Notes on the State of Virginia, by Thomas Jefferson

Notes on the State of Virginia, by Thomas Jefferson

Postby admin » Wed Jul 29, 2015 3:53 am

NOTES ON THE STATE OF VIRGINIA
by Thomas Jefferson
Illustrated with a Map, Including the States of Virginia, Maryland, Delaware and Pennsylvania.
A New Edition, Prepared by the Author, Containing Notes and Plates Never Before Published
J.W. Randolph
121 Main Street, Richmond, VA., 1853

NOTICE: THIS WORK MAY BE PROTECTED BY COPYRIGHT

YOU ARE REQUIRED TO READ THE COPYRIGHT NOTICE AT THIS LINK BEFORE YOU READ THE FOLLOWING WORK, THAT IS AVAILABLE SOLELY FOR PRIVATE STUDY, SCHOLARSHIP OR RESEARCH PURSUANT TO 17 U.S.C. SECTION 107 AND 108. IN THE EVENT THAT THE LIBRARY DETERMINES THAT UNLAWFUL COPYING OF THIS WORK HAS OCCURRED, THE LIBRARY HAS THE RIGHT TO BLOCK THE I.P. ADDRESS AT WHICH THE UNLAWFUL COPYING APPEARED TO HAVE OCCURRED. THANK YOU FOR RESPECTING THE RIGHTS OF COPYRIGHT OWNERS.


Table of Contents:

• Preface of the Publisher
• Advertisement
• 1. Boundaries of Virginia
• 2. Rivers
• 3. Seaports
• 4. Mountains
• 5. Cascades
• 6. Productions, mineral, vegetable and animal
• 7. Climate
• 8. Population
• 9. Military force
• 10. Marine force
• 11. Aborigines
• 12. Counties and towns
• 13. Constitution
• 14. Laws
• 15. Colleges, buildings and roads
• 16. Proceedings as to Tories
• 17. Religion
• 18. Manners
• 19. Manufactures
• 20. Subjects of commerce
• 21. Weights, measures and money
• 22. Public revenue and expenses
• 23. Histories, memorials and State papers
• Appendix No. I
• Appendix No. II
• Appendix No. III
• Appendix No. IV. Papers relative to the murder of Logan's family
• Translations of notes
• Plates and Topographical Analysis
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Re: Notes on the State of Virginia, by Thomas Jefferson

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A map of the country between ABEMARLE SOUND, and LAKE ERIE, comprehending the whole of VIRGINIA, MARYLAND, DELAWARE and PENNSYLVANIA, with parts of several other of the United States of America. -- Engraved for Jefferson's Notes on Virginia. J.W. Randolph, Richmond, Va. 1853. The country on the eastern side of the the Alleganey Mountains, is taken from Fry and Jefferson's Map of Virginia and Scull's Map of Pennsylvania, which were constructed chiefly on actual survey that on the western side of the Alleganey, is taken from Hutchins, who went over the principal water courses, with a compass and log line, correcting his work by observations of latitude: additions have been made, where they could be made on sure ground. Engraved on stone by Friend & Aub. 80, Walnut St. Phil.

PREFACE OF THE PUBLISHER.

Thomas Jefferson left at his death a printed copy of his Notes on Virginia, containing many manuscript notes, several plates and a map, intended apparently for a new edition of the work. As an edition had then been recently published, it was deemed best to delay any further publication until the book should become scarce. It is now nearly out of print, and a general desire is expressed for another edition. With a view of gratifying this wish, Mr. Jefferson's executor, Thomas Jefferson Randolph, has transferred to the publisher the materials prepared by the author for the new edition.

In making this preparation the author used a copy of the first edition, and thus inadvertently repeated an error in the narrative preceding Logan's speech, which had been corrected in a later edition. An historical statement making the correction, deduced by the author from certain documents, and the documents themselves, will be found in Appendix No. IV. They are taken from a re-print of the work in 1825.

The manuscript notes of the present edition are numerous and interesting. Many are in foreign languages, and disclose the extensive erudition of the author. Professor Schele De Vere, the accomplished and learned incumbent of the Chair of Modern Languages of the University of Virginia, has been kind enough to translate the French, Spanish and Italian notes. These translations will be found in Appendix No. IV.

