have recommended to especial admiration the finishing of the angular spots in Dr. Shortfs exquisite drawing of Hypnale Nepa. Mr. Alfred Tylor, on the evening when I last lectured, himself laid before the Zoological Society, for the first time, the theory of relation between the vertebras and the succession of dorsal bars or spots, which I shall be rejoiced if he is able to establish ; but I am quite ready to accept it on his authority, without going myself into any work on the bones. 192 DEUCALION. side ; and the first thing you have got to ask about it, is, why it goes from side to side. Those who attended carefully to Professor Huxley's lecture, do not need to be again told that the bones of its spine alloiv it to do so ; but you were not then told, nor does any scientific book that I know, tell you, why it needs to do so. Why should not it go straight the shortest way? Why, even when most frightened and most in a hurry, does it wriggle across the road, or through the grass, with that special action from which you have named your twisting lake in Hyde Park, and all other serpentine things ? That is the first thing you have to ask about it, and it never has been asked yet, distinctly. 36. Supposing that the ordinary impression were true, that it thrusts itself forward by the alternate advance and thrust- backward of the plates of its belly, there is no reason why it should not go straight as a centipede does, or the more terrific scarlet centipede or millepede, — a regiment of soldiers. I was myself long under the impression, gathered from scientific books, that it moved in this manner, or as this w T ise Natural History of Cuvier puts it, " by true reptation ; " * but, how- ever many legs a regiment or a centipede may possess, neither body of them can move faster than an individual pair of legs can, — their hundred or thousand feet being each capable of only one step at a time ; and, with that allowance, only a cer- tain proportion of pace is possible, and the utmost rapidity of the most active spider, or centipede, does not for an instant equal the dash of a snake in full power. But you — nearly all of you, I fancy — have learned, during the sharp frosts of the last winters, the real secret of it, and will recognize in a mo- ment what the motion is, and only can be, when I show you the real rate of it. It is not often that you can see a snake in a hurry, for he generally withdraws subtly and quietly, even f It cannot be too often pointed out how much would be gained by merely insisting on scientific books being written in plain English. If only this writer had been forbidden to use the word 4 repo' for k crawl,' and to write, therefore, that serpents were crawling creatures, who moved by true crawlation, — his readers would have seen exactly how far he and they had got. LIVING WAVES. 193 when distinctly seen ; but if you put him to his pace either by fear or anger, you will find it is the sweep of the outsiiio edge in skating, carried along the whole body, — that is to say, three or four times over. Outside or inside edge does not, however, I suppose, matter to the snake, the fulcrum being- according to the lie of the ground, on the concave or convex side of the curve, and the whole strength of the bod}' is alive in the alternate curves of it. 37. This splendid action, however, you must observe, can hardly ever be seen when the snake is in confinement. Half a second would take him twice the length of his cage ; and the sluggish movement which you see there, is scarcely ever more than the muscular extension of himself out of his • col- lected' coil into a more or less straight line ; which is an action imitable at once with a coil of rope. You see that one- half of it can move anywhere without stirring the other ; and accordingly you may see a foot or two of a large snake s body moving one way, and another foot or two moving the other way, and a bit between not moving at all ; which I, altogether, think we may specifically call ' Parliamentary ! motion ; but this has nothing in common with the gliding and truly ser- pentine power of the animal when it exerts itself. 38. (Thus far, I stated the matter in my lecture, apologizing at the same time for the incompleteness of demonstration which, to be convincing, would have taken me the full hour of - granted attention, and perhaps with small entertainment to most of my hearers. But, for once, I care somewhat to estab- lish my own claim to have first described serpent motion, just as I have cared much to establish Forbes's claim to have first discerned the laws of glacier flow ; and I allow myself, there- fore, here, a few added words of clearer definition. 39. "When languidly moving in its cage, (or stealthily when at liberty,) a serpent may continually be seen to hitch or catch one part of its body by the edge of the scales against the ground, and from the fulcrum of that fixed piece extend other parts or coils in various directions. But this is not the move- ment of progress. When a serpent is once in full pace, every part of its body moves with equal velocity ; and the whole in 194 DEUCALION. a series of waves, varied only in sweep in proportion to tha thickness of the trunk. No part is straightened — no part ex- tended — no part stationary. Fast as the head advances, the tail follows, and between both — at the same rate — every point of the body. And the impulse of that body bears it against, and is progressively resilient from, the ground at the edge of each wave, exactly as the blade of the oar in sculling a boat is progressively resilient from the water. In swimming, the action is seen in water itself, and is partially imitated also by fish in the lash of the tail. I do not attempt to analyze the direction of power and thrust in the organic structure, because I believe, without very high mathematics, it cannot be done even for the inorganic momentum of a stream, how much less for the distributed volition of muscle, which applies the thrust at the exact point of the living wave where it will give most forwarding power. I am not sure how far the water serpents may sometimes use vertical instead of lateral undulation ; but their tails are I believe always vertically flattened, implying only lateral oar- stroke. My friend Mr. Henry Severn, however, on one occa- sion saw a large fresh- water serpent swimming in vertically sinuous folds, with its head raised high above the surface, and making the water foam at its breast, just as a swan would.) 40. Adding thus much to what I said of snake action, I find - myself enabled to withdraw, as unnecessary, the question urged, in the next division of the lecture, as to the actual pain inflicted by snakebite, by the following letter,* since received on the subject, from Mr. Arthur Nicols : — * A series of most interesting papers, by Mr. Nicols, already pub- lished in 1 The Country,' and reprinted in ' Chapters from the Physical History of the Earth,' (Kegan, Paul, & Co.), may be consulted on all the points of chiefly terrible interest in serpent life. I have also a most valuable letter describing the utter faintness and prostration, without serious pain, caused by the bite of the English adder, from Mr. Speddiug Cur wen, adding the following very interesting notes. u The action was, and, so far as I have seen, always is, a distinct hammer-like stroke of the head and neck, with the jaw wide open. In the particular case in question, my brother had the adder hanging by the tail between his finger and thumb, and was lowering it gradually into our botany-box LIVING WAVES. 195 " With respect to your remark that there are no descrip- tions of the sensation produced by snake-poison, in the nature of things, direct evidence of this kind is not easy to get ; for, in the first place, the sufferer is very soon past the power of describing the sensations ; and, in the second, but a minute fraction of those who are killed by snakes in India come under the hands of medical men. A person of the better class, too, is rarely bitten fatally. The sufferers are those who go about with naked feet, and handle wood, and whose work generally brings them into contact with snakes. " A friend brought me from India last year several speci- mens of Echis carinata, a species about nine inches long, whose fangs (two on one maxilla in one instance) were as large as this— (a quarter of an inch long, curved), and hard as steel. " This Echis kills more people in its district than all the other snakes together ; it is found everywhere. We must also remember how very few persons bitten recover. Indirect evi- dence seems to point to a comatose state as soon as the poison takes effect ; and those writhings of bitten animals which it gives us so much pain to witness are probably not the expres- sion of suffering. In one of Fayrer's cases the patient (bitten by a cobra) complained, when taken to the hospital, of a burn- ing pain in his foot ; but as no more is said, I infer he then became incapable of giving any further description. The ? burning ' is just what I feel when stung by a bee, and the poison soon makes me drowsy. In one instance I lay for an the lid of which I was holding open. There were already three adders in the box ; and in our care lest they should try to escape, we did not keep enough watch over the new capture. As his head reached the level of the lid of the box, he made a side- dart at my hand, and struck by the thumb nail. The hold was quite momentary, but as the adder was suspended by the tail, that may be no guide to the general rule. The receding of the blood was only to a small distance, say a quarter of an inch round the wound. The remedies I used were whisky, (half a pint, as soon as I got to the nearest inn, and more at intervals all day, also ammonia,) both to drink and to bathe the wound with. The whisky seemed to have no effect : my whole body was cold and deathly, and I felt none of the glow which usually follows a stimulant." 196 DEUCALION. hour feebly conscious, but quite indifferent to the external world ; and although that is fourteen years ago, I well remem- ber speculating (albeit I was innocent of any knowledge of snakes then) as to whether their poison had a similar effect. It should not, I think, concern us much to learn what is the precise character of the suffering endured by any poor human being whose life is passing away under this mysterious influ- ence, but to discover its physiological action." 41. Most wisely and truly said : and indeed, if any useful result is ever obtained for humanity by the time devoted re- cently, both in experiment and debate, to the question of the origin of life, it must be in the true determination of the meanings of the words Medicine and Poison, and the separa- tion into recognized orders of the powers of the things which supply strength and stimulate function, from those which dis- solve flesh and paralyze nerve. The most interesting summed result which I yet find recorded by physicians, is the state- ment in the appendix to Dr. Fayrer's ' Thanatophidia \ of the relative mortal action of the Indian and Australian venomous snakes ; the one paralyzing the limbs, and muscles of breath- ing and speech, but not affecting the heart ; the other leaving the limbs free, but stopping the heart. 42. But the most terrific account which I find given with sufficient authority of the effect of snake-bite is in the general article closing the first volume of Kussell's ' History of Indian Serpents.' Four instances are there recorded of the bite, not of the common Cobra, but of that called by the Portuguese Cobra di Morte. It is the smallest, and the deadliest, of all venom- ous serpents known, — only six inches long, or nine at the most, and not thicker than a tobacco-pipe, — and, according to the most definite account, does not move like ordinary ser- pents, but throws itself forward a foot or two on the ground, in successive springs, falling in the shape of a horse-shoe. In the five instances given of its bite, death follows, in a boy, ten minutes after the bite ; and in the case of two soldiers, bitten by the same snake, but one a minute after the other, in their guard-room, about one in the morning, — the first died at seven in the morning, the second at noon ; in both, the powers LIVING WAVES. 197 of sight gradually failing, and tliey became entirely blind be- fore death. The snake is described as of a dark straw colour, with two black lines behind the head ; small, flat head, with eyes that shone like diamonds. 43. Next in fatal power to this serpent, — fortunately so rare that I can find no published drawing of it, — come the Cobra, Kattlesnake, and Trigonocephalus, or triangle-headed serpent of the West Indies. Of the last of these snakes, you will find a most terrific account (which I do not myself above one- third believe) in the ninth volume of the English translation of Cuvier's ' Animal Kingdom/ It is a grand book of fifteen volumes, copiously illustrated, and quite unequalled for col- lection of the things you do not want to know in the body of the text, and for ceasing to be trustworthy the moment it is entertaining. I will read from it a single paragraph concern- ing the Trigonocephalus, of which you may believe as much or as little as you like. " These reptiles possess an activity and vivacity of motion truly alarming. A ferocious instinct induces them to dart impetuously upon passengers, either by suddenly letting go the sort of spring which their body forms, rolled in concentric and superpoised circles, and thus shoot- ing like an arrow from the bow of a vigorous archer, or pur- suing them by a series of rapid and multiplied leaps, or climbing up trees after them, or even threatening them in a vertical position." 44. The two other serpents, one used to be able to study at our own Zoological Gardens ; but the cobra has now for some years had the glass in front of him whitened, to prevent vul- gar visitors from poking sticks at him, and wearing out his constitution in bad temper. I do not know anything more disgraceful to the upper classes of England as a body, than that, while on the one hand their chief recreations, without which existence would not be endurable to them, are gam- bling in horses, and shooting at birds, they are so totally with- out interest in the natures and habits of animals in general, that they have never thought of enclosing for themselves a park and space of various kinds of ground, in free and healthy air, in which there should be a perfect gallery, Louvre, or 198 DEUCALION, Uffizii, not of pictures, as at Paris, nor of statues, as a' Florence, but of living creatures of all kinds, beautifully kept, and of which the contemplation should be granted only to well-educated and gentle people who would take the trouble to travel so far, and might be trusted to behave decently and kindly to any living creatures, wild or tame. 45. Under existing circumstances, however, the Zoological Gardens are still a place of extreme interest ; and I have been able at different times to make memoranda of the ways of snakes there, which have been here enlarged for you by my friends, or by myself ; and having been made always with reference to gesture or expression, show you, I believe, more of the living action than you w T ill usually find in scientific drawings : the point which you have chiefly to recollect about the cobra being this curious one — that while the puffadder, and most other snakes, or snakelike creatures, sw T ell when they are angry, the cobra flattens himself ; and becomes, for four or five inches of his length, rather a hollow shell than a snake. The beautiful drawing made by Mr. Macdonald in enlarging my sketch from life shows you the gesture accu- rately," and especially the levelling of the head which gives it the chief terror. It is always represented with absolute truth in Egyptian painting and sculpture ; one of the notablest facts to my mind in the entire histoiy of the human race being the adoption by the Egyptians of this serpent for the type of their tyrannous monarchy, just as the cross or the lily was adopted for the general symbol of kinghood by the mon- arch s of Christendom. 46. I would fain enlarge upon this point,' but time forbids me : only please recollect this one vital fact, that the nature of Egyptian monarchy, however great its justice, is always that of government by cruel force ; and that the nature of Christian monarchy is embodied in the cross or lily, which signify either an authority received by divine appointment, and maintained by personal suffering and sacrifice ; or else a dominion consisting in recognized gentleness and beauty of character, loved long before it is obeyed. 47. And again, whatever may be the doubtful meanings of LIVING WAVES. 199 the legends invented among all those nations of the earth who have ever seen a serpent alive, one thing is certain, that they all have felt it to represent to them, in a way quite inevitably instructive, the state of an entirely degraded and malignant human life. I have no time to enter on any analysis of the causes of expression in animals, but this is a constant law for them, that they are delightful or dreadful to us exactly in the degree in which they resemble the contours of the human countenance given to it by virtue and vice ; and this head of the cerastes, and that of the rattlesnake, are in reality more terrific to you than the others, not because they are more snaky, but because they are more human, — because the one has in it the ghastliest expression of malignant avarice, and the other of malignant pride. In the deepest and most literal sense, to those who allow the temptations of our natural pas- sions their full sway, the curse, fabulously (if you will) spoken on the serpent is fatally and to the full accomplished upon ourselves ; and as for noble and righteous persons and nations, the words are for ever true, "Thou art fairer than the children of men : full of grace are thy lips ; " so for the ignoble and iniquitous, the saying is for ever true, " Thou art fouler than the children of the Dust, and the poison of asps is under thy lips. *' 48. Let me show you, in one constant manner of our na- tional iniquity, how literally that is true. Literally, observe. In any good book, but especially in the Bible, you must always look for the literal meaning of everything first, — and act out that, then the spiritual meaning easily and securely follows. Now in the great Song of Moses, in w^hich he fore- tells, before his death, the corruption of Israel, he says of the wicked race into which the Holy People are to change, " Their wine is the poison of dragons, and the cruel venom of asps." Their wine, — that is to say, of course, not the wine they drink, but the wine they give to drink. So that, as our best duty to our neighbour is figured by the Samaritan who heals wounds by pouring in oil and wine, our worst sin against our neigh- bour is in envenoming his wounds by pouring in gall and poison. The cruel venom of Asps — of that brow T n gentleman you see there ! 200 DEUCALION. 49. Now I am sure you would all be very much shocked, and think it extremely wrong, if you saw anybody deliberately poisoning so much as one person in that manner. Suppose even in the interests of science, to which you are all so de- voted, I were myself to bring into this lecture-room a country lout of the stupidest, — the sort whom you produce by Church of England education, and then do all you can to get emi- grated out of your way ; fellows whose life is of no use to them, nor anybody else ; and that — always in the interests of science — I were to lance just the least drop out of that beast's tooth into his throat, and let you see him swell, and choke, and get blue and blind, and gasp himself away — you wouldn't all sit quiet there, and have it so done — would you? — in the interests of science. 50. Well ; but how then if in your own interests ? Suppose the poor lout had his week's wages in his pocket — thirty shillings or so ; and, after his inoculation, I were to pick his pocket of them; and then order in a few more louts, and lance their throats likewise, and pick their pockets likewise, and divide the proceeds of, say, a dozen of poisoned louts, among you all, after lecture : for the seven or eight hundred of you, I could perhaps get sixpence each out of a dozen of poisoned louts ; yet you would still feel the proceedings pain- ful to your feelings, and wouldn't take the sixpen'north — would you ? 51. But how, if you constituted yourselves into a co-oper- ative Egyptian Asp and Mississippi Rattlesnake Company, with an eloquent member of Parliament for the rattle at its tail ? and if, brown asps getting scarce, you brewed your own venom of beautiful aspic brown, with a white head, and per- suaded your louts to turn their own pockets inside-out to get it, giving you each sixpence a night, — seven pounds ten a year of lovely dividend ! — How does the operation begin to look now ? Commercial and amiable — does it not ? 