r/i & = •• . 0 \ !. I f Digitized by the Internet Archive in 2018 with funding from Getty Research Institute https://archive.org/details/philosophicaltraOOsche •Jr PHILOSOPHICAL TRANSACTIONS. GIVING SOME ACCOUNT O F T H E Trejent Undertakings, Studies > and Labours OF THE INGENIOUS, IN MANY Confiderable Parts of the World. V o l. XXXV. For July, Attgufl, September ? Octo¬ ber, November and ©ecember 172,7, and for the Year 17x8, LONDON: Printed for W. Innys, Printer to the Royal Society , at the IVeft End of St. Paul's. M . DCC. XXIX. \ TO HIS royal highness FREDERICK Prince o {WALES. SIR, S INCE your Royal Highness has gracioufly condefcended to in- fcribe Your Name in the Book of Charters and Laws of the Royal Society , as a Token of your Favour and Encourage¬ ment of it, I prefume to offer this Thirty- fifth Volume of Thilofophical T'ran facti¬ ons t fome of its lateft Productions, to your Royal Highness’s more immedi¬ ate Protection. This alone would be fufficient Honour to the feveral Authors of the TraCts con¬ tained in it: But they muft ftill have a pri¬ vate Satisfaction in knowing, that they are a fub- - DEDICATION. fubmitted to the Obfervation of a Prince, whofe Difcernment renders him a compleat Judge of the Merits of their Labours; and whofe Benevolence, at the fame Time, will readily incline Him to think favourably of them. If, befides this, they fhould chance to furnilh any Matter for your learned, or in¬ genious Entertainment, I beg your Royal Highness to receive it, as one In- ilance of the grateful Senfe conceived of the late Honour done us, and particular¬ ly, of the profound Refpeft, with which I am. Tour Royal Highness’s O ■ »ifl Moji Devoted^ Obedient , and Humble Servant , William Rutty, R. S, Seer . / \ ft gm &qCP. Numb. 406. PHILOSOPHICAL TRANSACTIONS FOR THE Month of DECEMBER, 17x8. The CONTENTS. L (Remarks on the Height of Mountains in general, and of thofe of Swiflerland in particular, with an Account of the Rife of fome of the mofl conjide- rable Rivers of Europe. By J. G. Scheuchzer, M. T>. See. II. Optical Experiments made in the Beginning of Auguft 1718, before the Brejident and feveral Members of the Royal Society, and other Gentle¬ men of feVeral Nations, upon Occafion of Signior Rizzetti’r Opticks, with an Account of the faid Book, By J. T. Defaguliers, L L. B. and F. % S. a ^ III. The The CONTENTS. III. The Method of making Tin-Plates, extracted from the Memoirs of the Academy of Sciences , for the Tear 1715, by William Rutty, M. T>. Of S. Seer. IV. A Letter from the (Reverend Mr. James Brad¬ ley SaVilian Trofeffor of Aflronomy at Oxford, andF.%S. to £)r.Edmund Halley Aftronom. Reg. See. giving an Account of a new dif- coVered Motion of the Fixt Stars. ( 577 ) I. Remarks on the Height of Mountains in general, and of thofe of SwifTerland in particular, with an Account of the Ejfe of fome of the mofl conjide- rable Quivers of Europe. By J. G. Scheuchzer, M. T>. &c. I N a former Paper, I took Notice that ‘Dicaarchus found Mount Telius in TheJfalia , to be 115*0 Pa¬ ces high, which make 615*0 Roman , or 6811 Tar is Feet, a Height which we may well pronounce too great even for the abfolute Height of Mount Telius , I mean its Rife above the Level of the Sea. Conform to the Determination of ‘Dicaarchus , I mentioned, that Tint arch fixes the Height of the higheft Mountains, and the greateft Depth of the Sea to 10 Stadia, and Cleomedes affirms, that they cannot exceed 16 Stadia. The celebrated Galileus de Galileis is one of the moft modeft among the modern Writers on this Head: For he fays, * that the higheft Mountains do not rife above a Mile, or 8 Stadia, or ?ooo old Roman Ve/pafian Feet, which make f^VParis Feet above the Level of the Sea, which we fhall find by and by to agree pretty well with fome of the higheft Mountains in France , and may conjecture to do fo with thofe in Italy. Kepler went rather too far f when he affigned the Mountains of Rhcetia (thought the higheft in Swijferland) a Height of 16 Stadia, or 10000 old Roman Vefpajian Feet, which make 10916 Tar is Feet. The Opinions of fome other antient and modern Geographers and Ma¬ thematicians, will appear better by the Table annexed. * Nuntius Sidereus, p. 14. t Aftronom. Optic, p. 129, 135* & Epitom. Aftronoin. lib I. pag. 2 6 . H h h h A Table ( 578 ) A Table ihewing the Height of Mountains according to feveral antient and modern Writers. Strabo ( Lib. II. Geog .) fays, that the higheft Mountain,call¬ ed by him (Petra Sogdiana , is of - - - \Pererius {Lib. XII. in Ge-') nejin) determines the higheft > Mountains to -5 Leo Baft. Albertus (Architect, p Lib . x. Cap. i.) to - * c Ath. Kircher. (Ars magn. luc. a & umbr. (P. II. Trobl. 5.) C brings them to - - 3 Fromond. (Lib. I. Meteor. Cap A 2. Art. i. - - 3 Gilbertus de magnete. L. IV. C. i. iPliny (Lib. III. Cap. lxiv.) ac¬ cording to the Explanation of Fortunius Licetus (de Luna} Luce fubobfcura, Lib. II. p. I 306.) to - - -J Ricciolus, Geophr. (Lib. VI.) is of^ .Opinion, in Furfuance of what he imagines to have demon- ftrated of the Mountains A- thos and Caucafus , that pofli- bly there may be Mountains of * • Stadia.jOld Roman Paris Feet. Vefpajian Feet. 30 187*0 20468 3* 20000 21832 22500 23661 43 26875 *9337 64 4OOOO 43664 128 80000 87328 400 25OOOO 272900 yix 320000 349312 Now, ( 579 ) Now, in Oppofition to this Table, wherein the Heights muft needs, upon firft View, appear romantick and unnatural, let us confider the Height of fuch Moun¬ tains, as have been meafured,either by Trigonometrical or Barometrical Obfervations. In England , the Height of Snowdon-hill, one of the higheft Mountains in Wales , was meafured Trigo¬ nometrically, by Mr. J. Cafwell of Oxford, and found to be of 1240 Yards, or 3710 Engl'tjb Feet, which make 3488 Ear is Feet. At the Top of this Mountain, the Mercury fubfided to 2.$" 6 ’", which being redu- cedto Earis Meafure, make juft 24". Now in the Tables above, the Height of the Place where the Mer¬ cury fubfides to 24//, is, according to Mariotte, of 744 Toifes, two Foot, or 3266 Foot above the Level of the Sea, according to CaJJini , 676 Toifes, or 405 6 Feet, and according to my Uncle’s Calculation 559 0 2', or 335<5/, fo that Mariotte comes 222 Feet fhort of its Height, as it was determined Trigonometrically, Dr. Scheucbzer but 132', but Cajfmi exceeds this Height by 568 Feet, which confirms again, as I have fhewn in a former Paper, that the Mariottian Table is preferable to that of Cajfmi, though pretended to have been corrected upon the former, and that that of Dr. Scheucbzer is an Improvement upon both. According to the Obfervation made by Dr. Halley , May 26,1697, the Mercury flood at the Top of, Snowden-bill, at 2 6" F" Englifb , which, if reduced as above, would give the Height of the Mountain fomething lefs. In France , when the Meridian Line, firft begun in 1669, was continued in 1703, the Heights of feveral Mountains, particularly in the South of France, were determined Trigonometrically by the Members of the H h h h 2 Royal ( 5 8 ° ) Royal Academy of Sciences: And I find up and down in their Memoirs, the Heights of the following. Height in Toifes. Feet. 277 or 1662 397 — 2-382 408 — 2448 Mont Clairet in Brovence La Majfane in RouJJilion - - The fame according to another - ! Obfervation ... - -y Bugarach , a Mountain in Lan -7 gitedoc - - - -$ Mountains in Auvergne. Le Buy de Domme, near Clermont La Courlande La Cofie Le Buy de Violent Le Cantal ... Le Mont d’ or • In the County of Avignon. Le Mont ventoux - - 1036 Pyrenean Mountains. S. Barthelemy dans le poke? Q a, fnix . . X II8 ? ~ 71 de foix La Montagne du Mouffet Le Canigou 648 — 3888 810 — 4860 838 — 5028 851 — 5106 8 f 3 —• 5118 984 — 5 ’ 9°4 1030 — 6180 6zi6 10 1158 — 7548 1440 — 8640 Before I proceed farther, I muft beg Leave to obferve, that the Heights of thefe Mountains, in the main, feem rather too great. This indeed is eafily accounted for, as they were meafured byTrigonometrical Obfervations, which will, as I have took Notice above,becaufe of the Re- ( J8* ) Refraction of the Air, give the Heights greater than they actually are. But what confirms it ftill more, is, that according to the Tables above, the Numbers which anfwer to the Heights of the Mercury, as they were obferved at the Top of fome of thtpfe Mountains, are confiderably lefs, and that even Monf. Cajfini's own Numbers, which yet we have by fome undoubted Ex¬ periments (hewn to be too great, fall often Ihort. It will be enough to mention two or three Inftances. At the Tower of Majfane in RouJJillon$\z Mercury flood at 25 '' S 1 '' 1 and the Height of that Place was deter¬ mined trigonometrically, of - - 39,7 Toifes. Now 2.5'' <" r anfwer according? Mariotte, to " * S ° According to CaJJini , - - 392 4 According to Dr. Scheuchzer - - 3 70 o At the Top of the Mountain called la Cofle in Au¬ vergne, the Mercury flood, 0 £l. 9,1700, at 2 and the Height of this Mountain was determined Tri¬ gonometrically of Now 23 // 4"' anfwer ac-~) cording to Mariotte,to j Caffint Dr. Sbeuchzer - - The Difference is ftill more - confiderable withRegardto the high MoontamMontdl l rp - r or toAuvergne,th.e\He\g\\t I ~ ~ I 0 -l° 01 ‘ es whereof was determin- / ed Trigonometrically to J Toifes. differ. 206° At < 581 ) At the Top of this Mountain the Mercury fell, ac¬ cording to an Obfervation made by F. Sebajlien Truchet, June 8,1705-, to 22^ uwhich anfwer according to Mariotte ,to • 707° 5^ C3 32Q i> Cajfmi to - - 9x5 1 ^differ .