The circumstances under which the Notes on Virginia were written, are stated by the author in his preface. It may be well to add, that the foreigner of distinction to whom they were ad- dressed was Mons. Barbe De Marbois, the Secretary of the French Legation in the United States, and that they were written while the author was confined to his room by an injury received from the falling of his horse.

The beauty of style, the accuracy of information, and the scientific research displayed in the Notes have made them a permanent part of our national literature. The publisher therefore conceives that in publishing a new edition of this admirable work, he is renewing a valuable contribution to that literature, and rendering a just tribute to the illustrious author. September 13, 1853.
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Re: Notes on the State of Virginia, by Thomas Jefferson

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ADVERTISEMENT.

The following Notes Were written in Virginia in the year 1781, and somewhat corrected and enlarged in the winter of 1782, in answer to Queries proposed to the Author, by a Foreigner of Distinction, then residing among us. The subjects are all treated imperfectly; some scarcely touched on. To apologize for this by developing the circumstances of the time and place of their composition, would be to open wounds which have already bled enough. To these circumstances some of their imperfections may with truth be ascribed; the great mass to the want of information and want of talents in the writer. He had a few copies printed, which he gave among his friends; and a translation of them has been lately published in France, but with such alterations as the laws of the press in that country rendered necessary. They are now offered to the public in their original form and language.

February 27, 1787.
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Re: Notes on the State of Virginia, by Thomas Jefferson

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QUERY I.

AN EXACT DESCRIPTION OF THE LIMITS AND BOUNDARIES OF THE STATE OF VIRGINIA?


Virginia is bounded on the East by the Atlantic; on the North by a line of latitude, crossing the Eastern Shore through Watkins's Point, being about 37° 57' North latitude; from thence by a straight line to Cinquac, near the mouth of Patowmac; thence by the Patowmac, which is common to Virginia and Maryland, to the first fountain of its Northern branch; thence by a meridian line, passing through that fountain till it intersects a line running East and West, in latitude 39° 43' 42.4", which divides Maryland from Pennsylvania, and which was marked by Messrs. Mason and Dixon; thence by that line, and a continuation of it westwardly to the completion of 5 degrees of longitude from the Eastern boundary of Pennsylvania, in the same latitude, and thence by a meridian line to the Ohio: on the West by the Ohio and Missisipi, to latitude 36° 30' North; and on the South by the line of latitude last mentioned. By admeasurements through nearly the whole of this last line, and supplying the unmeasured parts from good data, the Atlantic and Missisipi are found in this latitude to be 758 miles distant, equal to 13° 38' of longitude, reckoning 55 miles and 3,144 feet to the degree. This being our comprehension of longitude, that of our latitude, taken between this and Mason and Dixon's line, is 3° 13', 42.4", equal to 223.3 miles, supposing a degree of a great circle to be 69 m. 864 f., as computed by Cassini. These boundaries include an area somewhat triangular, of 121,525 square miles, whereof 79,650 lie westward of the Alleghaney mountains, and 57,034 westward of the meridian of the mouth of the Great Kanhaway. This State is therefore one-third larger than the islands of Great Britain and Ireland, which are reckoned at 88,357 square miles.

These limits result from — 1. The ancient charters from the crown of England. 2. The grant of Maryland to the Lord Baltimore, and the subsequent determinations of the British Court as to the extent of that grant. 3. The grant of Pennsylvania to William Penn, and a compact between the General Assemblies of the Commonwealths of Virginia and Pennsylvania as to the extent of that grant. 4. The grant of Carolina, and actual location of its Northern boundary, by consent of both parties. 5. The treaty of Paris of 1763. 6. The confirmation of the charters of the neighboring States by the Convention of Virginia at the time of constituting their Commonwealth. 7. The cession made by Virginia to Congress of all the lands to which they had title on the North side of the Ohio.
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Re: Notes on the State of Virginia, by Thomas Jefferson

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QUERY II

A NOTICE OF ITS RIVERS, RIVULETS, AND HOW FAR THEY ARE NAVIGABLE?


An inspection of a map of Virginia will give a better idea of the geography of its rivers than any description in writing. Their navigation may be imperfectly noted.

Roanoke, so far as it lies within this State, is no where navigable but for canoes or light batteaux; and, even for these, in such detached parcels as to have prevented the inhabitants from availing themselves of it at all.