52. But how — to come to actual fact and climax — if, instead of a Company, you were constituted into a College of reverend and scholarly persons, each appointed — like the King of Salem — to bring forth the bread and wine of healing knowledge ; LIVING WAVES. 201 but that, instead of bread gratis, you gave stones for pay ; and, instead of wine gratis, you gave asp-poison for pay, — how then ? Suppose, for closer instance, that you became a College called of the Body of Christ, and with a symbolic pelican for its crest, but that this charitable pelican had begun to peck — not itself, but other people, — and become a vampire pelican, sucking blood instead of shedding, — how then ? They say it's an ill bird that fouls its own nest. My own feeling is that a well-behaved bird will neither foul its own nest nor another's, but that, finding it in any wise foul, it will openly say so, and clean it. 53. Well, I know a village, some few miles from Oxford, numbering of inhabitants some four hundred louts, in which .my own College of the Body of Christ keeps the public-house, and therein sells — by its deputy — such poisoned beer that the Rector's wife told me, only the day before yesterday, that she sent for some to take out a stain in a dress with, and couldn't touch the dress with it, it was so filthy with salt and acid, to provoke thirst ; and that while the public-house was there she had no hope of doing any good to the men, who always pre- pared for Sunday by a fight on Saturday night. And that my own very good friend the Bursar, and we the Fellows, of Corpus, being appealed to again and again to shut up that tavern, the answer is always, "The College can't afford it : we can't give up that fifty pounds a year out of those peasant sots' pockets, and yet ' as a College ' live." Drive that nail home with your own hammers, for I've no more time ; and consider the significance of the fact, that the gentlemen of England can't afford to keep up a college for their own sons but by selling death of body and soul to their own peasantry. 54. I come now to my last head of lecture — my caution concerning the wisdom which we buy at such a price. I had not intended any part of my talk to-night to be so grave ; and was forced into saying what I have now said by the ap- pointment of Fors that the said village Rector's wife should come up to town to nurse her brother, Mr. Severn, who drew your diagrams for you. I had meant to be as cheerful as I 202 DEUCALION. could ; and chose the original title of my lecture, c A Caution to Snakes/ partly in play, and partly in affectionate remem- brance of the scene in 'New Men and Old Acres,' in which the phrase became at once so startling and so charming, on the lips of my much-regarded friend, Mrs. Kendal. But this one little bit of caution more I always intended to give, and to give earnestly. 55. What the best wisdom of the Serpent may be, I assume that you all possess ; — and my caution is to be addressed to you in that brightly serpentine perfection. In all other re- spects as wise, in one respect let me beg you to be wiser than the Serpent, and not to eat your meat without tasting it, — meat of any sort, but above all the serpent-recommended meat of knowledge. Think what a delicate and delightful meat that used to be in old days, when it was not quite so common as it is now, and when young people — the best sort of them — - really hungered and thirsted for it. Then a youth went up to Cambridge, or Padua, or Bonn, as to a feast of fat things, of wines on the lees, well-refined. But now, he goes only to swallow, — and, more's the pity, not even to swallow as a glutton does, with enjoyment ; not even-*-forgive me the old Aristotelian Greek, ^So/xa'os rrj a^y — pleased w T ith the going down, but in the saddest and exactest way, as a constrictor does, tasting nothing all the time. You remember what Professor Huxley told you — most interesting it was, and new to me — of the way the great boa does not in any true sense swallow, but only hitches himself on to his meat like a coal- sack ; — well, that's the exact way you expect your poor modern student to hitch himself onto his meat, catching and notching his teeth into it, and dragging the skin of him tight over it, — till at last — you know I told you a little while ago our artists didn't know a snake from a sausage, — but, Heaven help us, your University doctors are going on at such a rate that it will be all we can do, soon, to know a man from a sausage. 56. Then think again, in old times what a delicious thing a book used to be in a chimney corner, or in the garden, or in the fields, where one used really to read a book, and nibble BE VISION. 203 a nice bit here and there if it was a bride-cakey sort of book, and cut oneself a lovely slice — fat and lean — if it was a round-of-beef sort of book. But what do you do with a book now, be it ever so good ? You give it to a reviewer, first to skin it, and then to bone it, and then to chew it, and then to lick it, and then to give it you down your throat like a hand- ful of pilau. And when you've got it, you've no relish for it, after all. And, alas ! this continually increasing deadness to the pleasures of literature leaves your minds, even in their most conscientious action, sensitive with agony to the sting of vanity, and at the mercy of the meanest temptations held out by the competition of the schools. How often do I re- ceive letters from young men of sense and genius, lamenting the loss of their strength, and waste of their time, but ending always with the same saying, " I must take as high a class as I can, in order to please my father." And the fathers love the lads all the time, but yet, in every word they speak to them, prick the poison of the asp into their young blood, and sicken their eyes with blindness to all the true joys, the true aims, and the true praises of science and literature ; neither do they themselves any more conceive what was once the faith of Englishmen ; that the only path of honour is that of rectitude, and the only place of honour, the one that you are fit for. Make your children happy in their youth ; let dis- tinction come to them, if it will, after well-spent and well- remembered years ; but let them now break and eat the bread of Heaven with gladness and singleness of heart, and send portions to them for whom nothing is prepared ; — and so Heaven send you its grace — before meat, and after it. CHAPTER H. REVISION. 1. If the reader will look back to the opening chapter of ' Deucalion,' he will see that the book was intended to be a col- lection of the notices of phenomena relating to geology which i>04 DEUCALION: were scattered through my former works, systematized so fai a& might be possible, by such additional studies as time per- mitted me. Hitherto, however, the scattered chapters have contained nothing else than these additional studies, which, so far from systematizing what preceded them, stand now greatly in need of arrangement themselves ; and still more of some explana- tion of the incidental passages referring to matters of higher science than geology, in which I have too often assumed that the reader is acquainted with — and in some degree even pre- pared to admit — the modes of thought and reasoning which have been followed throughout the general body of my writ- ings. I have never given myself out for a philosopher ; nor spoken of the teaching attempted in connection with any subject of inquiry, as other than that of a village showman's "Look — and you shall see." But, during the last twenty years, so many baseless semblances of philosophy have announced themselves ; and the laws of decent thought and rational question have been so far transgressed (even in our universities, where the moral philosophy they once taught is now only remembered as an obscure tradition, and the natural science in which they are proud, presented only as an impious conjecture), that it is forced upon me, as the only means of making what I have said on these subjects permanently useful, to put into clear terms the natural philosophy and natural theology to which my books refer, as accepted by the intellectual leaders of all past time. 2. To this end I am republishing the second volume of ' Modern Painters,' which, though in affected language, yet with sincere and very deep feeling, expresses the first and foundational law respecting human contemplation of the nat- ural phenomena under whose influence we exist, — that they can only be seen with their properly belonging joy, and in- terpreted up to the measure of proper human intelligence, when they are accepted as the work, and the gift, of a Living Spirit greater than our own. 3. Similarly, the moral philosophy which underlies all the BE VISION. 205 appeals, and all the accusations, made in the course of my wri tings on political science, assumes throughout that the principles of Justice and Mercy which are fastened in the hearts of men, are also expressed in entirely consistent terms through- out the higher — (and even the inferior, when undefiled)— ■ forms of all lovely literature and art ; and enforced by the Providence of a Ruling and Judging Spiritual Power, man- ifest to those who desire its manifestation, and concealed from those who desire its concealment. 4. These two Faiths, in the creating Spirit, as the source of Beauty, — in the governing Spirit, as the founder and main- tainer of Moral Law, are, I have said, assumed as the basis of all exposition and of all counsel, which have ever been at- tempted or offered in my books. I have never held it my duty, never ventured to think of it even as a permitted right, to proclaim or explain these faiths, except only by referring to the writings, properly called inspired, in which the good men of all nations and languages had concurrently — though at far distant and different times — declared them. But it has become now for many reasons, besides those above sj)ecined, necessary for me to define clearly the meaning of the words I have used — the scope of the laws I have appealed to, and, most of all, the nature of some of the feelings possible under the reception of these creeds, and impossible to those who refuse them. 5. This may, I think, be done with the best brevity and least repetition, by adding to those of my books still unfin- ished, ' Deucalion,' ' Proserpina/ ' Love's Meinie/ and Tors Clavigera,' explanatory references to the pieces of theology or natural philosophy which have already occurred in each, in- dicating their modes of connection, and the chiefly parallel passages in the books which are already concluded ; among which I may name the ' Eagle's Nest,' as already, if read care- fully, containing nearly all necessary elements of interpretation for the others. 6. I am glad to begin with ' Deucalion,' for its title already implies, (and is directly explained in its seventh page as imply- ing,) the quite first principle, with me, of historic reading in divinity, that all nations have been taught of God according 206 Dm C ALIGN. to their capacity, and may best learn what farther they would know of Him by reverence for the impressions which He has set on the hearts of each, and all. I said farther in the same place that I thought it well for the student first to learn the " myths of the Betrayal and Re- demption " as they were taught to the heathen world ; but I did not say what I meant by the e Betrayal ? and ' Redemption ■ in their universal sense, as represented alike by Christian and heathen legends. 7. The idea of contest between good and evil spirits for the soul and body of man, which forms the principal subject of all the imaginative literature of the world, has hitherto been the only explanation of its moral phenomena tenable by intel- lects of the highest power. It is no more a certain or suf- ficient explanation than the theory of gravitation is of the con- struction of the starry heavens ; but it reaches farther towards analysis of the facts known to us than any other. By ' the Be- trayal I in the passage just referred to I meant the supposed victory, in the present age of the world, of the deceiving spirit- ual power, which makes the vices of man his leading motives of action, and his follies, its leading methods. By ' the Re- demption ' I meant the promised final victory of the creating and true Spirit, in opening the blind eyes, in making the crooked places straight and the rough plain, and restoring the power of His ministering angels, over a world in which there shall be no more tears. 8. The £ myths ' — allegorical fables or stories — in wdrich this belief is represented, were, I went on to say in the same place, "incomparably truer " than the Darwinian — or, I will add, any other conceivable materialistic theory — because they are the instinctive products of the natural human mind, conscious of certain facts relating to its fate and peace ; and as unerring in that instinct as all other living creatures are in the difr covery of what is necessary for their life : while the material- istic theories have been from their beginning products, in the words used in the passage I am explaining (page 8, line 4), of the 'h alf wits of impertinent multitudes.' They are half- witted because never entertained by any person possessing REVISION, 207 imaginative power, — and impertinent, because they are always announced as if the very defect of imagination constituted a superiority of discernment. 9. In one of the cleverest — -(and, in description of the faults and errors of religious persons, usefullest) — books of this modern half-witted school, "une cure du Docteur Pontalais," of which the plot consists in the revelation by an ingenious doctor to an ingenuous priest that the creation of the world may be sufficiently explained by dropping oil with dexterity out of a pipe into a wineglass, — the assumption that 4a lo- gique ' and ' la methode ' were never applied to theological subjects except in the Quartier Latin of Paris in the present blessed state of Parisian intelligence and morals, may be I hope received as expressing nearly the ultimate possibilities of shallow arrogance in these regions of thought ; and I name the book as one extremely well worth reading, first as such ; and secondly because it puts into the clearest form I have yet met with, the peculiar darkness of materialism, in its denial of the hope of immortality. The hero of it, who is a perfectly virtuous person, and inventor of the most ingenious and be- nevolent machines, is killed by the cruelties of an usurer and a priest ; and in dying, the only consolation he offers his wife and children is that the loss of one life is of no consequence in the progress of humanity. This unselfish resignation to total death is the most heroic element in the Religion now in materialist circles called the Religion "of Humanity," and announced as if it were a new discovery of nineteenth-century sagacity, and able to replace in the system of its society, alike all former ideas of the power of God, and destinies of man. 10. But, in the first place, it is by no means a new discovery. The fact that the loss of a single life is of no consequence when the lives of many are to be saved, is, and always has been, the root of every form of beautiful courage ; and I have again and again pointed out, in passages scattered through writings carefully limited in assertion, between 1860 and 1870, that the heroic actions on which the material destinies of this world depend are almost invariably done under the conception 208 DEUCALION. of death as a calamity, which is to be endured by one for the deliverance of many, and after which there is no personal re- ward to be looked for, but the gratitude or fame of which the victim anticipates no consciousness. 11. In the second place, this idea of self-sacrifice is no more sufficient for man than it is new to him. It has, indeed, strength enough to maintain his courage under circumstances of sharp and instant trial ; but it has no power whatever to satisfy the heart in the ordinary conditions of social affection, or to console the spirit and invigorate the character through years of separation or distress. Still less can it produce the states of intellectual imagination which have hitherto been necessary for the triumphs of constructive art ; and it is a dis- tinctive essential point in the modes of examining the arts as part of necessary moral education, which have been constant in my references to them, that those of poetry, music, and painting, which the religious schools who have employed them usually regard only as stimulants or embodiments of faith, have been by me always considered as its evidences. Men do not sing themselves into love or faith ; but they are incapable of true song, till they love, and believe. 12. The lower conditions of intellect which are concerned in the pursuit of natural science, or the invention of mechan- ical structure, are similarly, and no less intimately, dependent for their perfection on the lower feelings of admiration and affection which can be attached to material things : these al- so — the curiosity and ingenuity of man — live by admiration and by love ; but they differ from the imaginative powers in that they are concerned with things seen — not with the evi- dences of things unseen — and it would be well for them if the understanding of this restriction prevented them in the present day as severely from speculation as it does from de- votion. 13. Nevertheless, in the earlier and happier days of Lin- naeus, de Saussure, von Humboldt, and the multitude of quiet workers on whose secure foundation the fantastic expatiations of modern science depend for whatever good or stability there is in them, natural religion was always a part of natural REVISION. 209 science ; it becomes with Linnaeus a part of his definitions ; it underlies, in serene modesty, the courage and enthusiasm of the great travellers and discoverers, from Columbus and Hudson to Livingstone ; and it has saved the lives, or solaced the deaths, of myriads of men whose nobleness asked for no memorial but in the gradual enlargement of the realm of manhood, in habitation, and in social virtue. 14. And it is perhaps, of all the tests of difference between the majestic science of those days, and the wild theories or foul curiosities of our own, the most strange and the most distinct, that the practical suggestions which are scattered through the writings of the older naturalists tend always di- rectly to the benefit of the general body of mankind ; while the discoverers of modern science have, almost without ex- ception, provoked new furies of avarice, and new tyrannies of individual interest ; or else have directly contributed to the means of violent and sudden destruction, already incalculably too potent in the hands of the idle and the wicked. 15. It is right and just that the reader should remember, in reviewing the chapters of my own earlier writings on the origin and sculpture of mountain form, that all the investiga- tions undertaken by me at that time were connected in my own mind with the practical hope of arousing the attention of the Swiss and Italian mountain peasantry to an intelligent administration of the natural treasures of their woods and streams. I had fixed my thoughts on these problems where they are put in the most exigent distinctness by the various distress and disease of the inhabitants of the valley of the Rhone, above the lake of Geneva : a district in which the ad- verse influences of unequal temperatures, unwholesome air, and alternate or correlative drought and inundation, are all gathered in hostility against a race of peasantry, the Valaisan, by nature virtuous, industrious, and intelligent in no ordinary degree, and by the hereditary and natural adversities of their position, regarded by themselves as inevitable, reduced in- deed, many of them, to extreme poverty and woful disease ; but never sunk into a vicious or reckless despair. 16. The practical conclusions at which I arrived, in study- 210 DEUCALION. ing the channels and currents of the Rhone, Ticino, and Ad. ige, were stated first in the letters addressed to the English press on the subject of the great inundations at Rome in 1871 ('Arrows of the Chace,' vol. ii., pp. 104-113), and they are again stated incidentally in 4 Fors 5 (Letter XIX.), with direct reference to the dangerous power of the Adige above Verona, Had those suggestions been acted upon, even in the most languid and feeble manner, the twentieth part of the sums since spent by the Italian government in carrying French Boulevards round Tuscan cities, and throwing down their ancient streets to find lines for steam tramways, would not only have prevented the recent inundations in North Italy, but rendered their recurrence for ever impossible. 