ill: ■ ■I 1 f i( mm «Mm- IVNflll^' ~ V 1 i : j u V 4 dr&$* ^fc^-&*^ JFM> f///'r //'/// ///s ;//yv// '' //a/// /■ ujy TUB- &WAM W£€> mmmx k, a cih d oil rnu^a' 2-AOE JJ.3 JD) © IK. I C ]B-©C]K., XtAKTE 3 iLTiBiU [©1 ■11BANY, PUBLISHED BY E.& NARRATIVE JOUHWVL GJ? AV ' tJi M I ■- I > :> — — -> — n^s* ^ . >«ioip.b» roaJJiyS-JasS na o*!ot?;:; • ft n J5 s >th of April, there was still some snow to be seen in situa- tions shaded by the buildings or fences, but it had entirely disappeared in the roads, and in the open fields. The roads continued muddy to Onondaga East Hill ; on the West Hill, they were dry, and so continued with partial exceptions, to Geneva, where the clouds of dust by which we were enveloped, and the appearances of vegetation, indicated the benign climate which pervades the luxuriant country of the Genesee. Every appearance indicated a season ten days more advanced than the valley of the Mohawk, which is only separated by the distance of a hundred miles. The wild poplar put forth leaves on the 18th, the house popular (populus dilataid) on the 23d, apricots were in blossom on the 22d. The ther- mometer observed at one o'clock, P. M. varied, be- tween the 1 lth and 28th, from 60°, to 78°, of Fahren- heit, during which period the weather was clear, mild, and pleasant, with the exception of a fall of rain on the 26th and 27th. The village of Geneva, occu- pying a beautiful eminence at the head of Seneca Lake, and surrounded by a district of country, under creased nearly in the same proportion. The census in the several counties, for 1820, is not yet completed ; but the total population in the territory, which, only thirty years since, contained but ten hundred and eighty one souls, doubtless exceeds two hundred tiioisand ! ! — We doubt whether a parallel can be found] in the rise and progress of any country in any age." — JY. Y. Statesman. 31 a high state of cultivation and improvement, pre- sents a most picturesque appearance, on approach- ing it in a clear day from the east; and the display of the town, so highly favoured by local advantages, at the distance of a mile, creates an idea of wealth, taste, and business, which is not disappointed on be- holding it the centre of a populous agricultural dis- trict, the mart of its produce and the theatre of its exchange, where the intersection of several import- ant roads, and a branch of the Erie Canal, facilitate a ready intercourse with all parts of the state. A person of information who has had opportunities of occular comparison, is disposed to consider the na- tural advantages of this village and vicinity, as a place susceptible of rural embellishments, superior to that of the celebrated city of Switzerland, in allu- sion to which it has been named. On the 28th of April. 1 left Geneva, and passing through Canandaigua, Bloomfield, and Lima, lodged at Avon, upon the banks of Genesee river. On the following day we passed through Caledonia, Le Roy, Batavia, Pembroke, and Clarence, and arrived at Buffalo in the evening, a distance of 210 miles from Utica. This route lies across the populous coun- ties of Ontario, Genesee, and Niagara, colloquially known under the name of the Genesee country, and proverbial for the fertility of its soil.* We found * At the annual fair and cattle show in Ontario county, in the fall of 1 819) premiums were awarded on the following articles, viz : Best winter wheat, 80 hushels 12 qts. on the acre. Barley, 34 bushels on the acre. Peas, 32 bushels 4 qts. on the acre. — Canandaigua Paper. In Onondaga county at the agricultural fair of the same season, premiums were awarded on, 32 the peach, and the earlier varieties of apple tree, eiery where in blossom, and the beech (fagusferru- ginea,) the wild poplar, or the American Aspen, and some other species of the early sprouting forest trees, already gave the forest a vernal aspect. These ap- pearances continued until within eight or ten miles of Buffalo, where the influence of the lake winds, and the bodies of unmelted ice in the lakes, have a sensible effect upon the progress of vegetation, which appears to be retarded eight or ten days later on account of this exposure. The peach tree had there budded, but not yet blown. We found the lake still covered with floating ice, and no vessel had The best Winter Wheat, 37 bushels 14lbs. to the acre. do. do. do. do. 12 qts. do. Onondaga paper. In Oneida County, at the annual fair and cattle show, of the same season, the following; articles received premiums : Winter Wheat, Reuben Gridley, of Paris, two acres 72 bushels per acre. Spring Wh f at, Jona. Wilcox, Paris, 44 bushels per a<*re. Indian Corn. Samuel Cary, DeerfiVld. 1 19 bushels per acre. Barley, R. Soutluvcrth, Paris, 56 bushels 28 quarts per acre. Oats, J^d. Sanger, Whitestown. 