James River and its waters afford navigation as follows:

The whole of Elizabeth River, the lowest of those which run into James River, is a harbor, and would contain upwards of 300 ships. The channel is from 150 to 200 fathom wide, and at common flood tide affords 18 feet water to Norfolk. The Strafford, a 60 gun ship, went there, lightening herself to cross the bar at Sowell's Point. The Fier Rodrigue, pierced for 64 guns, and carrying 50, went there without lightening. Craney Island, at the mouth of this river, commands its channel tolerably well.

Nansemond River is navigable to Sleepy Hole for vessels of 250 tons; to Suffolk for those of 100 tons; and to Milner's for those of 25.

Pagan Creek affords 8 or 10 feet water to Smithfield, which admits vessels of 20 tons.

Chickahominy has at its mouth a bar, on which is only 12 feet water at common flood tide. Vessels passing that, may go 8 miles up the river; those of 10 feet draught may go 4 miles further; and those of 6 tons burthen 20 miles further.

Appamattox may be navigated as far as Broadways by any vessel which has crossed Harrison's Bar in James River; it keeps 8 or 9 feet water a mile or two higher up to Fisher's Bar, and 4 feet on that and upwards to Petersburgh, where all navigation ceases.

James River itself affords harbor for vessels of any size in Hampton Road, but not in safety through the whole Winter; and there is navigable water for them as far as Mulberry Island. A 40 gun ship goes to James Town, and, lightening herself, may pass to Harrison's Bar, on which there is only 15 feet water. Vessels of 250 tons may go to Warwick; those of 125 go to Rocket's, a mile below Richmond; from thence is about 7 feet water to Richmond; and about the centre of the town, 4 feet and a half, where the navigation is interrupted by falls, which, in a course of 6 miles, descend about 80 feet perpendicular; above these it is resumed in canoes and batteaux, and is prosecuted safely and advantageously to within 10 miles of the Blue Ridge; and even through the Blue Ridge a ton weight has been brought; and the expense would not be great, when compared with its object, to open a tolerable navigation up Jackson's River and Carpenter's Creek, to within 25 miles of Howard's Creek of Greenbriar, both of which have then water enough to float vessels into the Great Kanhaway. In some future state of population, I think it possible that its navigation may also be made to interlock with that of the Patowmac, and through that to communicate by a short portage with the Ohio. It is to be noted, that this river is called in the maps James River, only to its confluence with the Rivanna; thence to the Blue Ridge it is called the Fluvanna; and thence to its source, Jackson's River. But, in common speech, it is called James River to its source.

The Rivanna, a branch of James River, is navigable for canoes and batteaux to its intersection with the Southwest mountains, which is about 22 miles; and may easily be opened to navigation through those mountains to its fork above Charlottesville.

York River, at York Town, affords the best harbor in the State for vessels of the largest size. The river there narrows to the width of a mile, and is contained within very high banks, close under which the vessels may ride. It holds 4 fathom water at high tide for 25 miles above York to the mouth of Poropotank, where the river is a mile and a half wide, and the channel only 75 fathom, and passing under a high bank. At the confluence of Pamunkey and Mattapony, it is reduced to 3 fathom depth, which continues up Pamunkey to Cumberland, where the width is 100 yards, and up Mattapony to within 2 miles of Frazer's Ferry, where it becomes 2J fathom deep, and holds that about 5 miles. Pamunkey is then capable of navigation for loaded flats to Brockman's Bridge, 50 miles above Hanover Town, and Mattapony to Downer's Bridge, 70 miles above its mouth.

Piankatank, the little rivers making out of Mobjack Bay, and those of the Eastern Shore, receive only very small vessels, and these can but enter them.

Rappahanock affords 4 fathom water to Hobb's Hole, and 2 fathom from thence to Fredericksburg.