< 114 5 Dr. Scheuchzer - 717 3 j £311 3 I come now to the Mountains of Swijferland. The Barometrical Obfervations made by my Father upon ieveral of the higheft will convince us, that they rife aloft, above all the neighbouring ones in France,Spain, Italy and Germany. And that it mull be fo appears farther, becaufefrom their elevated Tops, they difpenfe their Waters to all the European Kingdoms and Pro¬ vinces around them. Nay, I doubt not, but that they may vye in Height with the moft confiderable Mountains in any other Part of the known Globe. Swijferland it felf, I mean its Valleys and lower Parts, as they are confiderably remote from the Sea, rife alfo in Propor¬ tion above the Level of it. ’Tis true, the Afcent thi¬ ther is but gradual, in Proportion to the Remotenefs. At Zur'tc, for Inftance,which lies towards the Northern Borders of Swijferland, the mean Height of the Baro¬ meter hath been obferved of 16" p», which give the Elevation of that Town, above the Level of the Sea, according to Mariotte , 105- Toifes, 4 Foot, or 1234', according to Dr. Scheuchzer, zio° 4L or 1164', and according to CaJJini, 211° 4', or 1330'. This Town is diftant from the Mouth of the Rhine, which is the neareft Part of the Ocean, at leaft 3 75- Englijk Miles, or an hundred marine French Leagues, and from Ge¬ noa which is neareft upon the Mediterranean, 225 En- 1 glijh ( 58 1 ) glijb Mile?, or 6z French marine Leagues. So that go¬ ing down from Zuric Northwards towards the Sea, the Defcent, or Fall, is but fomething more than iz Foor, .’for a marine League of France , if we fuppofea ftreight Line to be drawn from Z uric to the Sea-fhore in Hol¬ land \ but it is much greater going Southward towards the Mediterranean, where it comes at leaft to zo Foot for one League. Nay, if we confider that the high- eft Mountains of Swijferland lie almoft dire&ly be¬ tween Zuric and the Mediterranean Shores, we muft allow fo much more in Proportion, as thofe Mountains are elevated above the Horizon of Zuric , and how great and fudden this Elevation be, will appear by the following Obfervations. At Ennen Sewen gen Aweren in the Afcent of the high Mountain Freyberg, in the Canton of Glarus , which lies South Eaft of Zuric , the Mercu¬ ry was obferved Sept, it, *710, at 23" 10'", which gives the Height of that Place above the Level of the Sea, according to Mariotte - - 569° 2' or 3416' Dr. Scheuchzer - 584 4 — 35-08 Cajfmi - - - l\z 3 — 4275 Upon Scherf, one of the Branches of the Freyberg, the Mercury fell Sept. 12,1710, to 21" 8'", which gives the Height of that Part of the Mountain according to Mariotte - - 906° 1' or 543 7' Dr. Scheuchz>er - - 931 2 or 5588 CaJJini • - - . 1247 4 or 7486 Still C 5*4 ) Still higher upon Blattenjlock, another Part of the fame Mountain, the Mercury fell on the fame Day to 21" 6 '", which anfwer according to Mariotte, to - - 933 0 2' or $600' Dr. Scheuchzer - - 95-9 2 or 575-6 CaJJini - - 1293 3 or 7761 Hence from Zuric to the Blattenjlock near the Top of the Freyberg, there is, in lefs than three Days Journey, a Rife of 4366 Feet, according to Mariotte , and 4492, according to Dr. Scheuchzer, that is, more than three times the Elevation of Zuric above the Le¬ vel of the Sea. At Gujpen ob Schwanden, in the fame Canton of Glarus, the Mercury was obferved, Augujl 5, 1705-, at 23" 4"', which give, according to Mariotte - - 644° 1' or 3865' Dr. Scheuchzer - - 661 5 or 3971 (I omit giving the Numbers according to the Tables of Mr. Cajfini , having already {hewn, that they are too great) The Height of this Mountain is nearly the fame with the celebrated Buy de Domme, where Monf. Terier obferved the Mercury, Sejt. 19, 1648, at 23 " 2'". Upon Joch , a high Mountain in the Territory of En- gelberg , where it confines upon the Canton of Bern , full South of Zuric, the Mercury flood, June 23, 1706, at 21" 4"', which gives the Height of that Mountain according to Mariotte - - 961° o' or $766 Dr. Sheuchzer, - - 987 4 or 5-926 This Mountain, though very high, is far from being the higheft in that Neighbourhood, for next to it there ( 5 8 * ) there rifes another called the Titlisberg, , covered with everlading Snow, which we may, upon a moderate Computation, pronounce at lead 1000 Foot higher than the Top of the Joch , and confequently one of the higheft in the Country, Upon the Avicula , by the Italians called Monte del ’ Uccello , and by fame S. Bernhard's Mountain, from a Chappel built in Honour of that Saint, a high Mountain in Rhoetia , towards Italy , the Mercury was obferved, July 30, 1707, at 22" n'", which give ac¬ cording to Mariotte - - 707° 5' or 4247' Dr .Scheuchzer - - 727 3 4365 s This Height mud be underdood only of that Part of the Mountain which is paffed over by Travellers, the Mountain it felf riling confiderably above it, andthe^- dula^o r of Strabo>Gz og. L. III. of which the Avicula is only a Part, being dill higher. The Rhenus pofterior , or Hinder Rhein , and the Moiifs , which at lad lofes itfelf into the Tejin , near Beilin - not much above the Entry of the Tejin into the Lake of Locarno , arife upon this Mountain. At Santa Maria , upon the Luckmannier Berg , by fome S. BarnabJ s Mountain, which is likewife a Branch of the Adula^ the Mercury dood^/£. 9, 1725 s , as upon the Avicula, , at 22" n'", which diews the Height of thefe two Places to be equal. In the Alp jPtfr/^,near the Source of the Hinter Rhein ,, Rhenus pojlerior , five Hours and a half from Speluga^ Splugen in Rhoetia , the Mercury was ob¬ ferved, July 29, 1707, at 21" 4'", where it dood like¬ wife upon the above-mentioned Mountain whi¬ ther the Reader is referred for the Height of this Alp. I i i i - At ( ) At Splugen itfelf, the Mercury flood the fame Morn¬ ing early, at X3" 4'", which give the Elevation of Spliigen according to Mariotte 644° P or 3865, and according to Dr. Scheuchzer , 66 1° 5' or 3971'. So that the Fall of the Rhine from the Aip aforefaid to Splugen , in five Hours and a half, comes, according to Mariotte\ to 1901, and according to Dr. Scheuchzer , to 1955 Faris Feet perpendicular. At the Capuchins, upon the high Mountain S. Gothardj a celebrated PaiTage out of Swifferland into Italy , the Mercury flood, 30, 1705, at n" o, which gives the Height of that Paflage, which with Regard to the higheft Tops of S. Gothard , lies but as it were at the Foot of a high Mountain, according t o Mariotte 85^°, or 5 nx', and according to Dr. Scheuchzer , 875° 5', or 5x55, above the Level of the Sea. Upon the Furca , a high Mountain between the Urferen Thai , Urfaria Vallis , and the upper /e/K?, and one of the Branches of the S. Gothard , the Height of the Mercury in the Barometer was obferved, July , 31, 1707, atxP' 5'", which give the Height of this Mountain above the Level of the Sea, according to Mariotte , 947 0 Per 5683', and according to Dr. Scheuchzer , 973 0 3' Or 5841. Near this Mountain there are others, which cannot be lefs than 800 or 900 Foot higher. Thefe Mountains, I mean the Avicula> the Luck - mannier Berg , the S. Gothard , and the Furca , toge¬ ther with the Grimfula , the Crifpalt , the Sempronier , or Sempronius Mons , the Adula , and a Chain of others, are the Lepont'ue Alpes of Fliny * and the Summa t * Lib. iii. c. xx* Alpes ( 587 ) Alpes of Cafar * They begin in the upper Valle/ia , traverfe the Canton of ri t and fo run on Ea ft wards, a-crofs the Country of the Grifoons , towards Tirol. Their greateft Height above the Level of the Sea, may be fixed in round Numbers to 7500, or 8000 Faris Feet. 5 f is upon thefe very Mountains, that fome of the moft confiderable Rivers of Europe take their firft Rife, within very fmall Diftances of each other. The Rhojhefov Inftance, Rhodanus , by Marc Minus call¬ ed, maximi nominis flumen , and by Varro , Fluvius inter tres Europe maximus , arifes from two Gletch* ers , as we call them, or Montes glaciates^ huge Moun¬ tains of Ice , near the Furca, whofe Height hath been above determined, and thence runs with great Impetu- ofity down Vallefia , the Walii(ferland, forming a long Valley, furrounded on both Sides with huge Mountains, till it loofes its Waters and Name in the La - cus Lemannus , or Lake of Geneva, , but refumes it again near the Town of Geneva, whence it flows with a more gentle Defcent through fome Provinces of France into the Mediterranean Sea. The The fin, Ticinus , by Claudian , in his Pane¬ gyric upon the Confulate of the Emperor Honorius , called Fulcher , the handfom , takes its firft Rife from two fmall Lakes upon the S. Gothard , and fome late¬ ral Sources from the Lago fopra la Cima di Fettine , upon a Mountain called Fettine, the Lago della Sella, the Lake of Rottom upon the Luckmannier Berg, the Lake of Tom , and the Lake of Bedretto, upon a Moun¬ tain of this Name. It defcends the Lavinia Vallis , or Liviner Valley , and in its Way to the Lake of * De Eello Gallico 1. iii. I i i i a Lo- ( J88 ) Locarno , receives many Brooks and Rivulets from the adjoining Mountains : It unites its Waters with the *p0) near Ravia , and loofes itfelf jointly with that River into the Adriatick Gulf. The Rhine, Rhenus , by Cafar de Bello Galileo termed, latijfimus atque altijjimus , arifes in three fe- veral Branches, which are called Rhenus anterior , fofterior , & medius , the further , the hinder , and middle Rhine. The hinder Rhine takes its Rife upon the high Mountain Avicula^ Colmen del Occello , Part of the Adula, in the Alp San Rorta , from a Gletcher , or Ice-mountain, which extends in Length full two Hours. The middle Rhine , Rhenus medius , arifes upon the Luckmannier Berg , which is likewife Part of the Adula , in the upper Part of a Valley called San Maria , oppofite to one of the Sources of the Thefin . The furthermojl Rhine, Rhenus anterior , arifes upon that Branch of the Crifpalt , which is call¬ ed del Badut , Baduz , and foon receives feve- ral lateral Branches from the Mugels and Come- ra. My prefent Purpofe will not fuffer me to purfue the Courfe of this River in its feveral Branches. Near the Monaftery of Difentis , the farther and middle Rhine join together, and the united Stream falls into the hinder Rhine, near Reichenau . Below Rheineck , the Rhine falls into the Lacus Bodamicus 3 or Boden Sea y and comes out of it near Stein ^ whence walking for fometime the Borders of Swijferland\ it then tra- verfes great Part of Germany in a very irregular Courfe, till at laft, in Holland , it loofes itfelf into the great Ocean. The Reufs , Rufa y arifes from a fmall Lake called ,Lago di LuzendrOj upon the S-. Gothard , but foon receives a confiderable Inforcement from the Furca 9 and ( S8p ) and near ^rfelen , another from a mountainous Lake in Oberalp. Near Fiuelen , not far from Vry 9 it en¬ ters the IV. Waldfietten Sea, Lacus quatuor Civi- tatum Sylveftrium, but refumes its Courfe and Name at Lucern , and at