84^ per. acre. Feas, D. Barton, Paris, 52 bushels, per acre. Potato's, A. Bartlett, Paris, 5( 5 bu-hels per acre. Butter, D. Barton, Paris, had already made 3107 pounds from 21 cows. — Plough Boy and Journal of the Board of Agriculture by S. Southivick, Vol. 1. But the greatest product of Indian corn raised during this sea- son, and perhaps the greatest ever known, was by Mr. Jedediah Pusenbury, of Portland, Chautauque county, which was 132 bush- els 12 quarts from an acre. — Plough Boy, Vol. 1. p. 199 Spring 23 33 Barley 41 17 Flax, 350 lbs. Oats, 54 11 Corn, 121 12 33 attempted the navigation. The steam boat had ad- vertised to start on her first trip, on the first of May, but the backward state of the weather, and the ice in the lake, had induced the captain to defer it until the 6th, leaving me a week to visit the Falls of Ni- agara, and the battle grounds on the north banks of the Niagara. The town of Buffalo contained a hundred houses, besides the county buildings, in 1810.* On the 30th of December, 1813, it was burnt by a party of Bri- tish troops and Indians, who laid waste this frontier. It has since been rebuilt with increased elegance, and is now a town of about 200 gildings, a pro- portion of which are of brick. It occupies an em- inence, which was recommended to the French go- vernment, as a commanding site for a garrison, by the Baron La Hontan, in 1693, and marked Fort Suppose, upon his map.f The first vessel which navi- gated Lake Erie, was built in this vicinity by La Sal- le, in 1679, being a vessel of sixty tons burden.f A part of the tribe of the Seneca Indians, about 700 souls, are located in this vicinity. The village of Black Rock, the residence of Gen. Peter B. Porter, is situated two miles below, at a spot which is sup- posed to unite superior advantages, as a place of trade, and a harbour for vessels. On the first of May, I visited the celebrated Falls of Niagara,^ situated 22 miles below. Keeping the * Spafford. t La Hontan's New Voyages to Canada, p. 187, vol. 1, | Smith's History of New-York, p. 80. § This is an Iroquois word said to signify the thunder of waters, and the word as still pronounced by the Senecas is O-niraa-gardh, 5 34 American shore, the road lies over an alluvial coun- try, elevated from ten to twenty feet above the water of the river, without a hill, or a ledge of rocks, and with scarce an undulation of surface, to indicate the existence, or prepare the eye for the stupenduous prospect which bursts, somewhat unexpectedly, into view. The day was clear and warm, with a light breeze blowing down the river. We stopped fre- quently on our approach to listen for the sound of the Fall, but at the distances of fifteen, ten, eight, and even five miles, could not distinguish any, even by laying the ear to the ground. It was not until within three miles of the precipice, where the road tuns close to the edge of the river, and brings the ra- pids in full view, that we could distinctly hear the sound, which then, owing to a change of the wind, fell so heavy upon the ear, that in proceeding a short distance, it was difficult to maintain a conversation, as we rode along. On reaching the Falls, nothing struck me with more surprise, than I hat the Baron La Hon- tan, who visited it in August, 1638, should have fal- len into so egregious a mistake, as to the height of the perpendicular pilch, which he represents at seven or ei^ht hundred feet* Nor does the narrator of the discoveries of the unfortunate La Salle, Monsieur Tout i, approach much nearer to the truth, when he states it at six hundred fcet.t Charlevoix, whose work Veingtsfrongl accentuated on the third syllable, while the interjec- tion O, is ho feebly uttered, that without a nice attention, it may escape notice. * La Honian's Voyages, vol. I. p. 82. t An Account of the last Expedition and Discoveries of Mon- sieur 1)^ La Salle.— -Collections of the Mw-Yorlc Historical Society . Vol. II. p. 228. 35 is characterized by more accuracy, learning, and re- search, than those who had preceded him, and who saw the Falls in 1721, makes, on the contrary, an es- timate which is surprising for the degree of accuracy he has attained. " For my own part," he says, " af- ter examining it on all sides, where it could be view- ed to the greatest advantage, I am inclined to think we cannot allow it less than a hundred and forty or fifty feet."