Patowmac is 7-1/2 miles wide at the mouth; 4-1/2 at Nomony Bay; 3 at Aquia; 1-1/2 at Hallooing Point; 1-1/4 at Alexandria. Its soundings are, 7 fathom at the mouth; 5 at St. George's Island; 4-1/2 at Lower Matchodic; 3 at Swan's Point, and thence up to Alexandria; thence 10 feet water to the falls, which are 13 miles above Alexandria. These falls are 15 miles in length, and of very great descent, and the navigation above them for batteaux and canoes is so much interrupted as to be little used. It is, however, used in a small degree up the Cohongoronta branch as far as Fort Cumberland, which was at the mouth of Wills's Creek, and is capable, at no great expense, of being rendered very practicable. The Shenandoah branch interlocks with James River about the Blue Ridge, and may perhaps in future be opened.

The Missisipi will be one of the principal channels of future commerce for the country westward of the Alleghaney. From the mouth of this river, to where it receives the Ohio, is 1,000 miles by water, but only 500 by land, passing through the Chickasaw country. From the mouth of the Ohio, to that of the Missouri, is 230 miles by water, and 140 by land. From thence to the mouth of the Illinois River is about 25 miles. The Missisipi, below the mouth of the Missouri, is always muddy, and abounding with sand bars, which frequently change their places. However, it carries 15 feet water to the mouth of the Ohio, to which place it is from one and a half to two miles wide, and thence to Kaskaskia, from one mile to a mile and a quarter wide. Its current is so rapid, that it never can be stemmed by the force of the wind alone, acting on sails. Any vessel, however, navigated with oars, may come up at any time, and receive much aid from the wind. A batteau passes from the mouth of Ohio to the mouth of Missisipi in three weeks, and is from two to three months getting up again. During its floods, which are periodical, as those of the Nile, the largest vessels may pass down it if their steerage can be ensured. These floods begin in April, and the river returns into its banks early in August. The inundation extends further on the Western than Eastern side, covering the lands in some places for 50 miles from its banks. Above the mouth of the Missouri, it becomes much such a river as the Ohio, like it clear, and gentle in its current, not quite so wide, the period of its floods nearly the same, but not rising to so great a height. The streets of the village at Cohoes are not more than 10 feet above the ordinary level of the water, and yet were never overflowed. Its bed deepens every year. Cohoes, in the memory of many people now living, was insulated by every flood of the river. What was the Eastern channel has now become a lake, 9 miles in length, and 1 in width, into which the river at this day never flows. This river yields turtle of a peculiar kind, perch, trout, gar, pike, mullets, herrings, carp, spatula fish of 50 lb weight, cat fish of 100 lb weight, buffalo fish and sturgeon. Alligators or crocodiles have been seen as high up as the Acansas. It also abounds in herons, cranes, ducks, brant, geese and swans. Its passage is commanded by a fort established by this State, 5 miles below the mouth of Ohio, and 10 miles above the Carolina boundary.

The Missouri, since the treaty of Paris, the Illinois and Northern branches of the Ohio since the cession to Congress, are no longer within our limits. Yet having been so heretofore, and still opening to us channels of extensive communication with the Western and Northwestern country, they shall be noted in their order.

The Missouri is, in fact, the principal river, contributing more to the common stream than does the Missisipi, even after its junction with the Illinois. It is remarkably cold, muddy and rapid. Its overflowings are considerable. They happen during the months of June and July. Their commencement being so much later than those of the Missisipi, would induce a belief that the sources of the Missouri are northward of those of the Missisipi, unless we suppose that the cold increases again with the ascent of the land from the Missisipi westwardly. That this ascent is great, is proved by the rapidity of the river. Six miles above the mouth it is brought within the compass of a quarter of a mile's width; yet the Spanish merchants at Pancore, or St. Louis, say they go 2,000 miles up it. It heads far westward of the Rio Norte, or North River. There is, in the villages of Kaskaskia, Cohoes and St. Vincennes, no inconsiderable quantity of plate, said to have been plundered during the last war by the Indians from the churches and private houses of Santa Fe, on the North River, and brought to these villages for sale. From the mouth of Ohio to Santa Fe is 40 days' journey, or about 1,000 miles. What is the shortest distance between the navigable waters of the Missouri and those of the North River, or how far this is navigable above Santa Fe I could never learn. From Santa Fe to its mouth in the Gulf of Mexico is about 1,200 miles. The road from New Orleans to Mexico crosses this river at the post of Rio Norte, 800 miles below Santa Fe; and from this post to New Orleans is about 1,200 miles; thus making 2,000 miles between Santa Fe and New Orleans, passing down the North River, Red River and Missisipi; whereas, it is 2,230 through the Missouri and Missisipi. From the same post of Rio Norte, passing near the mines of La Sierra and Laiguana, which are between the North River and the River Salina to Sartilla, is 375 miles; and from thence, passing the mines of Charcas, Zacatecas and Potosi, to the City of Mexico, is 375 miles; in all, 1,550 miles from Santa Fe to the City of Mexico. From New Orleans to the City of Mexico is about 1,950 miles; the roads, after setting out from the Red River, near Natchitoches, keeping generally parallel with the coast, and about 200 miles from it, till it enters the City of Mexico.