laft falls into the Aar below Win- dijb , Vindonijfa. The Aar^Arola, Arula. , arifes upon the high Moun. tain Grimfula , in the upper Vallefia. About three Hours below that, it falls into the Lake of Brientz , and out of that, not far from the Monaftery Interla- chen , into the Lake of Thun , which it leaves near the Town of Thun , and thence running by Bern , Solo- thurn , andfo down, falls at laft, after many Windings and Turnings into the Rhine near Coblentz, Confluen - tia , probably fo called from the uniting of thefe two confiderable Rivers. But to proceed. Gemmius Mons , the Gemmi , is a very high and fteep Mountain in Vallefia , over which there is a Paf- fage, but only in Summer-time, from the Fruttinger Valley , in the Canton of Bern, to the Mineral Waters at Leiik in Vallefia. The Defcent, on the South-fide of this Mountain, is fteep and frightful, even to the Afped, beyond what can be imagined, being a narrow Path, cut on the Side of almoft perpendicular Precipices, fometimes with trembling woodenBridges,or Planks over the Clefts in the Mountain, and here and there fupported with low Walls. Having been geometrically meafu- red, it was found of ioiio Feet in Length, or rather Height, its many Windings and Turnings included. At a fmall Cottage, called Zur TDauben, a poor refting Place for weary Travellers, being the higheft Part of the Mountain which is paflable, the Mercury fub- fided July i, 1709* to 21" 3"' which gives the Height o ( 59 o of that Place, according to Mariotte And Dr. Scheuchzer 974 ° 5 ' or 5-849' 1002 o or6012 Not far from this Cottage, is a fmall mountainous Lake, called the ‘Dauben Sea , or the Fidgeons Lake , encompaffed on all Sides with high Mountains, the Tops whereof, for their Steepnefs, it would be impof- fible to reach. At Kandelftag , the firft Village in the Frutinger Valley , in the Territory of Bern , going up to the Gemmi^ the Mercury rofe on the fame Day to 24" 2'", which give according to Mariotte - - 5*20° 1' or 3121' Dr. Scheuchzer - - 534 1 or 3205' And at Mullenen , at the Foot of the Gemmi , it flood at 25" 7" / , which anfwer according to Mariotte to - - 318° 5' or 1913* D r.Sheuchzer - - ' 327 o or 1962 On the other Side of the Gemmi. t at Leuck , a celebra¬ ted Place for its Mineral Waters,the Mercury was obferv- ed July 2, and July 1709, at 23" 9'", which anfwers according to Mariotte , to ^81° 4', or 3490', and ac¬ cording to Dr. Sheuchzer, to 5*97° 3', or 35%$'. So that the Cottage ! Dauben , rifes above Leuck, ac¬ cording to Mariotte , - - - 2.3 5^9 7 Dr. Scheuchzer - 2427 Above Mullenen , in the Frutinger Valley , accord¬ ing to Mariotte Dr. Scheuchzer 3936' 4050 And ( 5 JM ) And the perpendicular Height of the Gemtni , above the Level of the Sea, confiderably exceeds 6000 Taris Feet. But high above all the Mountains of Swijferland rifes the Stella , *Piz Stall , a fteep Mountain in the Schamfer Valley, in Rhcetia,or the Grifoons ? the Height whereof was by my Uncle Dr. John Scheuchzer , by Lome Obfervations made in the Year 1709, determin¬ ed to 9585* Raris Foot, above the Level of the Sea, according to his own Calculation, or 9441 according to Mariotte, and 11196 according to Cajjini : A Height, which the Ruficafra, or Shamoys themfelves fcarce venture toafcend. And his to theie only, and the like Heights the following Verfes of Stilus It aliens ought to be applied. Cundta gelu , canaque aternum grandine tetta, Atque aviglaciem cohibent: riget ardua mentis Ait herei facies, furgentique obvia Rhoebo ' T>uratas nefeit jlammis mollire Rruinas. Nullum ver ufquam , nullique aflat is honor es , Sola jugis habitat diris,fedefque tuetur R erf etnas deformis hyems - Having thus determined the Heights of the Moun¬ tains of Swijferland from Barometrical Obfervations, I will now clofe thefe Remarks, which are infenfibly grown to a much greater Length, than I at firft intended they Should, with a few general Obfervations on the na¬ tural Hiftory of that Country, arifing from the Height of its Mountains. The firft Observation (hall regard the Lakes, of which there are feveral, and very remarkable ones, in and ( 55 >* ) and upon the Borders of Swifferland* , which will af¬ ford roe a Angular Inftance of Divine Providence. The Afcent of the Mountains of Swijferland being fo very fudden and quick, that as I have above ftiewn, the Ele¬ vation of the Mountains in the Canton of Glarus a- bove the Horizon of Zuric , though not quite three Days diftant, is more than three Tiroes as great, as the Elevation of Zuric itfelf above the Level of the Ocean, of which it is upwards of 375 Englijh Miles diftant in a ftreight Line ^ and fo in Proportion of others; and the Rivers, which arife in thefe Mountains, rulhing down, in Confequence of fo quick a Defcent, with great Force and Impetuofity, it was to be feared, they would often overflow their Banks, and caufe frequent Inunda¬ tions in the flat Countries, (of which there are too many Inftances in our own Vallies and Plains,) if this Force and Impetuofity was not in great Meafure broke, and their Waters difpofed to a more gentle Defcent. And this is efteftually done by thofe great Receptacles of Water, the Lakes, which are befides of infinite Ufe to the Inhabitants around them, fupplying them with Plenty of Fifh for their Suftenance, and enriching them by the Facility with which Commerce may be carried on over them. Thus the Rhine falls into the Lacus Bodamkus , Boden-Sea , the Rhofne into the Lacus Lemannus, or Lake of Geneva , the Muefa and The - Jin into the Lake of Locarno, the Reus into the Lake of Lucern, the Adda and Maira into the Lake of Co- mo, the Lint, or Limat , into the Lake of Zuric , the Aar, into the Lakes of Brientz, and Thun. And it feems, that the more confiderable the Rivers are, and the more impetuous their Courfe, fo much the greater muft the Receptacles be, wherein they are to loofe their Force < 59? ) ‘Force and Rapidity. The Lake of Geneva, and the ' Boden-Sea, the two largeft in Svuijferland , evidently evince what I hete aflert, and the others above-named gradually decreafe in Largenefs, in proportion as the Rivers, which fall into them, are lefs and lefs rapid. The extream Smallnefs of the Alpine Plants is ano¬ ther Obfervatidn, 1 intend to make. They become lefs and lefs, in proportion as the Mountains, upon which they grow, rife higher. Whether this be outing to the Sharpnefs and Purity of the Alpine Air, or the decreaf- ing Preffure of the Atmofphere, which is far lefs upon Mountains than in Valleys and lower Countries, or to a Want of a fufficient Quantity of fubterraneous Heat, to pulh the Nourilhment into the Roots and Velfcls of the Plants, or rather to a joint Concurrence of thefe a:nd other Caufes, would require a more leifurely Con- fideration. The Thing itfelf is an indifputable Matter of Fad, and it extends alfo to Trees and Shrubs, which become fmaller, as they grow higher. Nay, what is Rill more remarkable, no Trees will grow beyond a certain Height, which is the Reafon why the Tops of Mountains appear fo bare and naked, if viewed at a Diftance, though a curious Traveller fhall not fail meeting upon their rich Paftures with an agreeable Vari¬ ety of beautiful Plants. The Height, where the Trees ccafe to grow, hath been, found, by Barometrical Obfer- vations, nearly to be the fame in divers Parts of Swijfer- land. Otherwife, the Smallnefs of the Alpine Plants is a- bundantly compenfated by the Richnefs of their Virtues, which are, as it were, purpofely centred there into fo narrow a Compafs. But to another ObferVation. The Mountains are l rv *'x • i - much more abrupt, and fteep, and the Precipices greater Kkkk to ( 594 ) to the South, than to the North, and Weftwards than Eaftwards. Many Inftances of this might be given in particular Mountains in Swijferland, as the Gemmi , the Mons fraElus and fo forth j but it is alfo evident¬ ly true with Regard to the whole. Thofe are the higheft Mountain?, which feparate Vallejia , tile Can* ton of Dri, and the feveral Leagues of the Grifons, from Savoy , Piemont , and the Tirol, which lie to the South, or South-Eaft. Thofe very Countries are, . as it were, one continued Set of high Mountains, quite to the Mediterranean Sea, and the like Strufture feems to be continued farther on into that Sea itfelf. The EPyrenean Mountains alfo are but a Continuation of that vaft Chain, which begins in the Lepontia Alpes, or the Mountains in the upper Vallejia, the Canton of ‘Dry and Rhoetia, and from thence fpreads itfelf chiefly Weft and South. On the contrary to the Eaft and North they break off by Degrees into gentle Plains, which appears evidently by the vaft Trafts of Ground, which the Rhine for Inftance, and the ^Danube com- pafs, before they lofe themfelves, the one into the Ger¬ man Ocean, the other into the black Sea, whereas the Rhofne , on the other Side, quickly and with a pro* portionable Velocity reaches the Mediterranean. The fame Obfervation, with Regard to the abrupt Steepnefs of Mountains to the South and Weft, holds true in other Parts of Europe , remarkably in EnglandNorway , more or lefs in other Countries. And fo far as our Maps, and the Accounts of Travellers go, the fame Thing is obfervable in other Parts of the World, but moft evidently in the high Mountains of Peru and Chi¬ li in South America , which, terminate very abruptly Weft wards into the Pacifick Sea, buf gradually decline to ( 595 ) to the Eaft into immenfe Plains, watered by fome of the moft confiderable Rivers in the known World, oar. ticularly the River of Amazons and the Rio della Rlata, which arife in the faid Mountains. To conclude, from what hath been hitherto faid, it appears evidently, that the Mountains of Swijfer- land are the higheft of Europe, and the great. Store- houfe, whence all the Countries around them are fup- plied with Water j conform to what the learned Lo- ritus Glareanus hath long fince elegantly expreffed in the following Verfes. jP raterea caput Europes hanc ejfe probabufit: Aiternis Alpes niv'tbus, juga Olympica, quorum 5 Porgitur in cxlum caput, & fub Tartar a venter : Et quod ad Auroram, Boream,Solemque cadentem Flumina perpetuo non deficientia curfu ‘Parturit, ilia volant & in omnia membra re dun* ( dant, Ad Xephyrum & Libyen Rhodanus, Rhenana fu - ( rent-em ‘Vnda citat Boream, gelidus rotat Ifier ad Eurum \Dirus aquas , Getico novus Hofpes €£ advena ( Tonto. Aflalios fileo, fileo quos Italia accipit amneis Alpibus a nofir is, quaque alto a vertice montes Agmina difparibus fundunt latijfima Sulcis. Whether the Depths of the Sea correfpond with the Heights of Mountains, muft be left to future Obfer- vations. K k k k 2 II. Opti - ('■ 59 & )> II. Optical Experiments made in the Beginning of Auguft 1728, before the Brefidenl and federal Members of the Bpyal Society, and other Gentle¬ men of federal Nationsupon Occaflon of Signior Rizzecti’-f Opticks, with an Account of the faid Book,, By J. T. Delaguliers, L L. D.. and F. (!