17. As it is thus the seal of rightly directed scientific inves- tigation, to be sanctified by loving anxiety for instant practi- cal use, so also the best sign of its completeness and sym- metry is in the frankness of its communication to the general mind of well-educated persons. The fixed relations of the crystalline planes of minerals, first stated, and in the simplest mathematical terms ex- pressed, by Professor Miller of Cambridge, have been exam- ined by succeeding mineralogists with an ambitious intensity which has at last placed the diagrams of zone circles for quartz and calcite, given in Cloizeaux's mineralogy, both as monuments of research, and masterpieces of engraving, a place among the most remarkable productions of the feverish energies of the nineteenth century. But in the meantime, all the characters of minerals, except the optical and crystalline ones, which it required the best instruments to detect, and the severest industry to register, have been neglected ; * the * Even the chemistry has been allowed to remain imperfect or doubt- ful, while the planes of crystals were being counted : thus for an ex- treme instance, the most important practical fact that the colour of ultramarine is destroyed by acids, will not be found stated in the de- scriptions of that mineral by either Miller, Cloizeaux, or Dana ; and no microscopic studies of refraction have hitherto informed the public why a ruby is red, a sapphire blue, or a flint black. On a large scale, the darkening of the metamorphic limestones, near the central ranges, remains unexplained. HE VISION. 211 arrangement of collections in museums has been made unin- telligibly scientific, without the slightest consideration whether the formally sequent specimens were in lights, or places, where they could be ever visible ; the elements of mineralogy pre- pared for schools have been diversified by eight or ten differ- ent modes, nomenclatures, and systems of notation ; and while thus the study of mineralogy at all has become impos- sible to young people, except as a very arduous branch of mathematics, that of its connection with the structure of the earth has been postponed by the leading members of the Geological Society, to inquire into the habits of animalculae fortunately for the world invisible, and monsters fortunately for the world unregenerate. The race of old Swiss guides, who knew the flowers and crystals of their crags, has mean- while been replaced by chapmen, who destroy the rarest liv- ing flowers of the Alps to raise the price of their herbaria, and pedestrian athletes in the pay of foolish youths ; the result being that while fifty years ago there was a good and valuable mineral cabinet in every important mountain village, it is impossible now to find even at Geneva anything offered for sale but dyed agates from Oberstein ; and the confused refuse of the cheap lapidary's wheel, working for the supply of Mr. Cooke's tourists with ' Trifles from Cha- mouni.' 18. I have too long hoped to obtain some remedy for these evils by putting the questions about simple things which ought to be answered in elementary schoolbooks of science, clearly before the student. My own books have thus some- times become little more than notes of interrogation, in their trust that some day or other the compassion of men of science might lead them to pause in their career of discovery, and take up the more generous task of instruction. But so far from this, the compilers of popular treatises have sought al- ways to make them more saleable by bringing them up to the level of last month's scientific news ; seizing also invariably, of such new matter, that which was either in itself most singu- lar, or in its tendencies most contradictory of former suppo- sitions and credences : and I purpose now to redeem, so far 212 DEUCALION. as I can, the enigmatical tone of my own books, by collecting the sum of the facts they contain, partly by indices, partly in abstracts, and so leaving what I myself have seen or known, distinctly told, for what use it may plainly serve. For a first step in the fulfilment of this intention, some explanation of the circumstances under which the preceding- lecture (on the serpent) was prepared, and of the reasons for its insertion in ' Deucalion,' are due to the reader, who may have thought it either careless in its apparent jesting, or ir- relevant in its position. I happened to be present at the lecture given on the same subject, a few weeks before, by Professor Huxley, in which the now accepted doctrine of development was partly used in support of the assertion that serpents were lizards which had lost their legs ; and partly itself supported reciprocally, by the probability which the lecturer clearly showed to exist, of their being so. Without denying this probability, or entering at all into the question of the links between the present generation of animal life and that preceding it, my own lecture was in- tended to exhibit another series, not of merely probable, but of observable, facts, in the relation of living animals to each other. And in doing so, to define, more intelligibly than is usual among naturalists, the disputed idea of Species itself. As I wrote down the several points to be insisted on, I found they would not admit of being gravely treated, unless at extreme cost of pains and time — not to say of weariness to my audience. Do what I would with them, the facts them- selves were still superficially comic, or at least grotesque : and in the end I had to let them have their own way ; so that the lecture accordingly became, apparently, rather a piece of badinage suggested by Professor Huxley's, than a serious com- plementary statement. Nothing, however, could have been more seriously intended ; and the entire lecture must be understood as a part, and a very important part, of the variously reiterated illustration, through all my writings, of the harmonies and intervals in the REVISION. 213 being of the existent animal creation — whether it be developed or undeveloped. The nobly religious passion in which Linnaeus writes the prefaces and summaries of the * Systema Naturae/ with the universal and serene philanthropy and sagacity of Humboldt, agree in leading them to the optimist conclusion, best, and unsurpassably, expressed for ever in Pope's f Essay on Man ' ; and with respect to lower creatures, epigrammatized in the four lines of George Herbert, — " God's creatures leap not, bat express a feast Where all the guests sit close, and nothing wants. Progs marry fish and flesh ; — bats, bird and beast, Sponges, non-sense and sense, mines,* th' earth and plants." And the thoughts and feelings of these, and all other good, wise, and happy men, about the world they live in, are summed in the 104th Psalm. On the other hand, the thoughts of cruel, proud, envious, and unhappy men, of the Creation, always issue out of, and gather themselves into, the shambles or the charnel house : the word £ shambles/ as I use it, meaning primarily the battle- field, and secondly, every spot where any one rejoices in tak- ing life ; f and the ' charnel house ' meaning collectively, the Morgue, brothel, and vivisection-room. But, lastly, between these two classes, of the happy and the heartless, there is a mediate order of men both unhappy and compassionate' who have become aware of another form of existence in the world, and a domain of zoology extremely difficult of vivisection, — the diabolic. These men, of whom Byron, Burns, Goethe, and Carlyle are in modern days the chief, do not at all feel that the Nature they have to deal with expresses a Feast only ; or that her mysteries of good and evil are reducible to a quite visible Kosmos, as they stand ; * 'Mines' mean crystallized minerals. f Compare the Modern with the Ancient Mariner — gun versus cross- bow. — " A magnificent albatross was soaring about at a short distance astern, for some time in the afternoon, and was knocked over, but un- fortunately not picked up." (' Natural History of the Strait of MageL lan' : Edmonston and Douglas, 1871, page 225.) 214 DEUCALION. but that there is another Kosmos, mostly invisible, yet per- haps tangible, and to be felt if not seen.* Without entering, with Dr. Reville of Eotterdam, upon the question how men of this inferior quality of intellect become possessed either of the idea — or substance — of what they are in the habit of calling ' the Devil ' ; nor even into the more definite historical question, " how men lived who did seriously believe in the Devil " — (that is to say, every saint and sinner who received a decent education between the first and the seventeenth centuries of the Christian eera,) — I will merely advise my own readers of one fact respecting the above-named writers, of whom, and whose minds, I know somewhat more than Dr. Reville of Rotterdam, — that they, at least, do not use the w T ord ' Devil ' in any metaphorical, typical, or abstract sense, but — whether they believe or disbelieve in what they say — in a distinctly personal one : and farther, that the con- ceptions or imaginations of these persons, or any other such persons, greater or less, yet of their species — whether they are a mere condition of diseased brains, or a perception of really existent external forces, — are nevertheless real Visions described by them ' from the life/ as literally and straight- forwardly as ever any artist of Rotterdam painted a sot — or his pot of beer : and farther — even were we at once to grant that all these visions — as for instance Zechariah's, " I saw the Lord sitting on His Throne, and Satan standing at His right hand to resist Him," are nothing more than emanations of the unphosphated nervous matter — still, these states of delirium are an essential part of human natural history : and the species of human Animal subject to them, with the peculiar charac- ters of the phantoms which result from its diseases of the brain, are a much more curious and important subject of science than that which principally occupies the scientific mind of modern days — the species of vermin which are the product of peculiar diseases of the skin. I state this, however, merely as a necessary Kosmic princi- ple, without any intention of attempting henceforward to en- * * The Devil Iris Origin Greatness and Decadence/ (Sic, without commas,) Williams and Norgate, 1871. BRUMA ABTIFBX. 215 gage my readers in any department of Natural History which is outside of the ordinary range of Optics and Mechanics : but if they should turn back to passages of my earlier books which did so, it must always be understood that I am just as literal and simple in language as any of the writers above re- ferred to : and that, for instance, when in the first volume of 'Deucalion,' p. 144-145, I say of the Mylodon — "This crea- ture the Fiends delight to exhibit to you," I don't mean by 'the Fiends ' my good and kind geological friends at the British Museum, nor even the architect who made the drain-pipes from the posteriors of its gargoyles the principal shafts in his design for the front of the new building, — be it far from me, — but I do mean, distinctly, Powers of supernatural Mischief, such as St. Dunstan, or St. Anthony, meant by the same ex- pressions. With which advice I must for the present end this bit of explanatory chapter, and proceed with some of the glacial investigations relating only to the Lakes — and not to the In- habitants — whether of Coniston or Caina. CHAPTER IH. BRUMA ARTIFEX. 1. The frost of 9th March, 1879, suddenly recurrent and severe, after an almost Arctic winter, found the soil and rock of my little shaded hill garden, at Brantwood, chilled under- neath far down ; but at the surface, saturated through every cranny and pore with moisture, by masses of recently thawed snow. The effect of the acutely recurrent frost on the surface of the gravel walks, under these conditions, was the tearing up of their surface as if by minutely and delicately explosive gases ; leaving the heavier stones imbedded at the bottom of little pits fluted to their outline, and raising the earth round them in a thin shell or crust, sustained by miniature ranges of 216 DEUCALION. "basaltic pillars of ice, one range set above another, with level plates or films of earth between ; each tier of pillars some half-inch to an inch in height, and the storied architecture of them two or three inches altogether ; the little prismatic crys- tals of which each several tier was composed being sometimes knit into close masses with radiant silky lustre, and sometimes separated into tiny, but innumerable shafts, or needles, none more than the twentieth of an inch thick, and many termi- nating in needle-points, of extreme fineness. 2. The soft mould of the garden beds, and the crumbling earth in the banks of streams, were still more singularly di- vided. The separate clods, — often the separate particles, — were pushed up, or thrust asunder, by thread-like crystals, con- torted in the most fantastic lines, and presenting every form usual in twisted and netted chalcedonies, except the definitely fluent or meltingly diffused conditions, here of course impos- sible in crystallizations owing their origin to acute and steady frost. The coils of these minute fibres were also more paral- lel in their swathes and sheaves than chalcedony ; and more lustrous in their crystalline surfaces : those which did not sustain any of the lifted clods, usually terminating in fringes of needle-points, melting beneath the breath before they could be examined under the lens. 3. The extreme singularity of the whole structure la} 7 , to my mind, in the fact that there was nowhere the least vestige of stellar crystallization. No resemblance could be traced, — no connection imagined, — between these coiled sheaves, or pil- lared aisles, and the ordinary shootings of radiant films along the surface of calmly freezing water, or the symmetrical arbo- rescence of hoar-frost and snow. Here was an ice-structure wholly of the earth, earthy ; requiring for its development, the weight, and for its stimulus, the interference, of clods or particles of earth. In some places, a small quantity of dust, with a large supply of subterranean moisture, had been enough to provoke the concretion of masses of serpentine fila- ments three or four inches long ; but where there was no dust, there were no filaments, and the ground, whether dry or moist, froze hard under the foot. BRUM A ART IF EX. 217 4. Greatly blaming myself for never having noticed this structure before, I have since observed it, with other modes of freezing shown in the streamlets of the best watered dis- trict of the British Islands, — with continually increasing in- terest : until nearly all the questions I have so long vainly asked myself and other people, respecting the variable forma- tions of crystalline minerals, seem to me visibly answerable by the glittering, and softly by the voice, of even the least- thought-of mountain stream, as it relapses into its wintry quietness. 5. Thus, in the first place, the action of common opaque white quartz in filling veins, caused by settlement or desicca- tion, with transverse threads, imperfectly or tentatively crys- talline, (those traversing the soft slates of the Buet and Col d'Anter are peculiarly characteristic, owing to the total ab- sence of lustrous surface in the filaments, and the tortuous aggregation of their nearly solidified tiers or ranks,) cannot but receive some new rays of light in aid of its future expla- nation, by comparison with the agency here put forth, before our eyes, in the early hours of a single frosty morning ; agency almost measurable in force and progress, resulting in the steady elevation of pillars of ice, bearing up an earthy roof, with strength enough entirely to conquer its adherence to heavier stones imbedded in it. G. Again. While in its first formation, lake or pool ice throws itself always, on calm water, into stellar or plumose films, shot in a few instants over large surfaces ; or, in small pools, filling them with spongy reticulation as the water is exhausted, the final structure of its compact mass is an aggre- gation of vertical prisms, easily separable, when thick ice is slowly thawing : prisms neither formally divided, like those of basalt, nor in any part of their structure founded on the primitive hexagonal crystals of the ice ; but starch-like, and irregularly acute-Eingled. 7. Icicles, and all other such accretions of ice formed by additions at the surface, by flowing or dropping water, are filways, when unaffected by irregular changes of tempera- ture or other disturbing accidents, composed of exquisitely DEUCALION. transparent vitreous ice, (the water of course being supposed transparent to begin with) — compact, flawless, absolutely smooth at the surface, and presenting on the fracture, to the naked eye, no evidence whatever of crystalline structure. They will enclose living leaves of holly, fern, or ivy, without disturbing one fold or fringe of them, in clear jelly (if one may use the word of anything frozen so hard), like the dainti- est candyings by Parisian confectioner's art, over glace fruit, or like the fixed juice of the white currant in the perfect con- fiture of Bar-le-Duc ; — and the frozen gelatine melts, as it forms, stealthily, serenely, showing no vestige of its crystal- line power ; pushing nowhere, pulling nowhere ; revealing in dissolution, no secrets of its structure ; affecting flexile branches and foliage only by its weight, and letting them rise when it has passed away, as they rise after being bowed under rain. 8. But ice, on the contrary, formed by an unfailing supply of running water over a rock surface, increases, not from above, but from beneath. The stream is never displaced by the ice, and forced to run over it, but the ice is always lifted by the stream ; and the tiniest runlet of water keeps its own rippling way on the rock as long as the frost leaves it life to run with. In most cases, the tricklings which moisten large rock surfaces are supplied by deep under-drainage which no frost can reach ; and then, the constant welling forth and wimpling down of the perennial rivulet, seen here and there under its ice, glit- tering in timed pulses, steadily, and with a strength according to the need, and practically infinite, heaves up the accumu- lated bulk of chalcedony it has formed, in masses a foot or a foot and a half thick, if the frost hold ; but always more or less opaque in consequence of the action of the sun and wind, and the superficial additions by adhering snow or sleet ; until the slowly nascent, silently uplifted, but otherwise mo- tionless glaciers, — here taking casts of the crags, and fitted into their finest crannies with more than sculptor's care, and anon extended in rugged undulation over moss or shale, cover the oozy slopes of our moorlands with statues of cascades, where, even in the wildest floods of autumn, cascade is not. BRUM A ARTIFEX. 219 9. Actual waterfalls, when their body of water is great, and much of it reduced to finely divided mist, build or block them- selves up, during a hard winter, with disappointingly ponder- ous and inelegant incrustations, — I regret to say more like messes of dropped tallow than any work of water-nymphs, But a small cascade, falling lightly, and shattering itself only into drops, will always do beautiful things, and often incom- prehensible ones. After some fortnight or so of clear frost in one of our recent hard winters at Coniston, a fall of about twenty-five feet in the stream of Leathes-water, beginning with general glass basket-making out of all the light grasses at its sides, built for itself at last a complete veil or vault of finely interwoven ice, under which it might be seen, when the embroidery was finished, falling tranquilly : its strength being then too far subdued to spoil by overloading or over-labouring the poised traceries of its incandescent canopy. 10. I suppose the component substance of this vault to have been that of ordinary icicle, varied only in direction by infinite accidents of impact in the flying spray. But without includ- ing any such equivocal structures, we have already counted five stages of ice familiar to us all, yet not one of which has been accurately described, far less explained. Namely, (1) Common deep-water surface ice, increased from beneath, and floating, but, except in the degrees of its own expansion, not uplifted. (2) Surface ice on pools of streams, exhausting the water as it forms, and adherent to the stones at its edge. Variously increased in crusts and films of spongy network (3) Ice deposited by external flow or fall of water in super- added layers — exogen ice, — on a small scale, vitreous, and perfectly compact, on a large one, coarsely stalagmitic, like impure carbonate of lime, but I think never visibly fibrous- radiant, as stalactitic lime is. (4) Endogen ice, formed from beneath by tricklings over ground surface. (5) Capillary ice, extant from pores in the ground itself, and carrying portions of it up with its crystals. 