The Illinois is a fine river, clear, gentle, and without rapids; insomuch that it is navigable for batteaux to its source. From thence is a portage of 2 miles only to the Chickago, which affords a batteau navigation of 16 miles to its entrance into Lake Michigan. The Illinois, about 10 miles above its mouth, is 300 yards wide.

The Kashaskia is 100 yards wide at its entrance into the Missisipi, and preserves that breadth to the Buffalo plains, 70 miles above. So far also it is navigable for loaded batteaux, and perhaps much further. It is not rapid.

The Ohio is the most beautiful river on earth. Its current gentle, waters clear, and bosom smooth and unbroken by rocks and rapids, a single instance only excepted. It is a quarter of a mile wide at Fort Pitt; 500 yards at the mouth of the Great Kanhaway; 1 mile and 25 poles at Louisville; quarter of a mile on the Rapids, 3 or 4 miles below Louisville; half a mile where the low country begins, which is 20 miles above Green River; one and a quarter at the receipt of the Tanissee; and a mile wide at the mouth. Its length, as measured according to its meanders by Captain Hutchings, is as follows:

Image

In common Winter and Spring tides it affords 15 feet water to Louisville, 10 feet to La Tarte's Rapids, 40 miles above the mouth of the Great Kanhaway, and a sufficiency at all times for light batteaux and canoes to Fort Pitt. The Rapids are in latitude 38° 8'. The inundations of this river begin about the last of March, and subside in July. During these, a first rate man of war may be carried from Louisville to New Orleans, if the sudden turns of the river and the strength of its current will admit a safe steerage. The Rapids at Louisville descend about 30 feet in a length of a mile and a half. The bed of the river there is a solid rock, and is divided by an island into two branches, the Southern of which is about 200 yards wide, and is dry four months in the year. The bed of the Northern branch is worn into channels by the constant course of the water, and attrition of the pebble stones carried on with that, so as to be passable for batteaux through the greater part of the year. Yet it is thought that the Southern arm may be the most easily opened for constant navigation. The rise of the waters in these rapids does not exceed 10 or 12 feet. A part of this island is so high as to have been never overflowed, and to command the settlement at Louisville, which is opposite to it. The fort, however, is situated at the head of the falls. The ground on the South side rises very gradually.

The Tanissee, Cherokee or Hogohege River is 600 yards wide at its mouth, a quarter of a mile at the mouth of Holston, and 200 yards at Chotee, which is 20 miles above Holston, and 300 miles above the mouth of the Tanissee. This river crosses the Southern boundary of Virginia, 58 miles from the Mis- sisipi. Its current is moderate. It is navigable for loaded boats of any burthen to the Muscle Shoals, where the river passes through the Cumberland Mountain. These shoals are 6 or 8 miles long, passable downwards for loaded canoes, but not upwards, unless there be a swell in the river. Above these the navigation for loaded canoes and batteaux continues to the Long Island. This river has its inundations also. Above the Chickamogga towns is a whirlpool, called the Sucking Pot, which takes in trunks of trees or boats, and throws them out again half a mile below. It is avoided by keeping very close to the bank, on the South side. There are but a few miles portage between a branch of this river and the navigable waters of the River Mobile, which runs into the Gulf of Mexico.

Cumberland, or Shawanee River, intersects the boundary between Virginia and North Carolina, 67 miles from the Missisipi, and again 198 miles from the same river, a little above the entrance of Obey's River into the Cumberland. Its clear fork crosses the same boundary, about 300 miles from the Missisipi. Cumberland is a very gentle stream, navigable for loaded batteaux 800 miles, without interruption; then intervene some rapids of 15 miles in length, after which it is again navigable 70 miles upwards, which brings you within 10 miles of the Cumberland mountains. It is about 120 yards wide through its whole course, from the head of its navigation to its mouth.