{. S. S Oine Time in the Year 1722, Signior Gizlanzoni; an Italian Gentleman, fhew’d me a Paper of Signi¬ or John Riszzetti, wherein he denied the different Refrangibiiity of the Rays of Light, becaufe an Ex¬ periment mentioned in Sir Ifaac Newton’s Opticks (B.i. Trop. 1. Exp. 2.) concerning an oblong Paper paint¬ ed half blue and half red (whofe Image projefted by a Lens upon a white Paper at a confiderable Di- ftance became diftinct in its blue half, nearer the Lens than in its red half) had not fucceeded with him, tho’ after many Trials. Sir Ifaac Newton being acquaint¬ ed with this, defired me to repeat his Experiment above- mentioned, which I did at my own Houfe, before him and Signior Gizlanzoni and fome other Perfons, who were fatisfied with the Succefs of it, according to Sir Ifaac Newton's Affertion. Afterwards on the 13th of ‘December 1722, I again repeated the Experiment before the Royal Society, with the fame Succefs, the full Account of which is printed in the Fhilofophical Tran fall ions. Number 3741 After this, Signior Gizlanzoni read me a Letter from Signior Rizzetti, wherein he faid “ He wanted to know whether the K Experiment would fucceed, if the’Paper was turned “ fo as to bring the red Half in the Place of the blue “ one j and that if it fucceeded then, yet he would ct not acquiefce, but he (hould have fomething (fill to c objed agaiiift it. Arid further, that he wanted to H know what could be faid to feveral other Objections “ (1 think there were twelve in the Paper (hewed me) “ againft many more of Sir Ifaac Newton's Optical Experiments, the greatefl Part of which he faid* c * he had found to fucceed differently from what u Sir Ifaac had related * 5 and would not allow the cC Confequences to be juft, which were drawn from c; the other Experiments which he had found to agree a with his TrialsUpon this I acquainted Signior “ Gizlanzoni in a Letter, which Idefired him to com- u municate to Signior Rizzetti ; “ that as" Signior 07 ) I fhould go on with my Account of this Book, if it could be of any Ufe either to vindicate Sir Ifaac Newton, or to convince the Author and his Adherenrs, if he has any. But Sir Ifaac *s Opticks need neither Defence nor Explanation. And when the Author is in the Humour to be convinced, ten Months well em¬ ployed in reading Sir Ifaac *s Book, will make him amends for his ten Tears prejudiced Examination. I beg Leave now to give the particular Defcnption of a few Experiments I made upon this Gccafion, fome of which are exactly as Sir Ifaac Newton made them: Some are his, but made fomething differently, and fome altogether my own. * Experiment!. Big. I. I prepared a Box of about three Foot high, and one Foot wide within (whofe Shape was a truncated Pyra¬ mid) in the following Manner. I painted the Infide of it black, and in the back Part, one Foot above the Bafe, made a fquare Hole of three Inches in Width (whofe Section is rr) to receive a Piece R {hutting clofe with a Rabbet or Shoulder, whofe Surface coming through the Hole was wholly covered with the painted Paper, on which the Experiment was to be made. Over againft r r , in the fore Part of the Box, was a Door to open with a Tube in it, four Inches wide and five Inches long, whofe Sedion is e,fg^ h , that two Candles fet on the Places /, k , to enlighten the Paper at r,r, might throw no dired Light out of the Box, whofe Sedion is reprefented at a Ir e d . Then having made the Room perfedly dark, I fixed the Box upon a Table, that it might remain in one , Place j at the Diftance of ( 6o6 ) eight Foot from rr, I fixed the Lens L L, of four Foot Focus, in a Frame upon another Table, with its Axis going through the Middle of rr: At the Diftance of about eight Foot beyond the Lens, I fet up the Skreen or Square of white PaperS. Having put into the Hole r r a ftiff Paper, painted with Vermillion, and wrapped four Times and an half with black Silk (as represented by R), that Paper enlighten’d by the Candles at /, k, the Image of the red Paper was pro¬ jected upon the Skreen at p, and whenthe molt diftind Place was found, the Skreen was fixed : Then a Paper painted with Ultramarine being fixed in the Hole r r, the Image of it was fo indiftind at p, that the Images of the black Silks could not be feen; but holding a Piece of Paper clofe to the Skreen, and bringing it forward, at about \ of an Inch from the Skreen, the Re- prefentation of the Silks began to appear on the blue Image ; but it was tnoft diftind at an Inch and f, or at Z Z j fo that there was i* Inch between the diftind Bafe of the red, and that of the blue Paper. But what has led feveral People into an Error in making this nice Experiment, is the Depth of the Focus of the Rays in both Cafes; for though the red Image was mod diftind at p, yet the Reprefentation of the black Silks might juft be perceived by a good Eye when the Skreen was moved backwards or forwards | of an Inch: The blue Image which was ftronger had its Silks vifible an Inch on either Side of Z Z; fo that in a Paper half red and half blue, painted with thefe Colours, one might have feen the Silks (though faintly) upon the two Images at once, and have been thereby deceived: But 1 of an Inch beyond the Place common to both, the red alone would have appeared diftind; and an Inch ( 6 08 ) Inch fhort of the faid Place, the blue Image moft di- ftind, and diftind alone ; that is an Inch and | nearer the Glafs. Inftead of Vermilion the red Paper may be painted with Carmine or Lake , but it will not do fo well, as was then tried j nor does TruJJian Blue do fo well ^Ultramarine, The belt Way is to heighten the Vermillion with a little Carmine , and the "Ultra- marine (which has too much white) with Indigo \ and then there will be a Space between the two di¬ ftind Bafes where both the Images will be indiflind. N. B. I made the Experiment with fuch Colours , in the Tear but now I ufid no Mixtures,that any Body elfe might repeat the Experiment . The fecond Figure reprefents the Box with one Side out, whofe Place is S' d b B j eg is the Hole far theTube in the Door of the Forefide, x ^ c d rr the Hole in the Back to receive the Piece R with its painted Paper. The third Figure is the Box open before, with the Candles and Paper in it, the fame Parts being marked with the fame Letters as in the other Figures. N. B. I made the Experiment in this Manner, be- caufe Signior Rizzetti attributed the different Foci of the Colours to different Inclinations, which could not be alledged here the red and blue being, as he had defired, fucceffively fixed in the very fame Place: And he fays (Page 64.) addidi permanentes colores a lumine direElo diverfa inclinatione illujlratos conjiante In- clinatione in lentem incidere. Nay, more than this was performed in the Experiment • for as the Candles were fixed, the Light fell upon the painted Paper always with the fame Incidence. EX PE ( b c, and c d , will be bent into the Curve abc d ; and the emergent Ray d d will make the fame Angle with the Incident Ray R r as if the Refradionhad been made at once at the Point n , which Point may be confidered as in the Surface G G, becaufe MM has been fuppofed extremely near that Surface: Then alfo may Refradi- ons be confidered in grofs, and Rays trac’d, in all Op¬ tical Propofitions, as if there were no fuch Curve as what we have been defcribing. Again, let D ( Fig, 13) reprefent the denfe Me¬ dium or Giafs, and A the rare Medium or Air ; R a a Ray of Light coming out of the denfe Medium in¬ to the Rare, in the Diredion Rr, in which it may be refraded (as for Example, in an Angle of 30 De¬ grees with the Perpendicular P a). Let M M be the Line which limits the Attradion of the Surface G G, which Attradion is exerted in Lines tending perpen¬ dicularly from MM to G G. As foon as the Ray of Light has emerged at a , it is attraded in the Di¬ redion a P, and therefore diverted from the Line a r, into the new Diredion a ; a t b, it is turned into the Line b b ; at r, into the Line c c ; and at ( <*'« ) d, into the Line d d; fo that the emergent Ray will be dd, as if the Refraction had been performed in the Point n, and that Point was in the Surface GG, without any Curve at a b c d ; and all the reft as we confidered it before, with this Difference only, viz. That the Ray is bent juft as it comes out ( or rather when it is come out) of the denle Medium ; where¬ as before we confidered its Bending before it came into it. Of the Bending of Rays in Reflection. But if the Ray R a {Fig. 14) coming out of Glaft into Air, fliould come in fiich a Direction as to be wholly reflected, as it will do when the An¬ gle R a P is of 45 Degrees; I fay the Reflection will not be made at the Surface GG, nor above it in the Glafs; but under the faid Surface, in the Air, or even in a Vacuum, or any Medium lefs denle, or rather left refractive than Glaft. MM reprefents the Limits of the Attraction of the Glaft exerted in a Direction from MM to GG perpendicularly, as we faid before. The Ray R a , moving in the Direction R r, at its Emerfion at a, is, for the Reafons before given, turned into the Direction a a; then at b, into the Direction b b j at e, into the Direction c c ; at d, in¬ to the Direction d d; at f, into the Direction e e ; and at f into the Direction f f parallel to GG ; then at g, the Ray is again turned towards the Glaft, by whofe Attraction