11. If to these five modes of slowly progressive formation 220 DEUCALION, we add the swift and conclusive arrest of vapour or dew on a chilled surface, we shall have, in all, six different kinds of — terrestrial, it may be called as opposed to aerial — conge- lation of water : exclusive of all the atmospheric phenomena of snow, hail, and the aggregation of frozen or freezing par- ticles of vapour in clouds. Inscrutable these, on our present terms of inquiry ; but the six persistent conditions, formed before our eyes, may be examined with some chance of arriv- ing at useful conclusions touching crystallization in general. 12. Of which, this universal principle is to be first under- stood by young people ; — that every crystalline substance has a brick of a particular form to build with, usually, in some angle or modification of angle, quite the mineral's own special property, — and if not absolutely peculiar to it, at least pecul- iarly used by it. Thus, though the brick of gold, and that of the ruby-coloured oxide of copper, are alike cubes, yet gold grows trees with its bricks, and ruby copper weaves samite with them. Gold cannot plait samite, nor ruby copper branch into trees ; and ruby itself, with a far more convenient and adaptable form of brick, does neither the one nor the other. But ice, which has the same form of bricks to build with as ruby, can, at its pleasure, bind them into branches, or w T eave them into w r ool ; buttress a polar cliff with adamant, or flush a dome of Alp with light lovlier than the ruby's. 13. You see, I have written above, 'ruby/ as I write 'gold s or ice, not calling their separate crystals, rubies, or golds, or ices. For indeed the laws of structure hitherto ascertained by mineralogists have not shown us any essential difference between substances which crystallize habitually in symmet- rical detached figures, seeming to be some favourite arrange- ment of the figures of their primary molecules ; and those which, like ice, only under rare circumstances give clue to the forms of their true crystals, but habitually show themselves in accumulated mass, or complex and capricious involution. Of course the difference may be a question only of time ; and the sea, cooled slowly enough, might build bergs of hexagonal ice-prisms as tall as Cleopatra's needle, and as broad as the tower of Windsor ; but the time and temperature required, BRUM A ART IF EX. 221 by any given mineral, for its successful constructions of form, are of course to be noted among the conditions of its history, and stated in the account of its qualities. 14. Neither, hitherto, has any sufficient distinction been made between properly crystalline and properly cleavage planes.* The first great laws of crystalline form are given by Miller as equally affecting both ; but the conditions of sub- stance which have only so much crystalline quality as to break in directions fixed at given angles, are manifestly to be distinguished decisively from those which imply an effort in the substance to collect itself into a form terminated at sym- metrical distances from a given centre. The distinction is practically asserted by the mineral itself, since it is seldom that any substance has a cleavage parallel to more than one or two of its planes : and it is forced farther on our notice by the ragged lustres of true cleavage planes like those of mica, opposed to the serene bloom of the crystalline surfaces formed by the edges of the folia. 15. Yet farther. The nature of cleavage planes in definitely crystalline minerals connects itself by imperceptible grada- tions with that of the surfaces produced by mechanical sepa- ration in their masses consolidating from fusion or solution. It is now thirty years, and more, since the question whether the forms of the gneissitic buttresses of Mont Blanc were owing to cleavage or stratification, became matter of debate between leading members of the Geological Society ; and it remains to this day an undetermined one ! In succeeding numbers of 'Deucalion,' I shall reproduce, according to my promise in the introduction, the chapters of 'Modern Painters ' which first put this question into clear form ; the drawings which had been previously given by de Saussure and other geologists having never been accurate enough to explain the niceties of rock structure to their readers, although, to their own eyes on this spot, the conditions of form had been per- fectly clear. I see nothing to alter either in the text of these chapters, written during the years 1845 to 1850, or in the plates and diagrams by which they were illustrated ; and f See vol. i., chap, xiv., 20-22. 222 DEUCALION. hitherto, the course of geological discovery has given me, I regret to say, nothing to add to them : but the methods of microscopic research originated by Mr. Sorby, cannot but issue, in the hands of the next de Saussure, in some trust- worthy interpretation of the great phenomena of Alpine form. 16. I have just enough space left in this chapter to give some illustrations of the modes of crystalline increment which are not properly subjects of mathematical definition ; but are variable, as in the case of the formations of ice above described, by accidents of situation, and by the modes and quantities of material supply. 17. More than a third of all known minerals crystallize in forms developed from original molecules which can be ar- ranged in cubes and octahedrons ; and it is the peculiarity of these minerals that whatever the size of their crystals, so far as they are perfect, they are of equal diameter in every di- rection ; they may be square blocks or round balls, but do not become pillars or cylinders. A diamond, from which the crystalline figure familiar on our playing cards has taken its popular name, be it large or small, is still a diamond, in figure as well as in substance, and neither divides into a star, nor lengthens into a needle. 18. But the remaining two-thirds of mineral bodies resolve themselves into groups, which, under many distinctive con- ditions, have this in common, — that they consist essentially of pillars terminating in pyramids at both ends. A diamond of ordinary octahedric type may be roughly conceived as com- posed of two pyramids set base to base ; and nearly all min- erals belonging to other systems than the cubic, as composed of two pyramids with a tower between them. The pyramids may be four-sided, six-sided, eight-sided ; the tower may be tall, or short, or, though rarely, altogether absent, leaving the crystal a diamond of its own sort ; nevertheless, the primal separation of the double pyramid from the true tower with pyramid at both ends, will hold good for all practice, and to all sound intelligence. 19. Now, so long as it is the law for a mineral, that how- Fig 1- Fig. 2 Plate X. — Modes of Crystalline Increment. BRUM A ART1FEX. 223 ever large it may be, its form shall be the same, we have only crystallographic questions respecting the modes of its increase. But when it has the choice whether it will be tall or short, stout or slender, and also whether it will grow at one end or the other, a number of very curious conditions present them- selves, unconnected with crystallography proper, but bearing much on the formation and aspect of rocks. 20. Let a, fig. 1, plate X., be the section of a crystal formed by a square tower one-third higher than it is broad, and having a pyramid at each end half as high as it is broad. Such a form is the simplest general type of average crystalline dimension, not cubic, that we can take to start with. Now if, as at b, we suppose the crystal to be enlarged by the addition of equal thickness or depth of material on all its surfaces, — in the figure its own thickness is added to each side, — as the process goes on, the crystal will gradually lose its elongated shape, 'and approximate more and more to that of a regular hexagon. If it is to retain its primary shape, the additions to its substance must be made on the diagonal lines dotted across the angles, as at c, and be always more at the ends than at the flanks. But it may chance to determine the additions wholly otherwise, and to enlarge, as at d, on the flanks instead of the points ; or, as at e, losing all relation to the original form, prolong itself at the extremities, giving little, or perhaps nothing, to its sides. Or, lastly, it may alter the axis of growth altogether, and build obliquely, as at /, on one or more planes in opposite directions. 21. All the effective structure and aspect of crystalline sub- stances depend on these caprices of their aggregation. The crystal of amethyst of which a longitudinal section is given in plate X., fig. 2, is more visibly, by help of its amethyst stain- ing,) but not more frequently or curiously, modified by acci- dent than any common prism of rough quartz will be usually found on close examination ; but in this example, the various humours, advances, and pauses of the stone are all traced for us by its varying blush ; and it is seen to have raised itself in successive layers above the original pyramid — always thin at the sides, and oblique at the summit, and apparently endeav* 224 DEUCALION. ouring to educate the rectilinear impulses of its being into compliance with a beautiful imaginary curve. 22. Of prisms more successful in this effort, and constructed finally with smoothly curved sides, as symmetrical in their entasis as a Greek pillar, it is easy to find examples in opaque quartz — (not in transparent*) — but no quartz crystal ever bends the vertical axis as it grows, if the prismatic structure is complete ; while yet in the imperfect and fibrous state above spoken of, § 5, and mixed with clay in the flammeate forms of jasper, undulation becomes a law of its being ! 23. These habits, faculties, and disabilities of common quartz are of peculiar interest when compared with the totally differ- ent nature and disposition of ice, though belonging to the same crystalline system. The rigidly and limitedly mathematical mind of Cloizeaux passes without notice the mystery, and the marvel, implied in his own brief statement of its elementary form " Frisme hexagonal regidier" Why 'regular'? All crys- tals belonging to the hexagonal system are necessarily regular, in the equality of their angles. But ice is regular also in di- mensions. A prism of quartz or calcite may be of the form a on the section, Fig. 6,f or of the form b ; but ice is always true — like c, as a bee's cell — ' prisme regulier.' So again, Cloizeaux tells us that ice habitually is formed in ' tables hexagonales minces.' But why thin ? — and hoiv thin ? What proportion of surface to edge was in his mind as he wrote, undefined? The square plates of uranite, the hex- agonal folia of mica, are 6 minces ' in a quite different sense. They can be seen separately, or in masses which are distinctly * Smoky quartz, or even Cairngorm, will sometimes curve the sides parallel to the axis, but (I think) pure white quartz never. f I think it best to number my woodcuts consecutively through the whole work, as the plates also ; but fig. 5 is a long way back, p. 11?, vol. i. Some further notes on it will be found in the next chapter. a b Fig. 6. c Plate XI. — The Olympian Lightning. BRUM A ART IF EX. 225 separable. But the "prisme hexagonale mince, regulier" of ice cannot be split into thinner plates — cannot be built into longer prishis ; but, as we have seen, when it builds, is fantas- tic in direction, sudden in force, endlessly complex in form. 24. Here, for instance, fig. 7, is the outline of one of the sjHculse of incipient surface ice, formed by sharp frost on calm water already cooled to the freezing point. I have seen liter- ally clouds of surface ice woven of these barbed arrows, shot, — or breathed, across half a mile of lake in ten minutes. And every barb of them itself a miracle of structure, complex as an Alpine peak. These spicule float with their barbs downwards, like keels, and form guiding ribs above like those of leaves, between which the entire surface of the water becomes laminated ; but, as it does so, the spiculse get pushed up into little mountain ^^^^^ Fig. 7. ridges, always steeper on one side than the other — barbed on the steep side, laminated on the other — and radiating more or less trigonally from little central cones, which are raised above the water-surface with hollow spaces underneath. And it is all done with ' prismes hexagonales reguliers 9 ! 25. Done, — and sufficiently explained, in Professor Tyndall's imagination, by the poetical conception of ■ six poles 1 for every hexagon of ice.* Perhaps !— if one knew first what a pole was. itself — and how many, attractive, or repulsive, to the east and to the west, as well as to the north and the south — one might institute in imaginative science — at one's pleasure ; — thus also allowing a rose five poles for its five petals, and a wallflower four for its four, and a lily three, and a hawkweed thirteen. In the meantime, we will return to the safer guidance of primal mythology. 26. The opposite plate (XI.) has been both drawn and en- graved, with very happy success, from a small Greek coin, n * 4 Forms of Water, 7 in the chapter on snow. The discovery is an< nounced, with much self-applause, as an important step in science. 226 DEUCALION. drachma of Elis, by my good publisher's son, Hugh Allen. It is the best example I know of the Greek type of lightning, grasped or gathered in the hand of Zeus. In ordinary coins or gems, it is composed merely of three flames or forked rays, alike at both extremities. But in this Eleian thunderbolt, when the letters F.A. (the old form of beginning the name of the Eleian nation with the di gamma) are placed upright, the higher extremity of the thunderbolt is seen to be twisted, in sign of the whirlwind of electric storm, while its lower ex- tremity divides into three symmetrical lobes, like those of a flower, with spiral tendrils from the lateral points : as con- stantly the honeysuckle ornament on vases, and the other double groups of volute completed in the Ionic capital, and passing through minor forms into the earliest recognizable types of the fleur-de-lys. 27. The intention of the twisted rays to express the action of storm is not questionable — "tres imbris torti radios, et alitis austri." But there can also be little doubt that the tranquillities of line in the lower divisions of the symbol are intended to express the vital and formative power of electricity in its terrestrial currents. If my readers will refer to the chapter in ' Proserpina ' on the roots of plants, they will find reasons suggested for concluding that the root is not merely a channel of material nourishment to the plant, but has a vital influence by mere contact with the earth, which the Greek probably thought of as depending on the conveyance of ter- restrial electricity. We know, to this day, little more of the great functions of this distributed fire than he : nor how much, while we subdue or pervert it to our vulgar uses, we are in every beat of the heart and glance of the eye, depen- dent, with the herb of the field and the crystal of the hills, on the aid of its everlasting force. If less than this was implied by the Olympian art of olden time, we have at least, since, learned enough to read, for ourselves his symbol, into the higher faith, that, in the hand of the Father of heaven, the lightning is not for destruction only ; but glows, with a deeper strength than the sun's heat or the stars' light, through all the forms of matter, to purify them, to direct, and to save. USTDEX TO YOL. I. Agate, 82, 83. See Chalcedony; also, if possible, the papers on this subject in the Geological Magazine, vol. iv., Nos. 8 and 11 ; v., Nos. 1, 4, 5 ; vi., No. 12 ; and vii., No. 1 ; and Pebbles. Ages of Rocks, not to be denned in the catalogue of a practical Museum, 106. • Alabaster, sacred uses of, 78. Alabastron, the Greek vase so called, 78, 88. Alps, general structure of, 11, 154 ; are not best seen from their highest points, 12 ; general section of, 13 ; violence of former energies in sculpture of, 20 ; Bernese chain of, seen from the Simplon, 120 ; sections of, given by Studer examined, 157, 158. Anatomy, study of, hurtful to the finest art-perceptions, 11 ; of minerals, distinct from their history, 125. Amethyst, 90 ; and see Hyacinth. Angelo, Monte St. , near Naples, 30. Angels, and fiends, contention of, for souls of children, 144. Anger, and vanity, depressing influence of, on vital energies, 5, 6. Argent, the Heraldic metal, meaning of, 91. Arrangement, permanence of, how necessary in Museums, 107. Artist, distinction between, and man of science, 24 ; how to make one, 79. Athena, her eyes of the colour of sunset sky, 78. Banded structure, in rocks, 116. Baptism, chimes in rejoicing for, at Maglans, 58. Bdellium, meaning of the word, 76. Bell- Alp, hotel lately built on, its relation to ancient hospice of Simplon, 109. Bells, sweetness of their sound among mountains, 58. Beauty, more at hand than can ever be seen, 71. Benedict, St., laments decline of his order, 111. Bernard, St., labours of, 89 ; sermons of, 94 ; his coming to help Dante, 112. Berne, town of, scenery in its canton, 13. 228 INDEX. Bionnassay, aiguille of, its beauty, 19. In the 25th line of that page, for 1 buttresses/ read 'buttress.' Blue, how represented in Heraldry, 89. Bischof, G-ustav, facts of mineral formation collected by, as yet in- sufficient, 111. Bowerbank, Mr., exhaustive examination of flint fossils by, 112. Breccia, (but for 'breccia' in these pages, read 'conglomerate ') of the outmost Bernese Alps, 16, 17. Brientz, lake and valley of, 14. Brunig, pass of, 14. Bunney, Mr. J., drawing in Yenice by, 96. Carbuncle, meaning of the stone in Heraldry, 91. Chalcedony, formation of, 109 ; general account of, 122. Chalk, formation of, in the Alps, 13. Chamouni, valley of, its relation to the valley-system of the Alps, 14. Channels of rivers, formation of, 52, 136 ; and compare with p. 52 Mr. Clifton Ward s account of the denudation of the Lake district, Geological Magazine, vol. vii., p. 16. Chede, lake of, its destruction, 29. Cleavage, general discussion of subject opens, 158 ; definition of the several kinds of, 166. Cliffs of the Bay of Uri, 61. Clifton Ward, Rev. Mr., justice of his observations on glaciation of Lake district, 32 ; examination of agate structure by, 111 ; con- tinued, 125, 147 ; completed, 150 ; note on cleavage by, 159. Cluse, valley of, in Savoy, described, 58. Colour, perception of, its relation to health and temper, 85, 95 ; di* visions and order of, 86 ; Heraldic, antiquity of, 87. Como, lake and valley of, 15. Conglomerate of the Alps, 16 ; and in the 6th line of that page, fof 4 breccia,' read 1 conglomerate.' Coniston, rocks and lake of, 136. Contortion of Strata, 17, 19 ; observations on by Mr. Henry Willett, 117 ; assumptions respecting the " Plissement de la croute terrestre," by M. Violet-le-Duc, 109 ; general question of, 139-140 ; practical experiments in imitation of, 141, 160. Compare Saussure, Voy- ages, § 35, 1801, 1802. Controversy, fatal consequences of, 5. Crystal, Scriptural references to 77 ; construction of, 81. Crystallization, mystery of, 80 ; terms of its description, 125. Compart ' Ethics of the Dust,' passim ; but especially chap. iii. Curve of ice -velocities, 51. Dante, use of, the Divina Commedia in mental purification, 111. Debate, mischievousness of, to young people, 71. INDEX. 229 Defiles, transverse, of Alps, 14. Deundation, first opening of discussion upon, 130 ; obscurity of the geological expression, 131 ; apparent violence of its indiscriminate action, 138. See above, Channels ; and compare * Modern Painters,' vol. iv., p. 110. Design of ornament, how obtainable, 98. 4 Deucalion' and * Proserpina,' reasons for choice of these names for the author's final works, 8. Devil, influence of the, in modern education, 144. Dew, Arabian delight in, 76. Diamond, its meaning in Heraldry, 91 ; the story of diamond necklace, moral of, 97. Dilatation, theory of, in glaciers, its absurdity, 115 ; the bed of the Mer de Glace, considered as a thermometer tube, 116. Dover, cliffs of, operations which would be needful to construct Alps with them, 20 ; imagined results of their softness, 139. Edinburgh Castle, geology of its rock, 27. Emerald, meaning of, in Heraldry, 89. English, how to write it best, 142. Erosion, how far the idea of it is exaggerated, 31. Esdras, second book of, curious verse in its 5th chapter, probable inter- pretation of, 8. Essence (real being) of things, is in what they can do and suffer, 73. 