The Wabash is a very beautiful river, 400 yards wide at the mouth, and 300 at St. Vincennes, which is a post 100 miles above the mouth, in a direct line. Within this space there are two small rapids, which give very little obstruction to the navigation. It is 400 yards wide at the mouth, and navigable 30 leagues upwards for canoes and small boats. From the mouth of Maple River to that of Eel River is about 80 miles in a direct line, the river continuing navigable, and from 100 to 200 yards in width. The Eel River is 150 yards wide, and affords at all times navigation for periaguas, to within 18 miles of the Miami of the lake. The Wabash, from the mouth of Eel River to Little River, a distance of 50 miles direct, is interrupted with frequent rapids and shoals, which obstruct the navigation, except in a swell. Little River affords navigation during a swell to within 3 miles of the Miami, which thence affords a similar navigation into Lake Erie, 100 miles distant in a direct line. The Wabash overflows periodically in correspondence with the Ohio, and in some places 2 leagues from its banks.

Green River is navigable for loaded batteaux at all times 50 miles upwards; but it is then interrupted by impassable rapids, above which the navigation again commences, and continues good 30 or 40 miles to the mouth of Barren River.

Kentuckey River is 90 yards wide at the mouth, and also at Boonsborough, 80 miles above. It affords a navigation for loaded batteaux 180 miles in a direct line, in the Winter tides.

The Great Miami of the Ohio is 200 yards wide at the mouth. At the Piccawee towns, 75 miles above, it is reduced to 30 yards; it is, nevertheless, navigable for loaded canoes 50 miles above these towns. The portage from its Western branch into the Miami of Lake Erie is 5 miles; that from its Eastern branch into Sandusky river is 9 miles.

Salt River is at all times navigable for loaded batteaux 70 or 80 miles. It is 80 yards wide at its mouth, and keeps that width to its fork, 25 miles above.

The Little Miami of the Ohio is 60 or 70 yards wide at its mouth, 60 miles to its source, and affords no navigation.

The Sioto is 250 yards wide at its mouth, which is in latitude 38° 22', and at the Saltlick towns, 200 miles above the mouth, it is yet 100 yards wide. To these towns it is navigable for loaded batteaux, and its Eastern branch affords navigation al- most to its source.

Great Sandy River is about 60 yards wide, and navigable 60 miles for loaded batteaux.

Guiandot is about the width of the river last mentioned, but is more rapid. It may be navigated by canoes 60 miles.

The Great Kanhaway is a river of considerable note for the fertility of its lands, and still more, as leading towards the head waters of James and Roanoke rivers. Nevertheless, it is doubtful whether its great and numerous rapids will admit a navigation, but at an expense to which it will require ages to render its inhabitants equal. The great obstacles begin at what are called the great falls, 90 miles above the mouth, below which are only 5 or 6 rapids, and these passable, with some difficulty, even at low water. From the falls to the mouth of Greenbriar is 100 miles, and thence to the lead mines 120. It is 280 yards wide at its mouth. It is said, however, that at a very moderate expense the whole current of the upper part of the Kanhaway may be turned into the South Fork of Roanoke, the Alleghaney there subsiding, and the two rivers approaching so near, that a canal of 9 miles long, and of 30 feet depth, at the deepest part, would draw the water of the Kanhaway into this branch of the Roanoke; this canal would be in Montgomery county, the court-house of which is on the top of the Alleghaney.

Hockhocking is 80 yards wide at its mouth, and yields navigation for loaded batteaux to the Press Place, 60 miles above its mouth.

The Little Kanhaway is 150 yards wide at the mouth. It yields a navigation of 10 miles only. Perhaps its Northern branch, called Junius's Creek, which interlocks with the Western of Monongahela, may one day admit a shorter passage from the latter into the Ohio.

The Muskingum is 280 yards wide at its mouth, and 200 yards at the lower Indian towns, 150 miles upwards. It is navigable for small batteaux to within one mile of a navigable part of Cayahoga River, which runs into Lake Erie.

At Fort Pitt the River Ohio loses its name, branching into the Monongahela and Alleghaney.