* The latter, (one hundred and fifty) is precisely what the Fall on the Canadian side, is now estimated at. There is a rapid of two miles in ex- tent above, and another of seven miles, extending to Lewiston, below the Falls. The breadth across, at the brink of the Fall, which is serrated and irregular, is estimated at four thousand two hundred and thirty feet, or a little more than three-fourths of a mile. The Fall on the American shore is one hunderd and sixty-four feet, being the highest known perpendi- cular pitch of so great a volume of water.f The fall of the rapid above, commencing at Chippewa, is estimated at ninety feet, and the entire fall of Niaga- ra river from Lake Erie to Lake Ontario, a distance of thirty-five miles, at three hundred feet. Goat Island, which divides the water into two unequal sheets, has recently been called /m,(in allusion to the perpetual rain bows by which it is characterized) by * Charlevoix's Journal of a Voyage to North America, vol. I. p. 353. t Tt is in the volume of falling water only, that Niagara claims a pre-eminence. There are many higher falls in various parts of South America and Europe. The greatest water fall in Eurupe,' is on the river Lattin, in Lapland, which is half a mile wide, and has a perpendicular pitch of 400 feet, 36 the commissioners for settling the boundaries of the United States, acting under the treaty of Ghent. In approaching this cataract from Lewiston, the elevat- ed and rocky description of country it is necessary to cross, together with the increased distance at which the roar is heard in that direction, must serve to prepare the mind for encountering a scene which there is nothing to indicate on approaching from Buf- falo ; and this impression unquestionably continues to exercise an effect upon the beholder, after his ar- rival at the falls. The first European visitors be- held it und«r this influence. Following the path of the Couriers de Bois, they proceeded from Montreal up the St Lawrence, to Fort Caderacqui, and around the shores of Lake Ontario, to the alluvial tract which stretches from the mouth of Niagara river, to the site of Lewiston. Here the Ridge, emphatically so cal- led, commences, and the number of elevations which it is necessary to ascend in crossing it, may, without a proper consideration of the intermediate descents, have led those who formerly approached that way into error, such as La Hontan, and Tonti fell into. They must have been deprived also of the advanta- ges of the view from the gulph at the foot of the Falls, for we are not prepared to admit the possibility of a descent without artificial stairs, or other analogous labourious and dangerous works, such, as at that re- mote period, must have been looked upon as a stu- pendous undertaking ; and could not, indeed, have been accomplished, surroundc d as the French then were, by their enemies, the jealous and ever watchful Iroquois. The descent at the present period, with every advantage arising trom the labours of mechan- ical ingenuity, cannot be performed without feeling 37 , some degree of personal solicitude. It is in this chasm that the sound of the water, falls heaviest upon the ear, and that the mind becomes fully impressed, with the appalling majesty of the Fall. Other views from the banks on both sides of the river, and from the Island of Iris, in its centre, are more beautiful and picturesque; but it is here that the tremulous motion of the earth, the clouds of irridescent spray, the broken column of falling water, the stunning sound, the lofty banks of the river, and the wide spread- ing ruin of rocks, imprint a character of wonder and terror upon the scene, which no other point of view is capable of producing. The spectator, who, on alighting at Niagara, walks hastily to the brink, feels his attention imperceptibly rivited to the novel and striking phenomenon before him. and. at this moment, is apt either to over-rate or to under- ratethe magnitude of the Fall. It is not easy to erect a standard of comparison ; and the view requires to be studied in order to attain a just conception and ap- preciation of its grandeur and its beauties. The ear is at first stunned by the incessant roar, and the eye bewildered in the general view. In proportion as these become familiarized, we seize upon the individual fea- tures of the landscape, and are enabled to distinguish between the gay and the sombre, the bold and the picturesque, the harsh and the mellow traits, which, like the deep contrasted shades of some high wrought picture, contribute to give effect to the scene. It was some time before I could satisfy myself of the ac- curacy of the accredited measurements of the height of the Fall, and not until after I had made repeated visits, and spent a considerable time in the abyss below. There appears a great disproportion be- 38 tween the height and the width of the falling sheet, but the longer 1 remained, the more magnificent it appeared to me ; and hence it is, that with some- thing like a feeling of disappointment, on mv first arrival, I left the Falls, after a visit of two days, with an impression of the scene, which every thing I had previously read, had failed to create. At the time of my visit, the wind drove the floating