'Evenings at Home,' quoted, 22. Excess in quantity, harm of, in Museum collections for educational pur- poses, 107. Expansion. See Dilatation. Eyes, their use, a nobler art than that of using microscopes, 22 ; colour of Athena's, 78. Facts, how few, generally trustworthy, yet ascertained respecting min- eral formation, 110. Faraday, Professor, discovery of regelation by, 34. Fissures in chalk containing flints, and traversing the flints, described by Mr. Henry Willett, 102, 107. Flint, essential characters of, 73 ; account of, carefully instituted by Mr. H. Willett, 110; no one knows yet how secreted, 112; dis- placed veins of, 101, 103. Forbes, Professor James, of Edinburgh, discovers the law of glacier mo- tion, 41 ; his survey of the Mer de Glace, 66 ; general notices of, 33 ? 64 ; the Author's meeting with, 108. Flowing, difficulty of defining the word, 43. Fluids, the laws of their motion not yet known, 69. Fractures of flint, difficulties in explaining, 102-107. 230 INDEX. Geology, the Author's early attachment to, 6 ; not needfut to artists, but rather injurious, 11 ; modern errors in developing, 60. Glaciers, are fluent bodies, 32 ; do not cut their beds deeper, but fill them up, 34, 53 ; original deposition of, 35 ; summary of laws of motion in, 41 ; rate of motion in, how little conceivable in slow- ness, 42 ; drainage of higher valleys by, 42 ; rising of their surface in winter, how accounted for, 68 ; false theories respecting, illus- trated, 115, 116. Compare also Tors Clavigera,' Letters xxxiv., pp. 88-94, and xxxv. , pp. 112-114. Gold, special mechanical qualities of, 62 ; need for instruction in its use, 79 ; mystery of its origin, 80 ; nomenclature of its forms, 105. Gondo, defile of, in the Simplon pass, 14. Good and Evil in spiritual natures, how discernible, 23, 144. Greek-English words, barbarism of, 142. Green, how represented in Heraldry, 89. Grey, meaning of, in Heraldry, 82. Gula, mediaeval use of the word, 94. Gules, meaning of the colour so called, in Heraldry, 82. Honey, use of, in experiments on glacier motion, 68, 140. Hyacinth, the precious stone so called, meaning of in Heraldry, 92. Heraldry, nobleness of, as a language, 95 ; order of colours in, 88 ; of the sky, 99. Hyalite, transition of, into chalcedony, 121-123. Ice, (of glaciers) will stretch, 47 ; is both plastic and viscous, 64. See Glacier. Interlachen, village of, stands on the soil deposited by the stream from Lauterbrunnen, 21 ; duty of geologists at, 166. Iris of the Earth, 62 ; the Messenger, 87. Imps, not to be bottled by modern chemists, 143. Iacinth. See Hyacinth. Jasper, Heraldic meaning of, 89. Jewels, holiness of, 79, 84; delighted in by religious painters, 98 ; duty of distributing, 99. Jones, Mr. Rupert, summary of mineralogical work by, 111. Judd, Mr. J. W., notice of geology of Edinburgh by, 27. Jungfrau, view of, from Castle of Manfred, 166. Jura mountains, view of the Alps from, 13 ; section of, in relation ta Alps, 13, 164 ; limestone formation of, 16. Kendal, town of, scenery near, 127. Kinnoull, hill of, near Perth, agates in, 82. INDEX. 231 Knighthood, Christian, its faithfulness to Peace, 85. Knots of siliceous rock, nature of, 113. Knowledge, how shortened by impatience, and blighted by debate, 70, 71. Lakes, level of, among Alps, 15 ; evacuation of, 135 ; English district of, section through, 157. Landscape, the study of, little recommended by the Author at Oxford, 10. Language, scientific, how to be mended, 142 ; dependence of, for its beauty, on moral powers, 95. Lauterbrunnen, valley of, 21, 166. Lava, definition of, 119 ; depth of, 120. Lenticular curiosity, vileness of, 23. Leslie, Mr. Stephen, reference to unadvised statements by, respecting the achievements of Alpine Club, 11. Limestone, Jura and Mountain, general notes on, 16, 164, 165. Lucerne, lake of, reason of its cruciform plan, 14. Lungren, lake of, its unusual elevation, 15. Lyell, Sir Charles, final result of his work, 25, 28. Maggiore, lake and valley of, 16. Maglans, village of, in Savoy, scenery near, 60. Malleson, the Rev. F. A., discovers rare form of Coniston slate, 138. Manna, (food of the Israelites,) reasons for its resemblance to crystal, 77. Mental perception, how dependent on moral character, 96. Metal-work, history of, proposal for its illustration, 72. Microscope, mistaken use of the, opposed to use of eyes, 23. Mineralogy, principles of arrangement in, adapted to popular intelli- gence, 101 ; present state of the science, 110. Modernism, the degradation of England by it, 95. * Modern Painters,' (the Author's book, so called,) contained the first truthful delineations of the Alps, 109 ; the Author's design for its republication, 8, 11 ; mistake in it, caused by thinking instead of observing, 36. Motion, proportionate, how to study, 47 ; rate of, in glaciers, 42. Mountains, how to see, and whence, 12. Museums, arrangement of, general principles respecting, 106 ; special plan of that at Sheffield, 99, 102. Muscular energy, not an all-sufficient source of happiness, or criterion of taste, 12. Nations, lower types of, without language or conscience, 95. Niagara, misleading observations upon, by the school of Sir Charles Lyell, 29. 232 INDEX. Noises in modern travelling, 57. Novelty the worst enemy of knowledge, 71. Nuts of silica, and almonds, why so called, 113. Onyx, importance of, in the history of the Jews, 77, 78 ; general ac- count of, 78, 83. Or, the Heraldic metal, meaning of, 87. Paradise, treasures of its first river, 75. Passion, evil effects of, on bodily health, 5. The reader would do well to study on this subject, with extreme care, the introductory clauses of Sir Henry Thompson's paper on Food, in the 28th number of the 'Nineteenth Century.' Paste, experiments in, on compression of strata, 139. Pearls, of great and little price, relative estimate of by English ladies, 98 ; Heraldic meaning of, 92. Pebbles, Scotch, nature of, unknown, 61. See Agate. Periods, the three great, of the Earth's construction, 25. Phillips, Professor, of Oxford, 61 ; section of Lake district by, 139. Plain of Switzerland, north of the Alps, its structure, 13. Plans, the Author's, of future work, 6. (I observe many readers have passed this sentence without recognizing its irony.) Plantagenet, Geoffrey, shield of, 91. Plasticity, the term defined, 62. Pools, how kept deep in streams, dubitable, 132. Poverty, how to be honourably mitigated, 107. Prestwich, Professor, of Oxford, 86. Priority in discovery, never cared for by the Author, 7. Progress, certainty of, to be secured in science only by modesty, 109. Proteus, the seal-herdsman, 94. Purple, modern errors respecting the colour, 94. Compare Hyacinth. Purpure, the Heraldic colour, meaning of, 90. Ram's skins, for covering of Jewish Tabernacle, 94. Red, how represented in Heraldry, 88. Regelation, theory of, as causing the motion of glaciers,-— its absurdity, 187. Rendu, Bishop of Amiens, his keenness of sense, 39. Rhine, upper valley of, 15. Rhone, upper valley of, 15. Rocks, wet and dry formation of, 110. Rood, Professor, Author receives assistance from, 69. Rosa, Monte, the chain of Alps to the north of it, 175. Rose, the origin of the Persian word for red, 88. Rossberg, fall of, how illustrating its form. 16. INDEX. 233 Sable, the Heraldic colour, meaning of, 91. Scarlet, the Heraldic colour, meaning of, 89. Science, modern, duties of, 30, 127 ; modern vileness and falseness of, 144 ; true, how beginning and ending, 146. (In that page, line 23, for ' science, 7 read * morals.') Scientific Persons, how different from artists, 24. Sealskins, use of, in the Jewish Tabernacle, 26. Selfishness, the Author's, 121. Sense, in morals, evil of substituting analysis for, 23. Senses, the meaning of being in or out of them, 23. Sensibility, few persons have any worth appealing to, 11. Sentis, Hoche, of Appenzell, structure of, 13, 17. Silica in lavas, 119 ; varieties of, defined, 120. Sinai, desert of, coldness of occasional climate in, 74. Simplon, village of, 107 ; Hospice of, 114. Slate, cleavage of, generally discussed, 158. Compare * Modern Paint- ers,' Part v , chapters viii.-x. Sloth, (the nocturnal animal,) misery of, 144. Snow, Alpine, structure of, 35, 38, 40. Sorby, Mr., value of his work, 111. Sovereign, (the coin,) imagery on, 102. Squirrel, beauty of, and relation to man, 145. Stalagmite, incrustation of, 109. Standing of aiguilles, method of, to be learned, 21. Stockhorn, of Thun, structure of, 13. Stones, loose in the Park, one made use of, 73 ; precious their real meaning, 96. Streams, action of, 132. See Channels ; and compare i Modern Paint- ers,' vol. x., pp. 91, 95. Studer, Professor, references to his work on the Alps, 18, 157. Sun, Heraldic type of Justice, 87, 88. Tabernacle, the Jewish fur-coverings of, 94 ; the spiritual, of God, in man, 99. Temeraire, the fighting, at Trafalgar, 87. Tenny, the Heraldic colour, meaning of, 89. Theory, mischief of, in scientific study, 109 ; the work of ' Deucalion ' exclusive of it, 20. Thinking, not to be trusted, when seeing is possible, 36. Thoughts, worth having, come to us ; we cannot come at them, 56. Thun, lake and vale of, 14 ; passage of the lake by modern tourists, 19 ; old-fashioned manners of its navigation, 19. Time, respect due to, in forming collections of objects for study, 107. Topaz, Heraldic meaning of, 88. Torrents, action of, in forming their beds, debated, 28. 234 INDEX. Town life, misery of, 146. Truth, ultimate and mediate, differing character of, 92. Turner, J. M. W., Alpine drawings by, 11. Tylor, Mr. Alfred, exhaustive analysis of hill curves by, 167. Tyndall, Professor, experiments by, 37 ; various references to his works t 46, 50, 67, 114, 158, 163. Tyrrwhitt, the Rev. St. John, sketches in Arabia by, 76. Valleys, lateral and transverse, of Alps, 14 ; names descriptive of, in England how various, 128. Valtelline, relation of, to Alps, 15. Vanity of prematurely systematic science, 101. Vert, the Heraldic colour, meaning of, 89. Via Mala, defile of, 14, 20. Violet-le-Duc, unwary geology by, 108. Viscosity, definition of, 47, 62 ; first experiments on viscous motion of viscous fluids by Professor Forbes, 45. Volcanos, our personal interest in the phenomena of, in this world, 143. Woman, supremely inexplicable, 72. Willett, Mr. Henry, investigations of flint undertaken by, 110 ; pro- ceeded with, 114. Waves of glacier ice, contours of, in melting, 117. Wood, the Rev. Mr., method of his teaching, 145 ; and compare 1 Fors Clavigera,' Letter li., vol. ii. pp. 356-357. Woodward, Mr. Henry, experiment by, on contorted strata, 18. Woods, free growth of, in Savoy, 59. Weathering of Coniston slate, 137. Yellow, how represented in Heraldry, 81. Yewdale, near Coniston, scenery of, 130, 134, 136. Yewdale Crag, structure of 137 ; a better subject of study than crags in the moon, 143. KING OF THE GOLDEN RIVER ADVERTISEMENT. The Publishers think it due to the Author of this Fairy Tale.', to state the circumstances under which it appears. The King of the Golden Kiver was written in 1841, at the request of a very young lady, and solely for her amusement, without any idea of publication. It has since remained in the possession of a friend, to whose suggestion, and the passive assent of the Author, the Publishers are indebted for the op- portunity of printing it. The Illustrations, by Mr. Kichard Doyle, will, it is hoped, be found to embody the Author's ideas with characteristic spirit. THE KING OF THE GOLDEN OR, THE BLACK BROTHERS. RIVER; CHAPTER I. How the Agricultural System of the Black Brothers was INTERFERED WITH BY SOUTHWEST WlND, ESQUIRE. A secluded and mountainous part of Stiria there was, in old time, a valley of the most surprising and luxuriant fertility. It was surrounded, on all sides, by steep and rocky mountains, rising into peaks, which were always covered with snow, and from which a number of torrents descended in constant cataracts. One of these fell westward, over the face of a crag so high, that, when the sun had set to everything else, and all below was darkness, his beams still $hone full upon this waterfall, so that it looked like a shower J. gold, it wa$, therefore, called, by the people of the neigh- 240 THE KING OF THE GOLDEN RIVER; borhood, the Golden Biver. It was strange that none of these streams fell into the valley itself. They all descended on the other side of the mountains, and wound away through broad plains and by popular cities. But the clouds were drawn so constantly to the snowy hills, and rested so softly in the circular hollow, that in time of drought and heat, when all the country round was burnt up, there was still rain in the little valley ; and its crops were so heavy, and its hay so high, and its apples so red, and its grapes so blue, and its wine so rich, and its honey so sweet, that it was a marvel to every one who beheld it, and was commonly called the Treas- ure Valley. The whole of this little valley belonged to three brothers, called Schwartz, Hans, and Gluck. Schwartz and Hans, the two elder brothers, were very ugly men, with over-hanging eyebrows and small dull eyes, which were always half shut, so that you couldn't see into them, and always fancied they saw very far into you. They lived by farming the Treasure Valley, and very good farmers they were. They killed every- thing that did not pay for its eating. They shot the black- birds, because they pecked the fruit ; and killed the hedge- hogs, lest they should suck the cows ; they poisoned the crickets for eating the crumbs in the kitchen ; and smothered the cicadas, which used to sing all summer in the lime trees. They worked their servants without any wages, till they would not work any more, and then quarrelled with them, and turned them out of doors without paying them. It would have been very odd, if with such a farm, and such a system of farming, they hadn't got very rich ; and very rich they did get. They generally contrived to keep their corn by them till it was very dear, and then sell it for twice its value ; they had heaps of gold lying about on their floors, yet it was never known that they had given so much as a penny or a crust in charity ; they never went to mass ; grumbled perpetually at paying tithes ; and were, in a word, of so cruel and grinding a temper, as to receive from all those with whom they had any dealings, the pickname of the "Black Brothers." The youngest brother, Gluck, was as completely opposed. OR, TEE BLACK BROTHERS. 2« in both appearance and character, to his seniors as could pos- sibly be imagined or desired. He was not above twelve years old, fair, blue-eyed, and kind in temper to every living thing. He did not, of course, agree particularly well with his brothers, or rather, they did not agree with him. He was usually ap- pointed to the honorable office of turnspit, when there was anything to roast, which was not often ; for, to do the brothers justice, they were hardly less sparing upon themselves than upon other people. At other times he used to clean the shoes, floors, and sometimes the plates, occasionally getting what was left on them, by way of encouragement, and a wholesome quantity of dry blows, by way of education. Things went on in this manner for a long time. At last came a very wet summer, and everything went wrong in the country around. The hay had hardly been got in, when the haystacks were floated bodily down to the sea by an inunda- tion ; the vines were cut to pieces with the hail ; the corn was all kil]ed by a black blight ; only in the Treasure Valley, as usual, all was safe. As it had rain when there was rain no- where else, so it had sun when there was sun nowhere else. Everybody came to buy corn at the farm, and went away pouring maledictions on the Black Brothers. They asked what they liked, and got it, except from the poor people, who could only beg, and several of whom were starved at their very door, without the slightest regard or notice. It was drawing toward winter, and very cold weather, when one day the two elder brothers had gone out, with their usual warning to little Gluck, who was left to mind the roast, that he was to let nobody in, and give nothing out. Gluck sat down quite close to the fire, for it was raining very hard, and the kitchen walls were by no means dry or comfortable look- ing. He turned and turned, and the roast got nice and brown. " What a pity," thought Gluck, " my brothers never ask any- body to dinner. I'm sure, when they've got such a nice piece of mutton as this, and nobody else has got so much as a piece of dry bread, it would do their hearts good to have somebody to eat it with them." Just as he spoke, there came a double knock at the house 2*2 THE KING OF THE GOLDEN RIVER; door, yet heavy and dull, as though the knocker had been tied up — more like a puff than a knock. "It must be the wind," said Gluck ; "nobody else would venture to knock double knocks at our door." No ; it wasn't the wind : there it came again very hard, and what was particularly astounding, the knocker seemed to be in a hurry, and not to be in the least afraid of the conse- quences. Gluck went to the window, opened it, and put his head out to see who it was. It was the most extraordinary looking little gentleman he had ever seen in his life. He had a very large nose, slightly brass-colored ; his cheeks were very round, and very red, and might have warranted a supposition that he had been blowing a refractory fire for the last eight-and-forty hours ; his eyes twinkled merrily through long silky eyelashes, his mus- taches curled twice round like a corkscrew on each side of his mouth, and his hair, of a curious mixed pepper-and-salt color, descended far over his shoulders. He was about four feet six in height, and wore a conical-pointed cap of nearly the same altitude, decorated with a black feather some three feet long. His doublet was prolonged behind into something re- sembling a violent exaggeration of what is now termed a " swallow tail/' but was much obscured by the swelling folds of an enormous black, glossy-looking cloak, which must have been very much too long in calm weather, as the wind, whist- ling round the old house, carried it clear out from the w T earer's shoulders to about four times his own length. Gluck was so perfectly paralyzed by the singular appear- ance of his visitor, that he remained fixed, without uttering a word, until the old gentleman, having performed another, and a more energetic concerto on the knocker, turned round to look after his fly-away cloak. In so doing he caught sight of Gl uck's little yellow head jammed in the window, with its mouth and eyes very wide open indeed. " Hollo ! " said the little gentleman, " that's not the way to answer the door : I'm w T et, let me in." To do the little gentleman justice, he teas wet. His feather hung down between his le^s like a beaten puppy's tail drip- or. ftiE b^ack brothers. 213 ping like an umbrella ; and from the ends of his mustaches the water was running into his waistcoat pockets, and out again like a mill stream. " I beg pardon, sir," said Gluck, " I'm very sorry, but I really can't." " Can't what ! " said the old gentleman. "I can't let you in, sir, — I can't, indeed; my brothers would beat me to death, sir, if I thought of such a thing. What do you want, sir ? " " Want ? " said the old gentleman, petulantly. " I want fire, and shelter ; and there's your great fire there blazing, crackling, and dancing on the walls, with nobody to feel it. Let me in, I say ; I only want to warm myself." Gluck had had his head, by this time, so long out of the window, that he began to feel it was really unpleasantly cold, and when he turned, and saw the beautiful fire rustling and roaring, and throwing long bright tongues up the chimney, as if it were licking its chops at the savory smell of the leg of mutton, his heart melted within him that it should be burn- ing away for nothing. "He does look very wet," said little Gluck ; " I'll just let him in for a quarter of an hour." Round he went to the door, and opened it ; and as the little gentle- man walked in, there came a gust of wind through the house, that made the old chimneys totter. " That's a good boy," said the little gentleman. " Never mind your brothers. I'll talk to them." "Pray, sir, don't do any such thing," said Gluck. "I can't let you stay till they come ; they'd be the death of me." " Dear me," said the old gentleman, " I'm very sorry to hear that. How long may I stay ? " " Only till the mutton's done, sir," replied Gluck, "and it's very brown." Then the old gentleman walked into the kitchen, and sat himself down on the hob, with the top of his cap accommo- dated up the chimney, for it was a great deal too high for the roof. "You'll soon dry there, sir," said Gluck, and sat down again to turn the mutton. But the old gentleman did not 244 THE KING OF THE GOLDEN RIVER; dry there, but went on drip, drip, dripping among the cin- ders, and the fire fizzed, and sputtered, and began to look very black, and uncomfortable : never was such a cloak ; ev- ery fold in it ran like a gutter. "I beg pardon, sir," said Gluck, at length, after watching the water spreading in long, quicksilver-like streams over the floor for a quarter of an hour ; " mayn't I take your cloak ?" "No, thank you," said the old gentleman. " Your cap, sir ? " "I am all right, thank you," said the old gentleman, rather gruffly. "But — sir — I'm very sorry," said Gluck, hesitatingly; "but — really, sir — you're — putting the fire out." " It'll take longer to do the mutton, then," replied his visi- tor dryly. Gluck was very much puzzled by the behavior of his guest ; it was such a strange mixture of coolness and humil- ity. He turned away at the string meditatively for another five minutes. "That mutton looks very nice," said the old gentlenmn, ai length. "Can't you give me a little bit?" OR, THE BLACK BROTHERS. 