The Monongahela is 400 yards wide at its mouth. From thence is 12 or 15 miles to the mouth of Yohoganey, where it is 300 yards wide. Thence to Red Stone by water is 50 miles, by land 30. Then to the mouth of Cheat River by water 40 miles, by land 28, the width continuing at 300 yards, and the navigation good for boats. Thence the width is about 200 yards to the Western Fork, 50 miles higher, and the navigation frequently interrupted by rapids; which, however, with a swell of 2 or 3 feet become very passable for boats. It then admits light boats, except in dry seasons, 65 miles further to the head of Tygart's Valley, presenting only some small rapids and falls of 1 or 2 feet perpendicular, and lessening in its width to 20 yards. The Western Fork is navigable in the Winter 10 or 15 miles towards the Northern of the Little Kanhaway, and will admit a good wagon road to it. The Yohoganey is the principal branch of this river. It passes through the Laurel Mountain, about 30 miles from its mouth; is so far from 300 to 150 yards wide, and the navigation much obstructed in dry weather by rapids and shoals. In its passage through the mountain it makes very great falls, admitting no navigation for 10 miles to the Turkey Foot. Thence to the great crossing, about 20 miles, it is again navigable, except in dry seasons, and at this place is 200 yards wide. The sources of this river are divided from those of the Patowmac by the Alleghaney Mountain. From the falls, where it intersects the Laurel Mountain, to Fort Cumberland, the head of the navigation on the Patowmac, is 40 miles of very mountainous road. Wills's Creek, at the mouth of which was Fort Cumberland, is 30 or 40 yards wide, but affords no navigation as yet. Cheat River, another considerable branch of the Monongahela, is 200 yards wide at its mouth, and 100 yards at the Dunkard's settlement, 50 miles higher. It is navigable for boats, except in dry seasons. The boundary between Virginia and Pennsylvania crosses it about 3 or 4 miles above its mouth.

The Alleghaney River, with a slight swell, affords navigation for light batteaux to Venango, at the mouth of French Creek, where it is 200 yards wide; and it is practised even to Le Boeuf, from whence there is a portage of 15 miles to Presque Isle, on Lake Erie.

The country watered by the Missisipi and its Eastern branches, constitutes five-eighths of the United States, two of which five-eighths are occupied by the Ohio and its waters; the residuary streams which run into the Gulf of Mexico, the Atlantic, and the St. Laurence, water the remaining three-eighths.

Before we quit the subject of the Western waters, we will take a view of their principal connections with the Atlantic. These are three; the Hudson's river, the Patowmac, and the Missisipi itself. Down the last will pass all heavy commodities. But the navigation through the Gulf of Mexico is so dangerous, and that up the Missisipi so difficult and tedious, that it is thought probable that European merchandise will not return through that channel. It is most likely that flour, timber, and other heavy articles will be floated on rafts, which will themselves be an article for sale as well as their loading, the navigators returning by land or in light batteaux. There will therefore be a competition between the Hudson and Patowmac rivers for the residue of the commerce of all the country westward of Lake Erie, on the waters of the lakes, of the Ohio, and upper parts of the Missisipi. To go to New York, that part of the trade which comes from the lakes or their waters must first be brought into Lake Erie. Between Lake Superior and its waters and Huron are the Rapids of St. Mary, which will permit boats to pass, but not larger vessels. Lakes Huron and Michigan afford communication with Lake Erie by vessels of 8 feet draught. That part of the trade which comes from the waters of the Missisipi must pass from them through some portage into the waters of the lakes. The portage from the Illinois River into a water of Michigan is of 1 mile only. From the Wabash, Miami, Muskingum, or Alleghaney, are portages into the waters of Lake Erie, of from 1 to 15 miles. When the commodities are brought into, and have passed through Lake Erie, there is between that and Ontario an interruption by the falls of Niagara, where the portage is of 8 miles; and between Ontario and the Hudson's River are portages at the falls of Onondago, a little above Oswego, of a quarter of a mile; from Wood Creek to the Mohawks River 2 miles; at the little falls of the Mohawks River half a mile, and from Schenectady to Albany 16 miles. Besides the increase of expense occasioned by frequent change of carriage, there is an increased risk of pillage produced by committing merchandise to a greater number of hands successively. The Patowmac offers itself under the following circumstances. For the trade of the lakes and their waters westward of Lake Erie, when it shall have entered that lake, it must coast along its Southern shore, on account of the number and excellence of its harbors, the Northern, though shortest, having few harbors, and these unsafe. Having reached Cayahoga, to proceed on to New York it will have 825 miles and five portages; whereas it is but 425 miles to Alexandria, its emporium on the Patowmac, if it turns into the Cayahoga, and passes through that, Bigbeaver, Ohio, Yohoganey, (or Monongalia and Cheat,) and Patowmac, and there are but two portages; the first of which between Cayahoga and Beaver may be removed by uniting the sources of these waters, which are lakes in the neighborhood of each other, and in a champaign country; the other from the waters of Ohio to Patowmac will be from 15 to 40 miles, according to the trouble which shall betaken to approach the two navigations.