ice out of Lake Erie, with the drift wood of its tributary rivers, and these were constantly precipitated over the Falls, but we were not able to discover any vestiges of them in the eddies below. Immediately in front of the sheet of falling water, on the American side, there was also an enormous bank of snow, of nearly an hundred feet in height, which the power of the sun had not yet been fierce enough to dissolve, and which, by giving an Icelandic character to the land- scape, produced a fine effect. It appeared to me to owe its accumulation, to the falling particles of froz- en spray. What has been said by Goldsmith, and repeated by others, respecting the destructive influence of the rapids above, to ducks and other water fowl, is only an effect of the imagination. So far from being the case, the wild duck, is often seen to swim down the rapid to the brink of the Falls, and then fly out, and repeat the descent, seeming to take a delight, in the exercise. Neither are small land-birds affected on flying over the Falls, in the manner that has been sta- ted. I observed the blue bird and the wren, which had already made their annual visit to the banks of the Niagara, frequently fly within one or two feet of the brink, apparently delighted with the gift of their wings, which enabled them to sport over such fright- 39 ful precipices, without danger. We are, certainly, not well pleased to find, that some of the wonderful stories, we have read of the Falls, during boyhood, do not turnout to be the truth; but, at the same time, a little attention is only necessary to discover, that many interesting facts and particulars, remain unnoticed, which fully compensate for others, that have been overstrained or misstated. Among these, the crystalline appearances, disclosed among the prostrate ruins, and the geological character of the Fall itseli. are not the least interesting. The scenes where nature has experienced her greatest convulsions, are always the most favourable for acquiring a knowledge of the internal structure of the earth. The peaks of the highest mountains, and the depths of the lowest ravines, present the greatest attractions to the geologist. Hence this cataract, which has worn its way for a number of miles, and to a very great depth, through the stony crust of the earth, is no less interesting for the geo- logical facts it discloses, than for the magnificence of its natural scenery. The chain of highlands, called the Ridge, originates in Upper-Canada, and running parallel with the south shore of Lake Onta- rio, forms a natural terrace, which pervades the wes- tern counties of New-York, from north to south, af- fording, by its unbroken chain, and the horizontal position ot its strata, the advantages of a natural road, and terminates in an unexplored part of the county of Oswego, or thereabout. It is in crossing this ridge, that the Falls of the Niagara, of the Gene- Bee, and of the Oswego rivers, all running into Lake Ontario, are produced ; together with those of an infinite number of smaller streams and brooks. — 40 Through this, the Niagara has cut its way tor a dis- tance of seven miles, and to a depth of more than two hundred feet, disclosing the number, order of stratification, and mineral character, of the different strata of secondary rocks, of which it is composed. These are, beginning at the lowest visible point, red sand stone, fragile slate, and fetid limestone, the lat- ter occupying the surface, and imbedding crystals of calcareous spar,* and foliated gypsum.f How far these formations, in the order in which they are here seen, continue towards the south, and extend la- terally towards the east and the west, the want of more extensive observations, prevents us from deter- mining. A similar formation exists at Genesee Falls, and the sand stone stratum, continues unbroken to Oswego, where it is quarried for the purposes of building.^ It is probable, that the slate rock, vari- ously modified, and combined, extends throughout the Genesee country, as it is found on the banks of the Seneca Lake, — the Cashong, Flint, and Allen's Creeks, — in the towns of Le Roy, and Clarence in digging wells, — on the banks of Lake Erie, at Ham- * Kalk spath. Werner. Common spar. Kirwan. Calc spar. Jamison. Chaux carbonatee pure spathique. Brongnairt. Chaveland. f Selenite. Cleaveland. Fraueneis. Werner. | The sand stone of Oswego, has been employed with some success, for the hearths, and lining of glass and iron founderies where the intense degree of heat employed, renders the discovery of the most refractory rocks, an object of constant solicitude. In- telligent manufacturers will see the important application of geo- logical science, in tracing the formations of rocks, upon which they are any wise dependant, into the vicinity of their manufacto- ries. 41 burgh, — on Mud Creek, near Canandaigua — on the outlet of Honey oye, and Caneseus Lakes, and on the Conostaga fork of the Genesee.