245 " Impossible, sir," said Gluck. "I'm very hungry," continued the old gentleman : "I've had nothing to eat yesterday, nor to-day. They surely couldn't miss a bit from the knuckle ! " He spoke in so very melancholy a tone, that it quite melted Gluck 's heart. "They promised me one slice to-day, sir,* 5 said he ; I can give you that, but not a bit more." " That's a good boy," said the old gentleman again. Then Gluck warmed a plate, and sharpened a knife. " I don't care if I do get beaten for it," thought he. Just as he had cut a large slice out of the mutton, there came a tremen- dous rap at the door. The old gentleman jumped off the hob, as if it had suddenly become inconveniently warm. Gluck fitted the slice into the mutton again, with desperate efforts at exactitude, and ran to open the door. "What did you keep us waiting in the rain for?" said Schwartz, as he walked in, throwing his umbrella in Gluck's face. Ay ! what for, indeed, you little vagabond ? " said Hans, administering an educational box on the ear, as he followed his brother into the kitchen. "Bless my soul! " said Schwartz, when he opened the door. "Amen," said the little gentleman, who had taken his cap off, and was standing in the middle of the kitchen, bowing with the utmost possible velocity. "Who's that?" said Schwartz, catching up a rolling-pin, and turning to Gluck, with a fierce frown. "I don't know, indeed, brother," said Gluck, in great ter- ror. " How did he get in ? " roared Schwartz. "My dear brother," said Gluck, deprecatingly, "he was so very wet ! " The rolling-pin was descending on Gluck's head ; but, at the instant, the old gentleman interposed his conical cap, on which it crashed with a shock that shook the water out of it all over the room. What was very odd, the rolling pin no sooner touched the cap, than it flew out of Schwartz's hand, spinning like a straw in a high wind, and fell into the corner at the further end of the room. 246 THE KING OF THE GOLDEN RIVER; " Who are you, sir ? " demanded Schwartz, turning upon hiin. " What's your business ? 93 snarled Hans. "I'm a poor old man, sir," the little gentleman began very modestly, " and I saw your fire through the window, and begged shelter for a quarter of an hour." " Have the goodness to walk out again, then," said Schwartz. " We've quite enough water in our kitchen, without making it a drying-house." "It is a cold day to turn an old man out in, sir ; look at my gray hairs." They hung down to his shoulders, as I told you before. " Ay ! " said Hans, " there are enough of them to keep you warm. Walk ! " " I'm very, very hungry, sir ; couldn't you spare me a bit of bread before I go ? " "Bread, indeed ! " said Schwartz ; " do you suppose we've nothing to do with our bread, but to give it to such red-nosed fellows as you ? " "Why don't you sell your feather ? " said Hans, sneeringly- "Out with you." "A little bit," said the old gentleman. OR, THE BLACK BROTHERS. 247 " Be off ! " said Schwartz. * ' Pray, gentlemen." " Off, and be hanged ! " cried Hans, seizing him by the collar. But he had no sooner touched the old gentleman's collar, than away he went after the rolling-pin, spinning round and round, till he fell into the corner on the top of it. Then Schwartz was very angry, and ran at the old gentleman to turn him out ; but he also had hardly touched him, when away he went after Hans and the rolling-pin, and hit his head against the wall as he tumbled into the corner. And so there they lay, all three. Then the old gentleman spun himself round with velocity in the opposite direction ; continued to spin until his long cloak was all wound neatly about him ; clapped his cap on his head, very much on one side (for it could not stand upright without going through the ceiling), gave an additional twist to his corkscrew mustaches, and replied with perfect coolness : *' Gentlemen, I wish you a very good morning. At twelve o'clock to-night I'll call again ; after such a refusal of hospital- ity as I have just experienced, you will not be surprised if that visit is the last I ever pay you." "If ever I catch you here again," muttered Schwartz, com- ing, half frightened, out of the corner — but, before he could finish his sentence, the old gentleman had shut the house door behind him with a great bang : and there drove past the win- dow, at the same instant, a wreath of ragged cloud, that whirled and rolled away down the valley in all manner of shapes ; turning over and over in the air ; and melting away at last in a gush of rain. "A very pretty business, indeed, Mr. Gluck !" said Schwartz. " Dish the mutton, sir. If ever I catch you at such a trick again — bless me, why the mutton's been cut ! " " You promised me one slice, brother, you know," said Gluck. " Oh ! and you were cutting it hot, I suppose, and going to catch all the gravy. It'll be long before I promise you such a thing again. Leave the room, sir ; and have the kindness to wait in the coal-cellar till I call you." 248 TEE KING OF THE GOLDEN RIVER; Gluck left the room melancholy enough. The brothers ate as much mutton as they could, locked the rest in the cup- board, and proceeded to get very drunk after dinner. Such a night as it was ! Howling wind, and rushing rain, without intermission. The brothers had just sense enough left to put up all the shutters, and double bar the door, be- fore they went to bed. They usually slept in the same room. As the clock struck twelve, they were both awakened by a tremendous crash. Their door burst open with a violence that shook the house from top to bottom. " What's that ? " cried Schwartz, starting up in his bed. " Only I," said the little gentleman. The two brothers sat up on their bolster, and stared into the darkness. The room was full of water, and by a misty moonbeam, which found its way through a hole in the shut- ter, they could see in the midst of it, an enormous foam globe, spinning round, and bobbing up and down like a cork, on which, as on a most luxurious cushion, reclined the little old gentleman, cap and all. There was plenty of room for it now, for the roof was off. " Sorry to incommode you," said their visitor, ironically. " I'm afraid your beds are dampish ; perhaps you had better go to your brother's room : I've left the ceiling on, there." 0P h THE BLACK BROTHERS. 249 They required no second admonition, but rushed into Gluck's room, wet through, and in an agony of terror. " You'll find my card on the kitchen table," the old gentle- man called after them. "Kemember, the last visit. " "Pray Heaven it may !" said Schwartz, shuddering. And the foam globe disappeared. Dawn came at last, and the two brothers looked out of Gluck's little window in the morning. The Treasure Valley was one mass of ruin and desolation. The inundation had swept away trees, crops, and cattle, and left in their stead a waste of red sand, and gray mud. The two brothers crept shivering and horror-struck into the kitchen. The water had gutted the whole first floor ; corn, money, almost every mov- able thing had been swept away, and there was left only % small white card on the kitchen table. On it, in large, breezy, long-legged letters, were engraved the words : 250 THE KING OF THE GOLDEN RIVER; CHAPTEE n. Of the Proceedings of the Three Brothers after the Visit of Southwest Wind, Esquire ; and how little Gluck hak an Interview with the King of the Golden Kiver. OIJTHWEST WIND, Esquire, was as good as his word. After the momentous visit above related, he en- tered the Treasure Valley no more ; and, what was worse, he had so much influ- ence with his relations, the West Winds in general, and used it so effectually, that they all adopted a similar line of conduct. So no rain fell in the val- ley from one year's end to another. Though everything remained green and flourishing in the plains below, the inheritance of the Three Brothers was a desert. What had once been the richest soil in the kingdom became a shifting heap of red sand ; and the brothers, unable longer to contend with the adverse skies, abandoned their valueless patrimony in despair, to seek some means of gaining a livelihood among the cities and people of the plains. All their money was gone, and they 02?, THE BLACK BROTHERS. 251 had nothing left but some curious old-fashioned pieces of gold plate, the last remnants of their ill-gotten wealth. " Suppose we turn goldsmiths ? " said Schwartz to Hans, as they entered the large city. " It is a good knave's trade ; we can put a great deal of copper into the gold, without any one's finding it out." The thought was agreed to be a very good one ; they hired a furnace, and turned goldsmiths. But two slight circum- stances affected their trade : the first, that people did not ap- prove of the coppered gold ; the second, that the two elder brothers, whenever they had sold anything, used to leave lit- tle Gluck to mind the furnace, and go and drink out the money in the ale-house next door. So they melted all their gold, without making money enough to buy more, and were at last reduced to one large drinking-mug, which an uncle of his had given to little Gluck, and which he was very fond of, and would not have parted with for the world ; though he never drank anything out of it but milk and water. The mug was a very odd mug to look at. The handle was formed of two wreaths of flowing golden hair, so finely spun that it looked more like silk than metal, and these wreaths descended into, and mixed with, a beard and whiskers of the same ex- quisite workmanship, which surrounded and decorated a very 252 THE KING OF THE GOLDEN E1VEE; fierce little face, of the reddest gold imaginable, right in the front of the mug, with a pair of eyes in it which seemed to command its whole circumference. It was impossible to drink out of the mug without being subjected to an intense gaze out of the side of these eyes ; and Schwartz positively averred, that once, after emptying it, full of Rhenish, seven- teen times, he had seen them wink ! When it came to the mug's turn to be made into spoons, it half broke poor little Gluck's heart ; but the brothers only laughed at him, tossed the mug into the melting-pot, and staggered out to the ale- house ; leaving him, as usual, to pour the gold into bars, when it was all ready. When they were gone, Gluck took a farewell look at his old friend in the melting-pot. The flowing hair was all gone ; nothing remained but the red nose, and the sparkling eyes, which looked more malicious than ever. " And no wonder," thought Gluck, "after being treated in that way." He saun- tered disconsolately to the window, and sat himself down to catch the fresh evening air, and escape the hot breath of the furnace. Now this window commanded a direct view of the range of mountains, which, as I told you before, overhung umn of pure gold, from precipice to precipice, with the double arch of a broad purple rainbow stretched across it, flushing and fading alternately in the wreaths of spray. "All! " said Gluck aloud, after he had looked at it for a the Treasure Valley, and more especially of the peak from which fell the Golden River. It was just at the close of the day, and, when Gluck sat down at the window, he saw the rocks of the mountain-tops all crimson and purple with M the sunset ; and there were bright tongues of fiery cloud burning and quivering about them ; and the river, brighter than all, fell, in a waving col- OR, THE BLACK BROTHERS. £53 while, " if that river were really all gold, what a nice thing it would be." " No, it wouldn't, Gluck," said a clear metallic voice, close at his ear. "Bless me, what's that?" exclaimed Gluck, jumping up 6 There was nobody there. He looked round the room, and under the table, and a great many times behind him, but there was certainly nobody there, and he sat down again at the window. This time he didn't speak, but he couldn't help thinking again that it would be very convenient if the river were really all gold. "Not at all, my boy," said the same voice, louder than before. " Bless me ! 99 said Gluck again, " what is that ? " He looked again into all the corners, and cupboards, and then began turning round, and round, as fast as he could in the middle of the room, thinking there was somebody behind him, when the same voice struck again on his ear. It was singing now very merrily, " Lala-lira-la ; " no words, only a soft run- ning, effervescent melody, something like that of a keitle on the boil. Gluck looked out of the window. No, it was cer- tainly in the house. Up-stairs, and down-stairs. No, it was certainly in that very room, coming in quicker time, and clearer notes, every moment. "Lala-lira-la." All at once it struck Gluck that it sounded louder near the furnace. He ran to the opening, and looked in : yes, he saw right, it seemed to be coming, not only out of the furnace, but out of the pot. He uncovered it, and ran back in a great fright, for the pot w T as certainly singing ! He stood in the farthest corner of the room, with his hands up, and his mouth open, for a min- ute or two, when the singing stopped, and the voice became dear and pronunciative. " Hollo ! " said the voice. Gluck made no answer. " Hollo ! Gluck, my boy," said the pot again. Gluck summoned all his energies, walked straight up to the crucible, drew it out of the furnace, and looked in. The gold was all melted, and its surface as smooth and polished as 254 THE KINO OF THE GOLDEN E1VER; a river ; but instead of reflecting little Gluck's head, as he looked in, he saw, meeting his glance from beneath the gold, the red nose and sharp eyes of his old friend of the mug, a thousand times redder and sharper than ever he had seen them in his life. "Come, Gluck, my boy," said the voice out of the pot again. "I'm all right ; pour me out." But Gluck was too much astonished to do anything of the kind. "Pour me out, I say," said the voice, rather gruffly. Still Gluck couldn't move. " Will you pour me out? " said the voice, passionately, "I'm too hot." By a violent effort, Gluck recovered the use of his limbs, took hold of the crucible, and sloped it, so as to pour out the gold. But instead of a liquid stream, there came out, first, a pair of pretty little yellow legs, then some coat-tails, then a pair of arms stuck a-kimbo, and, finally, the well-known head of his friend the mug ; all which articles, uniting as they rolled out, stood up energetically on the floor, in the shape of a little golden dwarf, about a foot and a half high. " That's right ! " said the dwarf, stretching out first his legs, and then his arms, and then shaking his head up and down, and as far around as it would go, for five minutes, without stopping ; apparently with the view of ascertaining if he were quite correctly put together, while Gluck stood contemplating him in speechless amazement. He was dressed in a slashed doublet of spun gold, so fine in its texture, that the prismatic colors gleamed over it as if on a surface of mother of pearl ; and, over this brilliant doublet, his hair and beard fell full half w T ay to the ground, in waving curls, so exquisitely delicate, that Gluck could hardly tell where they ended ; they seemed to melt into air. The features of the face, however, were by no means finished with the same delicacy ; they were rather coarse, slightly inclining to coppery in complexion, and indicative, in expression, of a very pertinacious and intractable disposition in their smal] OK, THE BLACK BROTHERS. 255 proprietor. When the dwarf had finished his self-examina- tion, he turned his small sharp eyes full on Gluck, and stared at him deliberately for a minute or two. "No, it wouldn't, Gluck, my boy," said the little man. This was certainly rather an abrupt and unconnected mode of commencing conversation. It might indeed be supposed to refer to the course of Gluck's thoughts, which had first produced the dwarf's observations out of the pot ; but what- ever it referred to, Gluck had no inclination to dispute the dictum. " Wouldn't it, sir V " said Gluck, very mildly and submit sively indeed. 256 THE KING OF THE GOLDEN RIVEU ; "No," said the dwarf, conclusively, "No, it wouldn't." And with that, the dwarf pulled his cap hard over his brows, and took two turns, of three feet long, up and down the room, lifting his legs up very high, and setting them down very hard. This pause gave time for Gluck to collect his thoughts a little, and, seeing no great reason to view his diminutive visitor with dread, and feeling his curiosity overcome his amazement, he ventured on a question of peculiar deli- cacy. " Pray, sir," said Gluck, rather hesitatingly, "were you my mug ? " On which the little man turned sharp round, walked straight up to Gluck, and drew himself up to his full height. " I, " said the little man, " am the King of the Golden River," Whereupon he turned about again, and took two more turns, some six feet long, in order to allow time for the conster- nation which this announcement produced in his auditor to evaporate. After which, he again walked up to Gluck, and stood still, as if expecting some comment on his communica- tion. Gluck determined to say something at all events. " I hope your Majesty is very well," said Gluck. " Listen ! " said the little man, deigning no reply to this polite inquiry. " I am the King of what you mortals call the Golden River. The shape you saw me in was owing to the malice of a stronger King, from whose enchantments you have this instant freed me. "What I have seen of you, and your conduct to your wicked brothers, renders me willing to serve you ; therefore, attend to w r hat I tell you. Whoever shall climb to the top of that mountain, from which you see the Golden River issue, and shall cast into the stream at its source three drops of holy waiter, for him, and for him only, the river shall turn to gold. But no one failing in his first, can succeed in a second attempt ; and if any one shall cast unholy water into the river, it will overwhelm him, and he will become a black stone." So saying, the King of the Golden River turned away, and deliberately walked into the centre of the hottest flame of the furnace. His figure became OB, THE BLACK BROTHERS. red, white, transparent, dazzling — a blaze of intense light — rose, trembled, and disappeared. The King of the Golden River had evaporated. " Oh ! 99 cried poor Gluck, running to look up the chimney after him ; " Oh, dear, dear, dear me ! My mug ! my mug ! my mug ! " 258 TEE KING OF THE GOLDEN PdVEU; CHAPTER HI. How Mr. Hans set off on an Expedition to the Golden River, and how he prospered therein. HE King of the Gold- en River had hardly made the extraordina- ry exit related in the last chapter, before Hans and Schwartz came roaring into the house, very savagely drunk The discov- ery of the total loss of their last piece of plate had the effect of sobering them just enough to enable them to stand over Gluck, beating him very steadily for a quarter of an hour ; at the expiration of which period they dropped into a couple of chairs, and requested to know what he had got to say for himself. Gluck told them his story, of which, of course, they did not believe a word. They beat him again, till their arms were tired, and staggered to bed. In the morning, however, the steadiness with which he adhered to his story obtained him some degree of cre- dence ; the immediate consequence of which was, that the two brothers, after wrangling a long time on the knotty ques- tion, which of them should try his fortune first, drew their swords and began fighting. The noise of the fray alarmed OR, THE BLACK BROTHERS. 