changing fucceflively into all the Directions g g, i i, k k, and l \; at laft it re-enters the Glafs in the Direction m m making the ( 6\7 ) the fame Angle with the Perpendicular m p that R a mada with a P. Now as the Lines perpendicular to GG drawn from MM are infinitely near, the Line abcdefgh'tk l m mull: be a Curve ; and as M M and G G are extremely near, the Vertex of the Curve ( whole Tangent is ff parallel to G G ) will be fo near the Point I, as to be con- fidered as co-inciding with it, when we compare the Angle of Incidence with that of Reflection ; then alfo will the Space between the Parallels p m and P a be fo far diminifhed, that thofe two Lines may be looked upon as co-inciding, the Angles m»p and R a P being equal, whether the three Points m, I, a, co-incide or not. For thefe Reafons, for common Ufe, one may confider the Reflexion from the under Surface of the Glafs as made at once in that Surface at the Point I. But when we examine Things ItriCtly, Ex¬ periments as well as the above Reafoning, will lhew, that there is fuch a Curve as we have mentioned. See Experiment VI. Fig. xoandii; and we fhall mention others. N. B. If any Point of the Curve a b c, Sec. be¬ tween a and f, fall below ( or beyond the Line M M, the Ray will then go on in a ftraight Line Tangent to the Curve in that Point where it leaves the Line MM. Now let us fuppole MedcbarM (in the fame Fig. ) to be Glals, or any other denfe Medium, and mp PR Air, or any other rare Medium, and Ra Ray of Light moving in the rare Medium towards the denfe Medium in the Direction R a towards r; if inftead of an Attraction at tjie Surface of the Glals N n n n MM, ( 6il ) MM, there be luppofed a repellent Force, whofe Limits are G G ; then will the Ray by the Repul- fion of the Surface M M be bent into the Curve abed efg hi klm in the fame Manner as we ihewed it would be under the Surface G G, when G p P G was confidered as a denfe Medium. Hence it follows that a Ray moving in the Air, is reflected from a lpecular Surface of Glafs, or any other Mirrour, opake or diaphanous, without touching the faid Surface. N. B. That the fame Tower may , under different Circumftances , attraB to and repel from the fame Surface, Jhall be made out in the remaining Tart of this Taper ; but now taking fuch a Tower for granted, we will proceed in confidering the Flexure of Rays of Light. Let us fuppofe a Prifm A C B (Fig. if) to have the attracting Power of its inferior Surface extend as far as the Line *0 m ; if another Prifm G D F (the attracting Force of whofe upper Surface extends as far as n n) be brought very near to the firft Prifm ; where the at¬ tracting Powers of the Prifms interfere, they will deftroy one another, becaufe they act in contrary Di¬ rections; and thereby the Limits of Attraction of each of the Surfaces will be contracted ; the Power of A B extending no farther than n n, and that of D F no farther than mm, whilft the Space nn mm lofes all the Force that it had ( and would have upon the Removal of either Prifm ) to turn a Ray of Lighr, moving obliquely, out of its Direction. Now in this Situation of the Prifins, a Ray of Light entering the Surface C B at right Angles, will go through the fecond Prifm alfo at Right Angles (not ( 6 \9 ) (not exactly in the fame Line, but) in a Line parallel to the Direction of the incident Ray: For Example, let the Ray R a ( not refracted at, becaufe perpendicular to, the Surface C B) emerge from the firfl Prifm at a, in the Direction a r ; its changed Direction at a will become a a, and at b , b b, or ra¬ ther the Ray will be inflexed in the Curve ab ; and at b getting out of the Power of the Attraction of the Surface AB, it will (for the Reafons before given) move in a ftraightLine from b to c , where it will be bent again the contrary Way in the Curve c d of the lame kind as a b , and laftly emerge in the Direction d d parallel to the firfl: Direction R r. From hence it fol¬ lows, that when the Prifrns are brought fo near as to touch, their mutual Attractions deftroying each other, the Rays of Light will not be bent, but pafs through the two Prifrns ( which in this Cafe perform the Of¬ fice of a Parallelopiped ) in the fame Direction with which they came into the firfl Prifm, and confe- quently produce no Colours ; contrary to what is affirmed by Rizzetti (Tage 78, 79, &c.) and when the Rays R a fall obliquely upon the Surface C B, the EffeCt of their RefraCtion at their Immer- fion at S to produce Colours, is taken off by the RefraCtion which they fuffer at their Emerfion at z. Experiment VII. I took the Cube of Fig. 8, and looking oblique¬ ly through it at the Hole of the Window of my dark Chamber (the Sun filming or not fhining) the Hole appeared entirely colourlefs, as did alio a Candle, JSJ n n n % both { 6io ) both appearing fringed with Colours when fecti through the Priftn. Then holding two Prifms to* gather, as in Fig. io, if the Hole of the dark Cham* ber be at k, it appears white to the Eye at E; but if the Angles of the Prifms at B F be a little fepa- rated, whilft the Points A D touch, the Hole will appear coloured : When the Surfaces are feparated at A D, and touch at B F, the Colours appear in an inverted Order; but if the Surfaces A D and B F are parallel, whether they touch or not, the Hole will ippear white. N. B. In this Cafe the Trifms muft be fimilar y that the Surface F G may be parallel to AC; other- wife A B and D F muft be fo inclined to one another as to render A C and F G parallel. Indeed if one of the Prifms be very far removed from the other y the heterogeneous Light which entered in at F G, may be fo far Jpread by the Separation of the dif¬ ferently refrangible Rays , that the Frifm ABC will not take it all in then the Eye behind the fe- cond Frifm may fee Colours , as I fuppofe Riz* zeti did . See Tage 79 of his Book. If the Ray of Light R a b c d d ( Fig . 15. ) changing its Direction in the Manner above-men¬ tioned, makes an Angle of about 45 Degres with the Perpendicular P a ^ upon the removal of the lower Prifm, the Ray will be turned up again, as in Fig . 14. But if the Angle P^R be greater, the Ray will (till be turned up again in a Curve, as a b c d e f ( Fig. 16) notwithftanding the lower Prifm is at DFG; but if that Prifm be brought up- clofer to the Surface A B, the Curves will be deftroyed where the Prifms touch, and all the Rays in the Place of Contact brought down through the lower Prifm. THE ( 6n ) THE mod refrangible Rays confid of fmaller Par¬ ticles than the lead refrangible Rays, and therefore mud have lead Momentum , the Velocity of all the Rays being the fame ; and confequently are more eafilyturned out of the Way by Attraction or Re- pulfion, which makes the Curves made by the pur¬ ple and violet Rays under the Surface A B, to be left and nearer the faid Surface than the Curves made by red and orange Rays. Suppofe a Violet R a moving in the Direction R r ( Fig. 1 6 .) to be fo bent under the Surface A B, that at the Vertex of the Curve, or where its Tangent c c is parallel to A B, there dill remains afinall Space be¬ tween the Curve and the Line n //, where the Limits of Attraction ( contracted by the Proximity of the undermod Prifm D F G end) that Ray will be turn¬ ed up again in the Curve d e /, and fo reflected in the Line/f, the Directions having been fucceflively changed, as in Fig . 14. But a red Ray with the fame Inclination, would pals on into the lower Prifm, as was explained in Fig. iy. Becaufe the Momentum of the red Ray being greater than that of the Violet, the fame Degree of Attraction could not give it the fame Flexure. This is confirmed by Experiment, for when the lower Prifm is not prefled hard againd the upper (as in Fig . 11.) the Rays brought down to R make a Spot of a Colour made up chiefly of red and orange Rays ; but when the Prifms are prefled clofer, the Spot grows bigger and perfectly white in its Middle, becaufe all Sorts of Rays are brought down to the Spot; but it is inclofed round with a reddiili Border, occafioned by the Parts of the Prilrn which are very. near, ( 61% ) near, but not in Contact, or at lead: not near enough to bring down the green, blue, purple and violet Rays. This lhews that the Refledion is not made from the interior folid Parts of the Glafs, nor from the Parts in the Surface, as Rizzetti affirms. But this is made more evident by Experiment VIII. Fig. 17. A Candle being in the Pofition K, the Eye at E, and the Prifm at A B C; a ftrong Image of the Can¬ dle was feen at k as in Fig.j. But lifting up a Veflel of Water VS S V till the Surface of the Water V V touched A B the lower Surface of the Prilm, the I- mage of the Candle became almoft infenfible, as the Eye loft all thofe Rays which now were attraded in¬ to the Water. And for a farther Proof, that the Re¬ fledion is made under the Surface and not in it, when the Prifm was taken out of the Water, being wet at its lower Surface, or having a Stratum of Water (whofe Surface was VV Fig. 18) under A B, the Image of the Candle did again become vivid, the Rays being turned up again under V V. Indeed the Image, in this Cafe, though ftrong, did not ap¬ pear well defined, by Reafon of the Unevennefs of the watry Surface VV Fig. 18. I am very well aware that Rizzetti may anfwer here, that what I have faid above, does in fome Mea- fure favour his Notions; and that the Rays which (in Fig. 7, having pafted through AB, the lower Surface of the Prifm) are turned up again to the Eye at E, do not fuffer a Refledion but a new Immerfion ; for he fays, in Page ixy. — ‘‘ Anglus (meaning Sir Ifaac ( 6i% ) a Ifaac Newton ) fecundo fubjungit, quod fi lumen “ in tranftu e vitro in aerem obliquius incidat r cc quam in angulo graduum 40, illud. in totum re - c< flettitur . Ego vero refpondeo, quod ex iis, quae c{ docui in Prop. 4. Cap, 1. elicitur hanc non efie “ veram luminis reflecftionem, led potius novam Im- “ merfionem ; & ideo nego quod ex ifto Phamome- no fequatur lumen a partibus corporum folidis, “ aliquo interjecfto intervallo, refle6l:i/ > And a little lower, having quoted what Sir Ifaac Newton lays* concerning the blue Light, which, coming from one