* At the three lat- ter places, it is so highly charged with bitumen, as to be capable of supporting combustion. The inflam- mable gas of the burning springs of Ontario, and the fountain of petroleum of Cattaraugus county, afford additional evidence of the existence of carbon and bitumen in the shistose rocks of the Genesee, and render it probable, that mineral coal, the dis- covery of which, has become so great a desidera- tum, will reward the future researches of the geolo- gist, and the miner in this region. The secondary character of the Genesee slate, is particularly appa- rent upon the banks of the Cashong creek, in Onta- rio county, where it imbeds various species of comJio- lites and erismatolites, together with globular masses of granular limestone. Along the southern borders of Seneca lake, it contains numerous impressions of univalve shells, and mollusca. The surface rock of this region, (limestone) which is fetid at Niagara, either does not preserve a uni- form character, or is succeeded by local formations of calcareous carbonats, of various character and extent. Thus, it is compact shelly (forming a shell marble,) at Wolcott, in Seneca county, and at Bath, in Steuben county; while the greater part of Onta- rio, Allegany, Chautauque, and Genesee, is charac- * For several of these localities, I am indebted to the observa- tions of Mr. C. K Guernsey, of Lima, a gentleman whose habits of observation, during occasional excursions through (hat county, has led him to notice many of those mineral coincidences and appear- ances,from which the geologist is enabled to draw the most import fant conclusions. 42 terized by an earthy, dull grey, compact limestone, which gives out no odour in breaking, contains shells, sparingly imbedded, and burns to a good quicklime. It is in this formation, that the gypsum beds of Caledonia, Vienna, and Waterloo, are situ- ated ; and which, also, appears in the vicinity of the sulphur springs, in Farmington,* and the beds of lenticular oxyd of iron,t in Palmyra, Williamson, * For an account of these springs, see a Memoir, by J. H. Redfield, in the 2d vol of the Literary and Philosophical Reper- tory. A'so, Dr. Mitchill's Descriptive Catalogue of Minerals, vol. I. p-3. Bruce's Minera logical Journal. t During the session of the legislature of New-York, in the win- terof 1820, a loan of $10,000, was made to A. Cole, and asso- ciates, to enable them to commence the manufacture of bar iron, from the se beds of ore ; and it is understood, that works are row in opera ion, at which a very malleable iron is manufactured. According to an analysis ol this re, by Professor Eaton, of Bur- lington Col'ege, (see Eaton's Geolog' , p. 266,) it yields thirty per centum of metallic iron, and the on 1 contains petrefied voluti- ns, small and well characterized. I am indebted to Mr. Andrew !\I'Nat, of Geneva, for the fol owing interesting account, of the locaii'.y of this mineral, ac< ompanied hy specimens of the ore. " MEMORANDUM. " Lenticular Argillaceous oxyd of Iron. " TWO VARIETIES. "Var. 1st. — A bright red, inclining to purple. — Is found in the towns of Oniari ■, Williamson, Penfield, and Sodus, in Ontario county. The small r d of ir>n, accompanying it, was wrought from this ore, at forges erected, and now in operation, in the town of Ontario. The ore is found in great abundance, (quantity sup- po>ed to be inexhaustible) in a strip of country, about a mile in width, and midway ' etween the Ridge (Niagara) Road, and the south shore of Lake Ontario, which are about an average of four miles apart, and nearly parallel with each other. The ore is found, geneially. ai the depth of three to five feet below the sur- face, and appears to extend downwards a considerable depth — 43 and Wolcott, in Ontario county. In the town of Caledonia it serves as the basis, to several varie- ties of madrepores, and corrallines, found in a state of petrefaction, and in the oak openings of Niagara county, it incloses nodules of hornstone.* This hornstone, is also found among the debris, of the Falls of Niagara, accompanied by radiated quartz, rhomboidal crystals of carbonate of lime, foliated and snowy gypsum, and slight traces of the sul- phuret of zinc.f These rocks, (sandstone, slate, and limestone) perhaps 10 to 15 feet, growing better as it descends. The upper soil, is a reddish sandy loam — then a species of greenish clay, resting upon the ore. The < re is sometimes wrapt up in insolaled roundish masses — sometimes in extended beds, similar to gypsum beds or quarries. " VAR.2d. — A dark red, inclining to brown. — Is found in (he town of Wolcott, Seneca county, on the inlet of P