259 the neighbors, who, finding they could not pacify the com- batants, sent for the constable. Hans, on hearing this, contrived to escape, and hid himself ; but Schwartz was taken before the magistrate, fined for breaking the peace, and, having drunk out his last penny the evening before, was thrown into prison till he should pay. When Hans heard this, he was much delighted, and deter- mined to set out immediately for the Golden River. How to get the holy water was the question. He went to the priest, but the priest could not give any holy water to so abandoned a character. So Hans went to vespers in the evening for the first time in his life, and, under pretence of crossing himself, stole a cupful, and returned home in triumph. Next morning he got up before the sun rose, put the holy water into a strong flask, and two bottles of wine and some meat in a basket, slung them over his back, took his alpine staff in his hand, and set off for the mountains. On his way out of the town he had to pass the prison, and as he looked in at the windows, whom should he see but Schwartz himself peeping out of the bars, and looking very disconso- late. " Good morning, brother," said Hans ; " have you any mes- sage for the King of the Golden River ? " Schwartz gnashed his teeth with rage, and shook the bars with all his strength ; but Hans only laughed at him, and ad- vising him to make himself comfortable till he came back again, shouldered his basket, shook the bottle of holy water 2G0 THE KING OF THE GOLDEN RIVER; in Schwartz's face till it frothed again, and marched off in the highest spirits in the world. It was, indeed, a morning that might have made any one happy, even with no Golden Eiver to seek for. Level lines of dewy mist lay stretched along the valley, out of which rose the massy mountains — their lower cliffs in pale gray shadow, hardly distinguishable from the floating vapor, but gradu- ally ascending till they caught the sunlight, which ran in sharp touches of ruddy color along the angular crags, and pierced, in long level rays, through their fringes of spear-like pine. Far above, shot up red splintered masses of castellated rock, jagged and shivered into myriads of fantastic forms/ with here and there a streak of sunlit snow, traced down their chasms like a line of forked lightning ; and, far beyond, and far above all these, fainter than the morning cloud, but purer and changeless, slept, in the blue sky, the utmost peaks of the eternal snow. The Golden River, which sprang from one of the lower and snowless elevations, was now nearly in shadow ; all but the uppermost jets of spray, which rose like slow smoke above the undulating line of the cataract, and floated away in feeble wreathes upon the morning wind. On this object, and on this alone, Hans' eyes and thoughts were fixed ; forgetting the distance he had to traverse, he set off at an imprudent rate of walking, which greatly exhausted OB, THE BLACK BROTHERS. 261 him before he had scaled the first range of the green and low hills. He was, moreover, surprised, on surmounting them, to find that a large glacier, of whose existence, notwithstanding his previous knowledge of the mountains, he had been abso- lutely ignorant, lay between him and the source of the Golden River. He entered on it with the boldness of a practised mountaineer; yet he thought he had never traversed so strange or so dangerous a glacier in his life. The ice was ex- cessively slippery, and out of all its chasms came wild sounds of gushing water ; not monotonous or low, but changeful and loud, rising occasionally into drifting passages of wild mel- ody, then breaking off into short melancholy tones, or sudden shrieks, resembling those of human voices in distress or pain. The ice was broken into thousands of confused shapes, but none, Hans thought, like the ordinary forms of splintered ice. There seemed a curious expression about all their outlines — a perpetual resemblance to living features, distorted and scorn- ful. Myriads of deceitful shadows, and lurid lights, played and floated about and through the pale blue pinnacles, daz- zling and confusing the sight of the traveller ; while his ears grew dull and his head giddy with the constant gush and roar of the concealed waters. These painful circumstances increased upon him as he advanced ; the ice crashed and yawned into fresh chasms at his feet, tottering spires nodded around him, and fell thundering across his path ; and though he had repeatedly faced these dangers on the most terrific glaciers, and in the wildest weather, it was with a new and oppressive feeling of panic terror that he leaped the last chasm, and flung himself, exhausted and shuddering, on the firm turf of the mountain. He had been compelled to abandon his basket of food, which became a perilous incumbrance on the glacier, and had now no means of refreshing himself but by breaking off and eating some of the pieces of ice. This, however, relieved his thirst ; an hour's repose recruited his hardy frame, and with the indomitable spirit of avarice he resumed his laborious journey. His way now lay straight up a ridge of bare red rocks, 262 THE KINO OF THE GOLDEN RIVER; without a blade of grass to ease the foot, or a projecting angle to afford an inch of shade from the south sun. It was past noon, and the rajs beat intensely upon the steep path, while the whole atmosphere was motionless, and penetrated with heat. Intense thirst was soon added to the bodily fatigue with which Hans was now afflicted ; glance after glance he cast on the flask of water which hung at his belt. " Three drops are enough," at last thought he ; "I may, at least, cool my lips with it." He opened the flask, and was raising it to his lips, when his eye fell on an object lying on the rock beside him ; he thought it moved. It was a small c ently in the last agony of death from thirst. Its tongue was out, its jaws dry, its limbs extended lifelessly, and a swarm of black ants were crawling about its lips and throat. Its eye moved to the bottle which Hans held in his hand. He raised it, drank, spurned the animal with his foot, and passed on. And he did not know how it was, but he thought that a strange shadow had suddenly come across the blue sky. The path became steeper and more rugged every moment ; OR, THE BLACK BROTHERS. and the high hill air, instead of refreshing him, seemed to throw his blood into a fever. The noise of the hill cataracts sounded like mockery in his ears ; they were all distant, and his thirst increased every moment. Another hour passed, and he again looked down to the flask at his side ; it was half empty ; but there was much more than three drops in it. He stopped to open it, and again, as he did so, something moved in the path above him. It was a fair child, stretched nearly lifeless on the rock, its breast heaving with thirst, its eyes closed, and its lips parched and burning. Hans eyed it deliberately, drank, and passed on. And a dark gray cloud came over the sun, and long, snake-like shadows crept up. along the mountain sides. Hans struggled on. The sun was sinking, but its descent seemed to bring no coolness ; the leaden weight of the dead air pressed upon his brow and heart, but the goal was near. He saw the cataract of the Golden River springing from the hillside, scarcely five hun- dred feet above him. He paused for a moment to breathe, and sprang on to complete his task. At this instant a faint cry fell on his ear. He turned, and saw a gray-haired old man extended on the rocks. His eyes were sunk, his features deadly pale, and gathered into an ex- pression of despair. "Water!" he stretched his arms to Hans, and cried feebly ; " Water ! I am dying." "I have none," replied Hans ; "thou hast had thy share of life." He strode over the prostrate body, and darted on. And a flash of blue lightning rose out of the east, shaped like a sword ; it shook thrice over the whole heaven, and left it dark with one heavy, impenetrable shade. The sun was setting ; it plunged toward the horizon like a red-hot ball. The roar of the Golden River rose on Hans' ear. He stood at the brink of the chasm through which it ran. Its waves were filled with the red glory of the sunset : they shook their crests like tongues of fire, and flashes of bloody light gleamed along their foam. Their sound came mightier and mightier on his senses ; his brain grew giddy with the prolonged thun- der. Shuddering he drew the flask from his girdle, and hurled it into the centre of the torrent. As he did so, an icy chili ^64 TEE KING OF THE GOLDEN RIVER; shot through his limbs ; he staggered, shrieked, and fell. The waters closed over his cry. And the moaning of the river rose wildly into the night, as it gushed over The Black Stone, OR, THE BLACK BROTHERS. 265 CHAPTEE IV. How Mr. Schwartz set off on an Expedition to the Goldeh River, and how he prospered therein. . OR little Gluck waited very anxiously alone in the house for Hans' return. Finding- he did not come back, he was terribly frightened, and went and told Schwartz in the prison all that had happen- ed. Then Schwartz was very much pleased, and said that Hans must certainly have been turned into a black stone, and he should have all the gold to himself. But Gluck was very sorry, and cried all night. When he got up in the morning, there was no bread in the house, nor any money : so Gluck went and hired himself to another gold- smith, and he worked so hard, and so neatly, and so long every day, that he soon got money enough together to pay his brother's fine, and he went and gave it all to Schwartz, and Schwartz got out of prison. Then Schwartz was quite pleased, and said he should have some of the gold of the river. But Gluck only begged he would go and see what had become of Hans. Now, when Schwartz had heard that Hans had stolen the holy water, he thought to himself that such a proceeding might not be considered altogether correct by the King of the Golden River, and determined to manage matters better. So he took some more of Gluck's money, and went to a bad priest, who 266 THE KING OF THE GOLDEN RIVER; gave liim some holy water very readily for it. Then Schwartz was sure it was all quite right. So Schwartz got up early in he was surprised at sight of the glacier, and had great diffi- culty in crossing it, even after leaving his basket behind him. The day was cloud- less, but not bright : leavy purple haze hanging over the sky, and the hills looked lowering loomy. And as Schwartz climbed the steep rock path, the thirst came upon him, as it had upon his brother, until he lifted his flask to his lips to drink. Then he saw the fair child lying near him on the rocks, and it cried to him, and moaned for water. " Water, indeed," said Schwartz ; "I haven't half enough for myself," and passed on. And as he went he thought the sunbeams grew more dim, and he say/ a low bank of black cloud rising out of the west ; and when he had climbed for another hour the thirst overcame him again, and he would have drunk. Then he saw the old man lying before him on the path, and heard him cry out for OR, TEE BLACK BROTHERS. 267 water. u Water, indeed," said Schwartz; " I haven't hail enough for myself," and on he went. Then again the light seemed to fade from before his eyes, and he looked up, and, behold, a mist, of the color of blood, had come over the sun ; and the bank of black cloud had risen very high, and its edges were tossing and tumbling like the waves of the angry sea. And they cast long shadows, which flickered over Schwartz's path. Then Schwartz climbed for another hour, and again his thirst returned ; and as he lifted his flask to his lips, he thought he saw his brother Hans lying exhausted on the path before him, and, as he gazed, the figure stretched its arms to him, and cried for water. "Ha, ha," laughed Schwartz, " are you there ? remember the prison bars, my boy. Water, in- deed ! do you suppose I carried it all the way up here for you ? " And he strode over the figure ; yet, as he passed, he thought he saw a strange expression of mockery about its lips. And, when he had gone a few yards farther, he looked back ; but the figure was not there. And a sudden horror came over Schwartz, he knew not why ; but the thirst for gold prevailed over his fear, and he rushed on. And the bank of black cloud rose to the zenith, and out of it came bursts of spiry lightning, and waves of darkness seemed to heave and float between their flashes, over the whole heavens. And the sky, where the sun was setting, was all level, and like a lake of blood ; and a strong wind came out of that sky, tearing its crimson clouds into frag- ments, and scattering them far into the darkness. And, when Schwartz stood by the brink of the Golden River, its waves were black, like thunder clouds, but their foam was like fire ; and the roar of the waters below and the thunder above met, as he cast the flask into the stream. And, as he did so, the lightning glared in his eyes, and the earth gave way beneath him, and the waters closed over his cry. And the moaning of the river rose wildly into the night, as it gushed over the Two Black Stones, 268 THE KINO OF THE GOLDEN RIVER; CHAPTEE V. HOW LITTLE GlUCK SET OFF ON AN EXPEDITION TO THE GOLDEN River, and how he prospered therein ; with other matters OF INTEREST. " The little king looked very kind," thought he. "I don't think he will turn me into a black stone." So he went to the priest, and the priest gave him some holy water as soon as he asked for it. Then Gluck took some bread in his basket, and the bottle of water, and set off very early for the mountains. If the glacier had occasioned a great deal of fatigue to his brothers, it was twenty times worse for him, who was neither so strong nor so practised on the mountains. He had several very bad falls, lost his basket and bread, and was very much frightened at the strange noises under the ice. He lay a long time to rest on the grass, after he had got over, and began to climb the hill just in the hottest part of the day. When he had climbed for an hour, he got dreadfully thirsty, and was going to drink, like his brothers, when he saw an old man coming down the path above him, looking very feeble, and leaning on a staff. " My son," said the old man, "lam faint HEN Gluck found that Schwartz did not come back, he was very sorry, and did not know what to do. He had no money, and was obliged to go and hire him- self again to the goldsmith, who worked him very hard, and gave him very little money. So, after a month or two, Gluck grew tired, and made up his mind to go and try his fortune with the Golden Eiver. OR, THE BLACK BROTHERS. 2G9 with thirst, give me some of that water." Then Gluck looked at him, and when he saw that he was pale and weary, he gave him the water ; fC Only, pray, don't drink it all," said Gluck. But the old man drank a great deal, and gave him back the bottle two-thirds empty. Then he bade him good speed, and Gluck went on again merrily. And the path became easier to his feet, and two or three blades of grass appeared upon if, and some grasshoppers began singing on the bank beside it ; and Gluck thought he had never heard such merry singing. Then he went on for another hour, and the thirst increased on him so that he thought he should be forced to drink. But, as he raised the flask, he saw a little child lying panting by the roadside, and it cried out piteously for water. Then Gluck struggled with himself, and determined to bear the thirst a little longer ; and he put the bottle to the child's lips, and it drank it all but a few drops. Then it smiled on him, and got up, and ran down the hill ; and Gluck looked after it, till it became as small as a little star, and then turned and began climbing again. And then there were all kinds of sweet flowers growing on the rocks, bright green moss with pale pink starry flowers, and soft belled gentians, more blue than the sky at its deepest, and pure white transparent lilies. And crimson and purple butterflies darted hither and thither, and the sky sent down such pure light, that Gluck had never felt so happy in his life. 270 THE KINO OF THE GOLDEN RIVER; Yet, when he had climbed for another hour, his thirst be* came intolerable again ; and, when he looked at his bottle, he saw that there were only five or six drops left in it, and he could not venture to drink. And, as he was hanging the flask to his j \ belt again, he saw j ^\ a little dog lying jl^ , on the rocks, gasp- (1 tf iug for breath — ^Wk just as Hans had ™^ seen it on the day of his ascent. And Gluck stopped and looked at it, and then at the Golden River, not five hundred yards above him ; and he thought of the dwarf's words, " that no one could succeed, ex- cept in his first \ attempt ; " and he tried to pass the dog, but it whined piteously, and Gluck stopped a^ain. « Poor beastie," said Gluck, " it'll be dead when I come down again, if I don't help it." Then he looked closer and closer at it, and its eye turned on him so mournfully, that he On, THE BLACK BROTHERS. 211 could not stand it. " Confound the King, and his gold too," said Gluek ; and he opened the flask, and poured all the water into the dog's mouth. The dog sprang up and stood on its hind legs. Its tail disappeared, its ears became long, longer, silky, golden ; its nose became very red, its eyes became very twinkling ; in three seconds the dog was gone, and before Gluck stood his old acquaintance, the King of the Golden River. " Thank you," said the monarch ; " but don't be frightened, its all right ; " for Gluck showed manifest symptoms of con- sternation at this unlooked-for reply to his last observation. 4 4 Why didn't you come before," continued the dwarf, "in- stead of sending me those rascally brothers of yours, for me to have the trouble of turning into stones ? Very hard stones they make too." "Oh dear me!" said Gluck, "have you really been so cruel ? " "Cruel ! " said the dwarf, "they poured unholy water into my stream : do you suppose I'm going to allow that ? " " Why," said Gluck, "I am sure, sir — y our majesty, I mean — they got the water out of the church-font." "Very probably," replied the dwarf ; " but," and his coun- tenance grew stern as he spoke, " the water which has been refused to the cry of the weary and dying is unholy, though it had been blessed by every saint in heaven ; and the water which is found in the vessel of mercy is holy, though it had been denied with corpses." So saying, the dwarf stooped and plucked a lily that grew at his feet. On its white leaves there hung three drops of clear dew. And the dwarf shook them into the flask which Gluck held in his hand. "Cast these into the river," he said, * & and descend on the other side of the mountains into the Treasure Valley. And so good speed." As he spoke, the figure of the dwarf became indistinct. The playing colors of his robe formed themselves into a pris- matic mist of dewy light : he stood for an instant veiled with them as with the belt of a broad rainbow. The colors grew faint, the mist rose into the air ; the monarch had evaporated. 272 THE KING OF THE GOLDEN RIVER And Gluck climbed to the brink of the Golden River, and its waves were as clear as crystal, and as brilliant as the sun. And, when he cast the three drops of dew into the stream, there opened where they fell a- small circular whirlpool, into which the waters descended with a musical noise. Gluck stood watching it for some time, very much disap- pointed, because not only the river was not turned into gold, but its waters seemed much diminished in quantity. Yet he obeyed his friend the dwarf, and descended the other side of the mountains, toward the Treasure Valley ; and, as he went, he thought he heard the noise of water working its way under the ground. And, when he came in sight of the Treasure Valley, behold, a river, like the Golden River, was springing from a new cleft of the rocks above it, and was flowing in in- numerable streams among the dry heaps of red sand. And as Gluck gazed, fresh grass sprang beside the new streams, and creeping plants grew, and climbed among the moistening soil.' Young flowers opened suddenly along the river-sides, as stars leap out when twilight is deepening, and thickets of myrtle, and tendrils of vine, cast lengthening shadows over the valley as they grew. And thus the Treasure Valley became a garden again, and the inheritance which had been lost by cruelty was regained by love. And Gluck went and dwelt in the valley, and the poor were never driven from his door : so that his barns became full of corn, and his house of treasure. And, for him, the river had, according to the dwarf's promise, become a River of Gold. And, to this day, the inhabitants of the valley point out the place where the three drops of holy dew were cast in- to the stream, and trace the course of the Golden River under the ground, until it emerges in the Treasure Valley. And at the top of the cataract of the Golden River are still to be seen two black stones, round which the waters howl mournfully every day at sunset ; and these stones are still called by the people of the valley The Black Brothers. DAME WIGGINS OF LEE. AAD HER SEVEN WOiNDERFUL CATS. A HUMOUROUS TALE, WRITTEN PRINCIPALLY BY A LADY OF NINETY. EMBELLISHED WITH EIGHTEEN COLOURED ENGRAVINGS, VBIKTED FOB A. K. NEWMAN & Co. LEA DENH ALL-STREET. 