Prifm obliquely upon the farther Surface of another, is wholly reflected, at the lame Inclination that the red Light is wholly tranfmitted. — He fays, “ Satis “ fit iterum refpondere, quod in hoc etiam cafu eft “ nova luminis immerfio, quae dicitur ab au. (f. S. Seer . T H E making of Tin-plates, or Lattin, as it is called, being not commonly praCtifed in Eng¬ land, though there is fo great a Confumption of it, either becaufe the Method is not fufficiently known, or becaufe that in Ufe to make fmall Quantities for particular Purpofes is much too dear to aufwcr the Artificer’s Expectation in making larger, whereby vve are obliged to export our own Tin to Germany , to receive it back again manufactured, I thought it not improper to lay before the Society the Method the Germans themfelves make uie of as I have ex¬ tracted it from a Differtation of Mr. He Reaumur, prin¬ ted in the laft Volume of the Memoirs of the Aca¬ demy of Sciences of Rar'ts, in which alfo he lays down fome Improvements, as he thinks, of his own. He takes notice then that the making of Tin-plates, (which is called in France, white Iron) does not pro¬ perly begin, fill they go about to prepare the Leaves or Plates of Iron that are to be tinned, which are fup- pofed to be fufficiently thin and flat, and cut into Squares : But there are only certain Sorts of Iron which can be reduced into thefe Leaves, of which thofe arc the molt proper, that when heated are eafi- eft extendible, and yet can be forged with a Hammer when cold ; the more foft and extremely flexible, as well ( ) well as the more brittle being to be rejected. Thefe Leaves are drawn from Bars of Iron, about an Inch fquare; which being made a little flat, they cut into thin Pieces or Soles ( femelles) which they fold toge¬ ther, and having made them intp Parcels containing forty Leaves each, beat them all at once with a Ham¬ mer that weighs from 600 to 700 ft* Weight. After this, the principal Part of the whole Art is to prepare thefe Leaves ; for the lighted Duft, or the leaft Rud upon their Surface will prevent the Tin from uniting with them. This may indeed be taken ofF by filing, but that being much too expenfive, the fame may be brought about by deeping the Plates in acid Waters, for a certain Time, to what Number they pleafe, and when they are taken out, fcouring them with Sand, in order to fetch off any Thing that may remain upon the Surface: And by this Method a Woman may clean more Plates in an Hour, than the mod expeditious Workman can file in many Days. Of thefe Waters the Author mentions feveral ; but what the Germans themfelves ufed, and which they make a mighty Se¬ cret of, he found to be only common Water made ea¬ ger with Rye, which requires very little Pains. For after they have ground the Grain grofly, and pounded it,they leave it to ferment in common Water for a certain Time, and with a little Patience they are fure to have an eager Mendruum. With this Mendruum they fill Troughs or Tuns, into which they put Piles of Iron Plates ; and to make it grow eager the better, and to have more A&ivity, they keep thefe Vedels in Vaults or Stoves which have little Air, and in which they keep lighted Charcoal. The Workmen go into thefe Vaults once or twice in a. Day, either to turn the Plates ( * 3 * ) Plates that they may be equally expofed to the Addon of the acid Liquor, or to take out thofe that are fuffi- ciently cleanfed, or to put others in their room: And as the Liquor is more acid, or the Heat of the Vault or Stove is more intenfe, the Plates are fooner cleanfed } but it requires at leaft two Days, and fometimes a great deal more. This is the Method which the Germans employed in the Tin*works in France, conftantly made ufe of to prepare the Iron-plates to receive the Coat of Tin: But as the Author obferved, that the conftant Attendance upon them in the Stoves was very labori¬ ous, the Heat therein being almoft infupportable to thofe who are not ufed to it, he propofes fome other Methods which are attended with very little Trouble, and as fmall, if not a lefs Expence j and which upon Trial fucceeded full as well. Having therefore ob¬ ferved that the Iron-leaves or Plates are covered with a Scale or Layer, half vitrified by the Fire, on which Acids have none or very little Effeft, he imagined that inftead of diffolving the Iron in thefe acid Waters, it would be better to make it ruft , and thereby put it in a Condition to be eafier cleanfed from thefe Scales^ as Ruft is accompanied with a fort of Fermentation and Rarefaftion, and the Matter which rufts takes up a great¬ er Space, and raifes up whatever oppofes it. To this Purpofe he fteeped Iron Plates in different eager Men- fttuums, as in Water in which Alum, common Salt and Sal-armoniack were feparately diffolved ; and others of the fame Iron he only dipped' into the fame Waters, and inftantly taking them out expofed them to the Air. Thefe latter were rufted by all of them, but fooner by that in which the Sal-armoniack was diffolved. Af¬ ter two Days, during which every Plate had been dip¬ ped ( ) ped into the Menftruum but twice or thrice, he fcour- ed them, and likewife thofe he had left to fteep for that Time; and comparing them together, found that thofe, which had been only wetted at different Times, cleanfed better than thofe which were fteeped j the Ruft covering all the Surface of the latter without raif- ing the Scale; whereas in the former, as foon as one Part of the Metal is detached, it is attracted by the Menftruum, and the Surface is raifed into Blifters of Ruft. Thefe Diifolvents,the Author takes notice, tho’ weak in themfelves, yet produce the Effeft as well as the ftronger, which are much dearer: But amongft the latter he prefers Vinegar, which being very plen¬ tiful in France , may be ufed with little Coft. For you need only dip each Leaf into it, and take it out again immediately, leaving it afterwards in fome moift Place, and it will be fcaled in eight and forty Hours, if you take care to repeat this 3 or 4 Times in a Day. The fcaling will ftill be more expeditious, if you dif- folve a little Sal-armoniack in the Vinegar, a Pound or two to a Puncheon j for as the Vinegar dilfolves I- ron well, fo Sal-armoniack, as juft obferved, rufts it fooner than any other Salt: But this muft be ufed very moderately, and the Leaf muft be left to fteep in clean Water to diifolve any Particles of it that may flick to its Surface, which may otherwife make it ruft after it is tinned. If you fcale with Vinegar, and want to do it at a lefs Expence, you need only plunge the Leaves once or twice at fartheft, and when the Vinegar is dri¬ ed upon the Surface, fprinkle it with Water; or dip them into it, and take them out immediately. There are feveral other Ways of making Iron ruft, as keeping it in a moift Cellar, expofing it to the Dew, fprinkling P p p p it ( r.Edmond Halley Aftronom. Reg. &c. giving an Account of a new dif- coVered Motion of the Fix’d Stars. SIR , Y O U having been pleafed to exprefs your Satis¬ faction with what I had an Opportunity fome- time ago, of telling you in Conversation, concerning fome Obfervations, that were making by our late wor¬ thy and ingenious Friend, the honourable Samuel Molyneux Efquire, and which have fince been conti¬ nued and repeated by my felf, in order to determine the ‘Parallax of the fixt Stars ; I (hall now beg leave to lay before you a more particular Account of them. Before I proceed to give you the Hiftory of the Ob¬ fervations themfelves, it may be proper to let you know, that they were atfirft begun in hopes of verifying and confirming thofe, that Dr. Hook formerly communicat¬ ed to the publick, which feemed to be attended with Circumftances that promifed greater ExaCtnefs in them, than could be expected in any other, that had been made andpublilhed on the fame Account. And as his Attempt was what principally gave Rife to this, fo his Method in making the Obfervations was in fome ( <38 ) Meafure that which Mr. Molyneux followed : For he made Choice of the fame Star ? and his Inftrument was conftru&ed upon almoft the fame Principles. But if it had not greatly exceeded the Doctor’s in Ex- achiefs, we might yet have remained in great Uncer¬ tainty as to the Tarallax of the fixt Stars ^ as you will perceive upon the Comparifon of the two Experiments* This indeed was chiefly owing to our curious Mem¬ ber, Mr. George Graham , to whom the Lovers of Aftronomy are alfo not a little indebted for feveral o~ ther exaft and well-contrived Inftruments. The Ne- ceflity of fuch will fearce be difputed by thofe that have had any Experience in making Aftronomical Ob- fervations^ and the Inconfiftency, which is to be met with among different Authors in their Attempts to de¬ termine fmall Angles, particularly the annual Paral¬ lax of the fixt Stars , may be a fufficient Proof of it to others. Their Difagreement indeed in this Article, is not now fo much to be wondered at, fince I doubt not, but it will appear very probable, that the In¬ ftruments commonly made ufe of by them, were liable to greater Errors than many times that Pa¬ rallax will amount to. The Succefs then of this Experiment evidently depending very much on the Accuratenefs of the In¬ ftrument that was principally to be taken Care of: In what Manner this was done, is not my prefent Purpofe to tell you ; but if from the Refult of the Obfervations which I now fend you, it fhall be judged neceftary to communicate to the Curious the Manner of making them, I may hereafter perhaps give them a particular Defcription, not only of Mr. Molyneux'$ Inftrument, but alfo of my own, which ( 6w ) which hath fince been eredted for the fame Purpofe and upon the like Principles, though it is fomewhat different in its ConftrudHon, for a Reafon you will meet with prefently. Mr. Mclyneux's Apparatus was compleated and fitted for obferving about the End of November 17x5, and on the third Day of December following, the bright Star in the Head of Draco (marked y by Bayer) was for the firft Time obferved, as it parted near the Zenith, and its Situation carefully taken with the Inftrument. The like Obfervations were made on the fth, nth, and nth Days of the fame Month, and there appearing no material Difference in the Place of the Star, a farther Repetition of them at this Seafon feemed needlefs, it being a Part of the Year, wherein no fenfible Alteration of Parallax in this Star could foon be expected. It was chiefly therefore Curiofity that tempted me (being then at KeWy where the Inftrument was fixed) to prepare for obferving the Star on ‘December 17th, when having adjufted the Inftrument as ufual, I perceived that it parted a little more Southerly this Day than when it was obferved before. Not fufpecfting any other Caufe of this Appearance, we firft concluded, that it was owing to the Uncertainty of the Obfer¬ vations, and that either this or the foregoing were not fo exacft as we had before fuppofed ; for which Reafon we purported to repeat the Obfervation again 3 in order to determine from whence this Difference proceeded 5 and upon doing it on December %oih T I found that the Star parted (till more Southerly than in the former Obfervations. This /enftble Alteration the more furprized us ? in lt was f he contrary way ( < 4 ° ) way from what it would have been, had it pro¬ ceeded from an annual Yarallax of the Star : But being now pretty well fatisfied, that it could not be entirely owing to the want of Exaitnefs in the Ob- fervations ; and having no Notion of any thing elft, that could caufe fuch an apparent Motion as this in the Star} we began to think that fome Change in the Materials, &c. of the Inftrument itfelf, might have occafioned it. Under theft Apprehenfions we remained fome time, but being at length fully con¬ vinced, by ftveral Trials, of the great ExaCtnefs of the Inftrument, and finding by the gradual Increafe of the Stars Diftance from the Pole, that there mud be fome regular Caufe that produced it ; we took care to examine nicely, at the Time cf each Obfer- vation, how much it was: and about the Beginning of March 1726, the Star was found to be 20" more Southerly than at the Time of the firft Obftrvation. It now indeed ftemed to have arrived at its utmoft Limit Southward, becaufe in feveral Trials made a- bout this Time, no fenfible Difference was obferved in its Situation. By the Middle of April it appear¬ ed to be returning back again towards the North ; and about the Beginning of June , it paffed at the fame Diftance from the Zenith as it had done in ‘Decern - her , when it was firft obferved. From the quick Alteration of this Star’s Declina- nation about this Time (it increafing a Second in three Days ) it was concluded, that it would now proceed Northward, as it before had gone Southward of its prefent Situation } and it happened as was con¬ jectured : for the Star continued to move Northward till September following, when it again became fta- tionary 5 ( <>4 l ) tionary, being then near 2.0" more Northerly than in June , and no lefs than 39" more Northerly than it was in March . From September the Star returned towards the South, till it arrived in 'December to the fame Situation it was in at that time twelve Months, allowing for the Difference of Declination on account of the Preceflion of the Equinox. This was a fufficient Proof, that the Inflrument had not been the Caufe of this apparent Motion of the Star, and to find one adequate to fuch an Effect teemed a Difficulty, A Nutation of the Earth’s Axis was one of the firfl; things that offered itfelf upon this Occafion, but it was toon found to be infufficient ; for though it might have accounted for the change of Declination in y Draconis yet it would not at the fame time agree with the Phenomena in other Stars ; particularly in a fmall onealmoft oppofite in right Afcenfion to y Draconis , at about the fame Diftance from the North Pole of the Equator: For, though this Star feemed to move the fame way, as a Nutation of the Earth’s Axis would have made it, yet it changing its Declination but about half as much as y Draconis in the fame time ( as appeared upon comparing the Obfervations of both made upon the fame Days, at different Seafons of the Year) thi$ plainly proved, that the apparent Motion of the Stars was not occafioned by a real Nutation, fince if that had been the Caufe, the Alteration in both Stars would have been near equal. The great Regularity of the Obfervations left no room to doubt, but that there was fome regu/ar Caufe that produced this unexpected Motion , which did not depend on the Uncertainty or Variety of the CLqqq Seafons ( «4* ) Seafons of the Year. Upon comparing the Obfer- vations with each other, it was difcovered, that in both the fore-mentioned Stars, the apparent Dif¬ ference of Declination from the Maxima ,, was al¬ ways nearly proportional to the verfed Sine of the Sun’s Diftance from the Equinoctial Points. This was an Inducement to think, that the Caufe, what¬ ever it was, had fome Relation to the Sun’s Situa¬ tion with relpedt to thofe Points. But not being able to frame any Hypothefis at that Time, fuffi- cient to fclve all the Phenomena, and being very defirous to fearch a little farther into this Matter; I began to think of erecting an Inftrument for my felf at IVanjled , that having it always at Hand, I might with the more Eafe and Certainty, enquire into the Laws of this new Motion. The Confide- ration likewife of being able by another Inftrument, to confirm the Truth of the Obfervations hitherto made with Mr. Molyneux’s , was no fmall Induce¬ ment to me; but the Chief of all was, the Oppor¬ tunity I fliould thereby have of trying, in what Manner other Stars were affecfted by the lame Caufe, whatever it was. For Mr. Molyneux's Inftrument being originally defigned for obferving y c Draconis (in order, as I faid before, to try whether it had any fenfible Parallax ) was fo contrived, as to be capable of but little Alteration in its Direction, not above feven or eight Minutes of a Degree : and there being few Stars within half that Diftance from the Zenith of Kew , bright enough to be well obferved, he could not, with his Inftrument, throughly examine how this Caufe affe&ed Stars differently fituated with refpedt ( «4? > refpetft to the equino&ial and folftitial Points of the EcJiptick. Thefe Confiderations determined me ; and by the Contrivance and Direction of the fame ingenious Perion, Mr. Graham , my Inftrument was fixed up Auguft 19, 172,7. As I had no convenient Place where I could make ufe of fo long a Telefcope as Mr. Molyneux's , I contented my felf with one of but little more than half the Length of his ( viz. of about 12- Feet, his being 241) judging from the Experience which I had already had, that this Ra¬ dius would be long enough to adjuft the Inftrument to a fufficient Degree of Exadtnefs, and I have had no Reafbn fince to change my Opinion: for from all the Trials I have yet made, l am very well fatisfied, that when it is carefully re the vifible or apparent Place of the Objed will be altered 7', if the Diredion of the Eye’s Mo¬ tion is at one time contrary to what it is at ano¬ ther. If the Earth revolve round the Sun annually, and the Velocity of Light were to the Velocity of the Earth’s Motion in its Orbit (which I will at prelent fuppofe to be a Circle) as 1000 to one; then tis eafy * to ( ^49 ) to conceive, that a Star really placed in the very Pole of the Ecliptick, would, to an Eye carried along with the Earth, feem to change its Place continually, and (negle&ing the finall Difference on the Account of the Earth’s diurnal Revolution on its Axis) would feem to defcribe a Circle round that Pole, every Way dirtant therefrom 3'f. So that its Longitude would be varied through all the Points of the Ecliptick every Year; but its Latitude would always remain the fame. Its right Afcenfion would alfo change, and its Decli¬ nation, according to the different Situation of th& Sun in relpedi to the equinoctial Points ; and its ap¬ parent Diflance from the North Pole of the Equator would be 7 / lefs at the Autumnal, than at the vernal Equinox. The greateft Alteration of the Place of a Star in the Pole of the Ecliptick (or which in Effect amounts to the fame, the Proportion between the Velocity of Light and the Earth’s Motion in itsOrbit) being known; it will not be difficult to find what would be the Dif¬ ference upon this Account, between the true and ap¬ parent Place of any other Star at any time ; and on the’contrary, the Difference between the true and appa¬ rent Place being given ; the Proportion between the Velocity of Light and the Earth’s Motion in its Or¬ bit may be found. As I only obferved the apparent Difference of De¬ clination of the Stars, I fhall not now take any far¬ ther Notice in what manner fuch a Caufe as I have here fuppofed would occafion an Alteration in their apparent Places in other RefpecSts ; hut, fuppofing the Earth to move equally in a Circle, it may be gather¬ ed from what hath been already faid, that a Star which R r r r is ( 6 5 ° ) is neither in the Pole nor Plain of the Ecliptick, will feemto defcribe about its true Place a Figure, infenfi- bly different from an Ellipfe, whofe Tranfverfe Axis is at Right-angle to the Circle of Longitude palling through the Stars true Place, and equal to the Diame¬ ter of the little Circle defcribed by a Star (as was before fuppofed) in the Pole of the Ecliptick ; and whofe Conjugate Axis is to its Tranfverfe Axis, as the Sine of the Stars Latitude to the Radius. And al¬ lowing that a Star by its apparent Motion does ex- ajftly defcribe fuch an Ellipfe, it will be found, that if A be the Angle of Pofition (or the Angle at the Star made by two great Circles drawn from it, thro’" the Poles of the Ecliptick and Equator) and B be another Angle, whofe Tangent is to the Tangent of A as Radius to the Sine of the Latitude of the Star; then B will be equal to the Difference of Longitude between the Sun and the Star, when the true and ap¬ parent Declination of the Star are the fame. And if the Sun’s Longitude in the Ecliptick be reckoned from that Point, wherein it is when this happens; then the Difference between the true and apparent Declination of the Star (on Account of the Caufe I am now conftdering) will be always, as the Sine of the