1823. DAME WIGGINS of Lee Was a worthy old soul, As e'er threaded a nee- die, or wash'd in a bowl : She held mice and rats In such antipa-.thy ; That seven fine eats Kept Dame Wiggins of Lee. The rats and mice scared By this fierce whisker' d crew, The poor seven cats Soon had nothing to do ; So, as anv one idle She ne'er loved to see, She sent them to school. Did Dame Wiggins of Lee* The Master soon wrote That they all of them knew How to read the word " milk " And to spell the word u mew." And they all washed their faces Before they took tea : * Were there ever such dears 1 9 Said Dame Wiggins of Lee. 3 He had also thought well To comply with their wish To spend all their play-time In learning to fish For stitlings ; they sent her .A present of three, Which* fried, were a feast For Dame Wiggins of Lee* But soon she grew tired Of living alone ; So she sent for her eats From school to come home* Each rowing a wherry, Returning yon see : The frolic made merry Dame Wiggins of Lee 0 Hie Dame was quite pleas'd, And ran out to market; When she came back They were mending the carpet. The needle each handled As brisk as a bee ; M Well done, my good eats/' Said Dame Wiggins of Lee* To give them a treat, She ran out for some rice ; When she came back, They were skating on ice. " J shall soon see one down^ Aje 7 perhaps 5 two or three, 1 ? U bet half-a-crown 3 ,f Said Dame Wiggins of Lee. 7 When spring-time came bade They bad breakfast of curds s And were greatly afraid Of disturbing the birds. " If you sit, like good eats, All the seven in a tree. They will teach you to sing S Said Dame Wiggins of Lee, s So they sat in a tree, And said "Beautiful! Hark ! " And they listened and looked In the clouds for the lark. Then sang, by the fireside, Syniphonious-ly, A song without words To Dame Wiggins of Lee. They called the next day On the tomtit and sparrow, And wheeled a poor sick lamb Home in a barrow* " You. shall all have some sprats For vour humani-tv. My seven good cats, 9 * Said Dame Wiggins of Lee, While she ran to the field, To look for its dam $ They were warming the bed For the poor sick Iamb : They turn'd up the clothes All as neat as could be ; " I shall ne'er want a nurse, Said Dame Wiggins of Lee. IE She wished them good night, And went up to hod : When, lo ! in the morning. The cats were all fled. But soon — what a ftiss ! ** Where can thev all be ? Here, pussy, puss, puss ! " Cried Dame Wiggins of Lee/ The Dame's heart was nigh broke. So she sat down tar weep, When she saw them come hack Each riding' a sheep : She fondled and patted Each purring 1 Tom -my : " Ah ! welcome, my dears/' Said Dame Wiggins of Lee, The Dame was unable Her pleasure to smother ; To see the sick Lamb Jump up to its mother* la spite of the gout, And a pain in her knee, She went dancing about ; Did Dame Wiggins of Lee. The Farmer soon heard Where his sheep went astray, And arrived at Dame's door With his faithful dog Tray. He knocked with his crook 5 And the stranger to see, Out of window did look Dame Wiggins of Lee 6 For their kindness he had them All drawn by his team ; And gave them some field- mice, And raspberry- cream. Said he, " All mv stock You shall presently see ; Eor I honour the cats Of Dame Wiggins of Lee " i6 Me sent' his maid out For some muffins and crumpets ; And when lie turn'd round They were Mowing of trumpets* Said he* 66 1 suppose* She's as deaf as can be* Or this ne'er could be borne By Dame Wiggins of Lee/* i7 To show them his poultry, He -turn'd them all loose. When each nimbly leap'd On the back of a Goose* Which fnghten'd them so That they ran to the sea, And half- drown 9 d the poor cats Of Daine Wiggins of Lee. IS For the care of his Iamb, And their comical pranks, He gave them a ham And abundance of thanks. " i wish you good-clay, My- fine fellows/' said he; " My compliments, pray, To Dame Wiggins of Lee; 19 * You see them arrived At their Dame's welcome door ; They show her their presents, And all their good store. " New come in to supper, And sit down with me ; Ail welcome once more/* Cried Dame Wiggins of Lee, 20 THE EAGLE'S NEST TEN LECTURES ON THE RELATION OF NATURAL SCIENCE TO ART GIVEN BEFORE THE UNIVERSITY OF OXFORD IN LENT TERM, 1872 PREFACE. The following Lectures have been written, not with less care but with less pains, than any in former courses, because no labour could have rendered them exhaustive statements of their subjects, and I wished, therefore, to take from them every appearance of pretending to be so : but the assertions I have made are entirely deliberate, though their terms are unstudied ; and the one which to the general reader will ap- pear most startling, that the study of anatomy is destructive to art, is instantly necessary in explanation of the system adopted for the direction of my Oxford schools. At the period when engraving might have become to art what printing became to literature, the four greatest point- draughtsmen hitherto known, Mantegna, Sandro Botticelli, Durer, and Holbein, occupied themselves in the new industry. All these four men were as high in intellect and moral senti- ment as in art-power ; and if they had engraved as Giotto painted, with popular and unscientific simplicity, would have left an inexhaustible series of prints, delightful to the most innocent minds, and strengthening to the most noble. But two of them, Mantegna and Durer, were so polluted and paralyzed by the study of anatomy that the former's best yorks (the magnificent mythology of the Vices in the Louvre, for instance) are entirely revolting to all women and children ; while Durer never could draw one beautiful female form or face ; and, of his important plates, only four, the Melencholia, St. Jerome in his study, St. Hubert, and Knight and Death, are of any use for popular instruction, because in these only, the figures being fuliy draped or armed, he was enabled to 300 PREFACE. think and feel rightly, being delivered from the ghastly toil of bone-delineation. Botticelli and Holbein studied the face first, and the limbs secondarily ; and the works they have left are therefore with- out exception precious ; yet saddened and corrupted by the influence which the contemporary masters of body-drawing exercised on them ; and at last eclipsed by their false fame. I purpose, therefore, in my next course of lectures, to explain the relation of these two draughtsmen to other masters of de- sign, and of engraving. Bbantwood, Sept. 2nd, 1872. THE EAGLE'S NEST. LECTUKE I. OF WISDOM AND FOLLY IN ART.* 8th February, 1872. 1. The Lectures I have given hitherto, though, in the matter of them conscientiously addressed to my undergraduate pu- pils, yet were greatly modified in method by my feeling that this undergraduate class, to which I wished to speak, was indeed a somewhat imaginary one ; and that, in truth, I was addressing a mixed audience, in greater part composed of the masters of the University, before whom it was my duty to lay down the principles on which I hoped to conduct, or pre- pare the way for the conduct of, these schools, rather than to enter on the immediate work of elementary teaching. But to-day, and henceforward most frequently, we are to be en- gaged in definite, and, I trust, continuous studies ; and from this time forward, I address myself wholly to my under- graduate pupils ; and wish only that my Lectures may be ser- viceable to them, and, as far as the subject may admit of it, interesting. 2. And, farther still, I must ask even my younger hearers to pardon me if I treat that subject in a somewhat narrow, and simple way. They have a great deal of hard work to do in other schools : in these, they must not think that I underrate their powers, if I endeavour to make everything as easy to * The proper titles of these lectures, too long for page headings, are given in the Contents. 302 THE EAGLE'S NEST. them as possible* No study that is worth pursuing seriously can be pursued without effort ; but we need never make the effort painful merely for the sake of preserving our dignity. Also, I shall make my Lectures shorter than heretofore. What I tell you, I wish you to remember ; and I do not think it possible for you to remember well much more than I can easily tell you in half-an-hour. I will promise that, at all events, you shall always be released so well within the hour, that you can keep any appointment accurately for the next. You will not think me indolent in doing this ; for, in the first place, I can assure you, it sometimes takes me a week to think over what it does not take a minute to say : and, secondly, believe me, the least part of the work of any sound art-teacher must be his talking. Nay, most deeply also, it is to be wished that, with respect to the study which I have to bring before you to-day, in its relation to art, namely, natural philosophy, the teachers of it, up to this present century, had done less work in talking, and more in observing : and it would be well even for the men of this century, pre-eminent and accomplished as they are in accuracy of observation, if they had completely conquered the old habit of considering, with respect to any matter, rather what is to be said, than what is to be known. 3. You will, perhaps, readily admit this with respect to science ; and believe my assertion of it with respect to art. You will feel the probable mischief, in both these domains of intellect, which must follow on the desire rather to talk than to know, and rather to talk than to do. But the third domain, into the midst of which, here, in Oxford, science and art seem to have thrust themselves hotly, like intrusive rocks, not without grim disturbance of the anciently fruitful plain your Kingdom or Princedom of Literature ? Can we carry our statement into a third parallelism, for that ? It is ill for Science, we say, when men desire to talk rather than to know ; ill for Art, when they desire to talk rather than to do. HI for Literature when they desire to talk, — is it? and rather than — what else ? Perhaps you think that literature means nothing else than talking ? that the triple powers of science, art, and scholarship, mean simply the powers of knowing, TEE EAGLE'S NEST. 303 doing, and saying. But that is not so in any wise. The faculty of saying or writing anything well, is an art, just as much as any other ; and founded on a science as definite as any other. Professor Max Midler teaches you the science of language ; and there are people who will tell you that the only art I can teach you myself, is the art of it. But try your triple parallelism once more, briefly, and see if another idea will not occur to you. In science, you must not talk before you know. In art, you must not talk before you do. In litera- ture, you must not talk before you — think. That is your third Province. The Kingdom of Thought, or Conception. And it is entirely desirable that you should define to your- selves the three great occupations of men in these following terms : — Science The knowledge of things, whether Ideal or Substantial. Art o ......... . The modification of Substantial things by our Substantial Power. Literature ..... The modification of Ideal things by our Ideal Power. 4. But now observe. If this division be a just one, we ought to have a word for literature, with the ' Letter ' left out of it. It is true that, for the most part, the modification of ideal things by our ideal power is not complete till it is ex- pressed ; nor even to ourselves delightful, till it is communi- cated. To letter it and label it — to inscribe and to word it rightly, — this is a great task, and it is the part of literature which can be most distinctly taught. But it is only the formation of its body. And the soul of it can exist without the body ; but not at all the body without the soul ; for that is true no less of literature than of all else in us or of us — "litera occidit, spiritus autem vivificat." Nevertheless, I must be content to-day with our old word* We cannot say * spiriture ' nor ' animature,' instead of litera- ture ; but you must not be content with the vulgar interpret 304 THE EAGLE'S NEST. tation of the word. Remember always that you come to this University, — or, at least, your fathers came, — not to learn how to say things, but how to think them. 5. " How to think them ! but that is only the art of logic," you perhaps would answer. No, again, not at all : logic is a method, not a power ; and we have defined literature to be the modification of ideal things by ideal power, not by me- chanical method. And you come to the University to get that power, or develope it ; not to be taught the mere method of using it. I say you come to the University for this ; and perhaps some of you are much surprised to hear it ! You did not know that you came to the University for any such purpose. Nay, perhaps you did not know that you had come to a Uni- versity at all ? You do not at this instant, some of you, I am well assured, know what a University means. Does it mean, for instance — can you answer me in a moment, whether it means — a place where everybody comes to learn something ; or a place where somebody comes to learn everything? It means — or you are trying to make it mean — practically and at present, the first ; but it means theoretically, and always, the last ; a place where only certain persons come to learn everything ; that is to say, where those who wish to be able to think, come to learn to think : not to think of mathematics only, nor of morals, nor of surgery, nor chemistry, but of everything, rightly. 6. I say you do not all know this ; and yet, whether you know it or not, — whether you desire it or not, — to some ex- tent the everlasting fitness of the matter makes the facts con- form to it. For we have at present, observe, schools of three kinds, in operation over the whole of England. We have — I name it first, though, I am sorry to say, it is last in influence — the body consisting of the Royal Academy, with the Insti- tute of Architects, and the schools at Kensington, and their branches ; teaching various styles of fine or mechanical art. We have, in the second place, the Royal Society, as a central body ; and, as its satellites, separate companies of men de- voted to each several science : investigating, classing, and THE EAGLE'S NEST. 305 describing facts with unwearied industry. And, lastly and chiefly, we have the great Universities, with all their subordi- nate public schools, distinctively occupied in regulating, — as I think you will at once admit, — not the language merely, nor even the language principally, but the modes of philosophical and imaginative thought in which we desire that youth Should be disciplined, and age informed and majestic. The methods of language, and its range ; the possibilities of its beautv, and the necessities for its precision, are all dependent upon the range and dignity of the unspoken conceptions which it is the function of these great schools of literature to awaken, and to guide. 7. The range and dignity of conceptions ! Let us pause a minute or two at these words, and be sure we accept them. First, what is a conception ? What is this separate object of our work, as scholars, distinguished from artists., and from men of science ? "We shall discover this better by taking a simple instance of the three agencies. Suppose that you were actually on the plain of Paestum, watching the drift of storm-cloud which Turner has here engraved.* If you had occupied yourself chiefly in schools of science, you would think of the mode in which the elec- tricity was collected ; of the influence it had on the shape and motion of the cloud ; of the force and duration of its flashes, and of other such material phenomena. If you were an artist, you would be considering how it might be possible, with the means at your disposal, to obtain the brilliancy of the light, or the depth of the gloom. Finally, if you were a scholar, as distinguished from either of these, you would be occupied with the imagination of the state of the temple in former times ; and as you watched the thunder-clouds drift past its columns, and the power of the God of the heavens put forth, as it seemed, in scorn of the departed power of the god who was thought by the heathen to shake the earth — the utterance of your mind would become, whether in actual * Educational Series, No. 8 ? E, 306 THE EAGLE'S NEST. words or not, such as that of the Psalmist : — u Clouds and darkness are round about Him — righteousness and judgment are the habitation of His throne." Your thoughts would take that shape, of their own accord, and if they fell also into the language, still your essential scholarship would consist, not in your remembering the verse, still less in your knowing that "judgment" was a Latin word, and "throne" a Greek one ; but in your having power enough of conception, and elevation enough of character, to understand the nature of justice, and be appalled before the majesty of dominion. 8. You come, therefore, to this University, I repeat once again, that you may learn how to form conceptions of proper range or grasp, and proper dignity, or worthiness. Keeping then the ideas of a separate school of art, and separate school of science, what have you to learn in these ? You would learn in the school of art, the due range and dignity of deeds ; or doings — (I prefer the word to "makings," as more general) ; and in the school of science, you would have to learn the range and dignity of knowledges. Now be quite clear about this : be sure whether you really agree with me or not. You come to the School of Literature, I say, to learn the range and dignity of conceptions. To the School of Art, to learn the range and dignity of Deeds. To the School of Science to learn the range and dignity of Knowledges. Do you agree to that, or not? I will assume that you admit my triple division ; but do you think, in opposition to me, that a school of science is still a school of science, whatever sort of knowledge it teaches ; and a school of art still a school of art, whatever sort of deed it teaches ; and a school of literature still a school of literature, whatever sort of notion it teaches ? Do you think that ? for observe, my statement denies that. My statement is, that a school of literature teaches you to have one sort of conception, not another sort ; a school of art to do a particular sort of deed, not another sort ; a school THE EAGLE'S NEST. 307 of science to possess a particular sort of knowledge, not an- other sort. 9. I assume that you differ with me on this point ; — some of you certainly will. Well then, let me go back a step. You will all go thus far with me, that — now taking the Greek words — the school of literature teaches you to have vovs, or concep- tion of things, instead of avota, — no conception of things ; that the school of art teaches you r^vy of things, instead of areata ; and the school of science, lirLa-rrnx-q, instead of dyvota or 'ignorantia.' But, you recollect, Aristotle names two other faculties with these three, — ^povrjats, namely, and ia. He has altogether five, tc^vt/, l-nuTTr]^, p6vr)o-is, o-o<£ux, vovs ; that is to say, in simplest English, — art, science, sense, wisdom, and wit. We have got our art, science, and wit, set over their three domains ; and we old people send you young ones to those three schools, that you may not remain artless, science- less, nor witless. But how of the sense, and the wisdom ? What domains belong to these ? Do you think our trefoil division should become cinquefoil, and that we ought to have two additional schools ; one of Philosophia, and one of Philo- phronesia ? If Aristotle's division were right it would be so. But his division is wrong, and he presently shows it is ; for he tells jou in the next page, (in the sentence I have so often quoted to you,) that " the virtue of art is the wisdom which consists in the wit of what is honourable." Now that is per- fectly true ; but it of course vitiates his division altogether. He divides his entire subject into A, B, C, D, and E ; and then he tells you that the virtue of A is the B which consists in C. Now you will continually find, in this way, that Aris- totle's assertions are right, but his divisions illogical. It is quite true that the virtue of art is the wisdom which consists in the wit of what is honourable ; but also the virtue of sci- ence is the wit of what is honourable, and in the same sense, the virtue of vovs, or wit itself, consists in its being the wit or conception of what is honourable. 2o<£ia, therefore, is not only the dperrj t€x^9, but, in exactly the same sense, the apcn} c7rto-rr;/xr/9, and in the same sense, it is the dperrj voov. And if not governed by