Son’s Longitude from thence. It will likewife be found, that the greatefl Difference of Declination that can be between the true and apparent Place of the Star, will be to the Semi-Tranfverfe Axis of the Ellipfe (or to the Semi-diameter of the little Circle de¬ fended by a Star in the Pole of the Ecliptick) as the Sine of A to the Sine of B. If the Star hath North Latitude, the Time, when its true and apparent Declination are the fame, is be¬ fore: {* 5 * ) fore the Sun comes in Conjun&ion with or Oppofition to it, if its Longitude be in the .firft or laft Quadrant (viz. in the afcending Semi-circle) of the Ecliptick ; and after them, if in the defending Semi-circle ; and it wilt appear neareft to the North Pole of the Equator, at the Time of that Maximum (or when the greateft Differ¬ ence between the true and apparent Declination happens) which precedes the Sun’s Conjun&ion with the Star. Thefe Particulars being fufficient for my prefent Purpofe, I fhall not detain you with the Recital of any more, or with any farther Explication of thefe. It may be time enough to enlarge more upon this Head, when I give a Defcription of the Inftruments &c. if that be judged neceflary to be done; and when I (hall find, what I now advance, to be allowed of (as I flat¬ ter my felf it will) as fomething more than a bare Hy¬ pothecs. I have purpofely omitted fome matters of no great Moment, and confidered the Earth as moving in a Circle, and not an Ellipfe, to avoid too perplexed a Calculus , which after all the Trouble of it would not fenfibly differ from that which I make ufe of, efpecial- ly in thofe Confequences which I (hall at prefent draw from the foregoing Hypothefis. This being premifed, I fhall now proceed to deter¬ mine from the Obfervations, what the real Proportion is between the Velocity of Light and the Velocity of the Earth’s annual Motion in its Orbit; upon Suppofition that the ‘Phenomena before mentioned do depend upon the Caufes I have here afligned. But I i«uft firft let you know, that in all the Obfervations hereafter men¬ tioned, I have made an Allowance for the Change of the Star’s Declination on Account of the Preceflion of R r r r 2 the (6 5 \> the Equinox, upon Suppofition that the Alteration from this Caufe is proportional to the Time, and regu* lar through all the Parts of the Year. I have deduced the real annual Alteration of Declination of each Star from the Obfervations themfelves ; and I the rather choofe to depend upon them, in this Article, becaufe alt. which I have yet made, concur to prove, that the Stars near the Equino&ial Colure, change their Declination at this time i" I or 2" in a Year more than they would do if the Preceflion was only 50", as is now generally fup- pofed. I have likewife met with fome fmall Varieties in the Declination of other Stars in different Years, which do not feem to proceed from the fame Caufe, par* ticularly in thofe that are near the folftitial Colure, which on the contrary have altered their Declination iefs than they ought, if the Preceflion was $o n \ But whether thefe fmall Alterations proceed froth a regular Caufe, or are occaftoned by any Change in the Mate* rials &c. of my Inftrument, I am not yet able fully to determine. However, I thought it might not be a- mifs juft to mention to you how I have endeavoured ta allow for them, though die Refult would have been nearly the fame, if I had not confidered them at all. What that is, I will fhew, firft from the Obfervations of y Draconic , which was found to be 39" more South* erly in the Beginning of March , than in September. From what hath been premifed, it will appear that the greateft Alteration of the apparent Declination of y'Draconic, on Account of the fucceffive Propagation of Light, would be to the Diameter of the little Circle which a Star (as was before remarked) would feem to defcribe about the Pole of the Ecliptick, as 39^ to 40", 4. The half of tills is the Angle A C B*(as repre- fented f . ibid. pag. 489. 1. 15. leg. hexaedra . p.490. 1. 27. leg, ^r. £ 5B5-1- 14. leg* thirtythree , c pag. 294* 1, 23. le '. 322.1. 1. 26. leg. l P ’ 4 . P* 55 7 - Eclipfe of the Moon objerved at Liston, n. 400. p. 338. At Pekin China, n. 405. p. 554. Eclipfe of the Sun obferved ^Lisbon, n. 400. p. 335. At Vera Cruz, n. 401. p. 388/ Near Lisbon, n. 403. p. 471. At Rome, ib. p. 473. At Bologna, ib. p. 477. At Padua, ib. p. 479. At Ingolftadt, n. 405. p. 558. Elephants, their Teeth and Bones found under Ground, n. 403. p. 457. n. 404. p. 497- Experiments on the Fffeffs of the Poifon of a Rattle-Snake, n. 399. p. 309. n. 401. p. 380. For drawing Damps out of Mines, n. 400. p. 353- For meafuring the 'Depths of the Sea, n. 405. p. 559. Several in Opticks , n. 4.06. p. 607. Eyes, a new Operation on them , n. 402. p. 451. F. Falling Stars, the Geographical Longitude of places determinable by them , n. 400. p. 351. Finlanders, an Account of them , n. 400. p. 357. Fire Subterraneous, a Species of it obferved in Kent, n. 399. p. 307 * Fixt Stars, a new Motion difcovered in them , n. 406'. p. 637. Forces of moving Bodies considered , n. 400. p. 343. n. 401. p. 381. Foflil Teeth and Bones of Elephants , n. 403. p. 457. n. 404. p.497. G. Gage to meafure the Depth of the Sea , n. 405. p, 559. Gout, its Nature and Caufes , n. 403. p. 491. Ground, an uncommon Jinking of it, n. 405. p. 551, H. Hernia aquofa, a remarkable one, n. 401. p. 414. Holt-Waters, their Impregation whence, n. 403. p. 489. Hydraulicks, Remarks upon fome Experiments in them, relating to the Forces of moving Bodies, n. 400. p. 34.3. L Iris contrasted , its Cure, n. 402. p. 451. Iron Oar, different Species of it, n. 403. p. 480. Jupiter, his Satellites eclipfed, n. 401. p. 408. n, 402. p c 415. n.404 p. 5 34. n. 405. p. 5.5 3. ibid p. 5 5 7-. K. Kent, an Earthquake felt there, n. 399. p. 305. A Species of fuh- terraneous Fire in that County , n. 399. p. 307. An uncommon Sinking of the Ground in the fame, n. 40 5. p. 551. Kidneys, remarkable Stones found in them, n.402. p. 452. Lateral ■J INDEX. L. Lateral Operation, Thirty three Stones cm out of the Bladder by it, n.404. p. 535. Latitude of Lisbon, n. 401. p. 405?. London and Paris, their Magnitude compared , n. 402. p. 432. Longitude Geographical of ‘Places determiifable from IE ailing Stars,, n. 400. p. 351. Of Vera Cruz, n. 401. p* 389. Long Life, Examples of it, n. 400. p. 364. M. Maniacal Diforders cured by Camphire, n. 400. p. 347. Marriages, an Account of them , n. 400. p. 3 <55. Mars, an Occultation of it by the Moon, n. 405. p. 55^. Materia purulenta per triennium ex ore defluens, n. 400. p. 374. Meteors, ^ new Method for a natural Hiftory of them , n. 401. p. 390. Metals, Obfervations towards a natural Hiftory of them, n. 401. p. 402. n. 403. p. 480. Mines, Experiments for drawing Damps out of them , n. 400. p._ 353. Obfervations towards a natural Hiftory of them, n. 401. p. 402. n. 403. p. 480. Mifleto, its germinating ‘Principle, n. 3 99. p. 5 otf. Of different Sex , n. 405. p. 54.7. Moon, an Eclipfe of it obferved at Lisbon, n. 400. p. 338. At Pe¬ kin in China, n. 405. p. 554. Mortality, Bills of it, n. 400. p. 365. Motion, A new one difcovered in the fixt Stars , n. 4 c6. p. 637. Moving Bodies, their Forces conftdered , n. 400. p. 343. n. 401. p. 381. Mountains, the Heights of feveral meafur'd by the Barometer, n! 405. p. 537. n. 40 6. p. 577. N. Needle, its Variation , n. 401. p. 389. Newton, Sir Ifaac ’5 Chronology defended , n. 399. p. 29^. Of ticks defended , n. 406V p. 596. Norwegian Finns, an Account of them , n. 400. p. 357. Occultation of Venus, n. 404. p. 535. Of Mars by the Moon, n a 405. p. 5 5 6. Omentum, a great Part of it found in the Scrotum , n. 401. p. 414.. Opticks, fever al Experiments concerning them , n. 406'. p. 596. Oxen, their Du&us alimentalis deferibed, n. 404. p. 532. P. Paris and London, their Magnitude compared, n. 402. p. 432. Plants, a Catalogue of fifty , n. 399. p. 293. Exotick, n. 403. p, 485. Poifonous Apparatus cf a Rattle-Snake differed, n. 4or. p. 377. Preternatural perforation in the Stomach , n. 400. p, 36L j 2 Pumice INDEX. Pumice Stones on the main Ocean, n. 402 p. 444. <■ - Q. - v - Queftions Chirurgical ft ate d and anfwered, n. 399. p. 318. R. Rattle-Snake, the EffeHs of its Poifon, n. 399. p. 309. n. 401. p 380. Itspoifonous apparatus , n. 401. p.377. Rizzetti, his Book of Of ticks refuted, n. 406". p. 59^. Roman Pavement in Lincolnfhire, n. 402. p. 428. Roots impojftble of adfeEled Aquations, n. 404. p. 515. # S. Saffron, its Culture, n. 405. p. 566. Sea, a Gage-taweafure the Depth of it , n. 405. p. 559. Seeds exotick raifed in England, n. 403. p. 485. Skeleton of an extraordinary Large?iefs, n. 400. p. 3^3. Specifick Gravity of Tin-Cryftals to the Metal , n. 403. p. 484. Spleen of an enormous Size , n. 401. p. 414. Stars, a new Motion difcovered in them , n 40 6 . p. eT3 7 . Stomach, a preternatural perforation in it , n. 400. p. 3^1. Stones, Sixty found in the Bladder, n. 401. p. 413. Several in the Veficulae Seminales, ibid. p. 414. Remarkable Ones in both Kid¬ neys, n. 402. p.452. Thirty three cut fuccefsfully out of the Bladder, n. 404. p. 535. Sun, an Eclipfe of it obferved at Lisbon, n. 400. p. 338. At Vera Cruz, n. 401. p. 388. Near Lisbon, n. 403. p. 471. At Rome, ibid. p. 473. At Bologna, ibid, p.477. Ad Padua, ibid. .479. At Ingoldffadt, n. 405. p. 558. Surgery, two ghieftions in it ftated and anfwered, n. 399. p. 318. Swifferland, the Heights of its Mountains meafured, n. 405. p. 537. n. 406". p. 577. T. Teeth and Bones of Elephants found under Ground, n. 403. p. 459. n. 404. p. 497- Tin Oar, its Compofnion, n. 403. p. 482. Specifick Gravity of its Cryfials to the Metal, ibid. p. 484. Tin-Slates, the Method of making them, n. 406. p. 637. Tumours, two extraordinary ones of the Abdomen , n. 405. p. 562. V. Variation of the Needle, n. 401. p. 389. Venus, an Occultation of it by the Moen,cbferved at Eologna, n. 404. p. 5 5 5 • Vera Cruz, Longitude of it, n. 401. p. 389. Veficulae Seminales, Stones found in them, n. 401. p. 414. Villi of the Stomach of Oxen, n. 404. p. 5 32. Virgo eclipfed by the Moon, n. 404. p. 5 34. FINIS . ’