For the trade of the Ohio, or that which shall come into it from its own waters or the Missisipi, it is nearer through the Patowmac to Alexandria than to New York by 580 miles, and it is interrupted by one portage only. There is another circumstance of difference too. The lakes themselves never freeze, but the communications between them freeze, and the Hudson's River is itself shut up by the ice three months in the year; whereas the channel to the Chesapeake leads directly into a warmer climate. The Southern parts of it very rarely freeze at all, and whenever the Northern do, it is so near the sources of the rivers, that the frequent floods to which they are there liable break up the ice immediately, so that vessels may pass through the whole Winter, subject only to accidental and short delays. Add to all this, that in case of a war with our neighbors, the Anglo-Americans or the Indians, the route to New York becomes a frontier through almost its whole length, and all commerce through it ceases from that moment. But the channel to New York is already known to practice; whereas the upper waters of the Ohio and the Patowmac, and the great falls of the latter, are yet to be cleared of their fixed obstructions (1.)
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Re: Notes on the State of Virginia, by Thomas Jefferson

Postby admin » Wed Jul 29, 2015 3:54 am

QUERY III

A NOTICE OF THE BEST SEA PORTS OF THE STATE, AND HOW BIG ARE THE VESSELS THEY CAN RECEIVE?


Having no ports but our rivers and creeks, this query has been answered under the preceding one.
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Re: Notes on the State of Virginia, by Thomas Jefferson

Postby admin » Wed Jul 29, 2015 3:54 am

QUERY IV.

A NOTICE OF ITS MOUNTAINS?


For the particular geography of our mountains I must refer to Fry and Jefferson's map of Virginia, and to Evans's analysis of his map of America for a more philosophical view of them than is to be found in any other work. It is worthy of notice, that our mountains are not solitary and scattered confusedly over the face of the country, but that they commence at about 150 miles from the sea-coast, are disposed in ridges one behind another, running nearly parallel with the sea-coast, though rather approaching it as they advance Northeastwardly. To the Southwest, as the tract of country between the sea-coast and the Missisipi becomes narrower, the mountains converge into a single ridge, which, as it approaches the Gulf of Mexico, subsides into plain country, and gives rise to some of the waters of that Gulf, and particularly to a river called the Apalachicola, probably from the Apalachies, an Indian nation formerly residing on it. Hence the mountains giving rise to that river, and seen from its various parts, were called the Apalachian mountains, being in fact the end or termination only of the great ridges passing through the continent. European geographers however extended the name northwardly as far as the mountains extended; some giving it, after their separation into different ridges, to the Blue Ridge, others to the North Mountain, others to the Alleghaney, others to the Laurel Ridge, as may be seen in their different maps. But the fact I believe is, that none of these ridges were ever known by that name to the inhabitants, either native or emigrant, but as they saw them so called in European maps. In the same direction generally are the veins of lime stone, coal and other minerals hitherto discovered; and so range the falls of our great rivers. But the courses of the great rivers are at right angles with these. James and Patowmac penetrate through all the ridges of mountains eastward of the Alleghaney; that is broken by no watercourse. It is in fact the spine of the country between the Atlantic on one side, and the Missisipi and St. Laurence on the other. The passage of the Patowmac through the Blue Ridge is perhaps one of the most stupendous scenes in Nature. You stand on a very high point of land. On your right comes up the Shenandoah, having ranged along the foot of the mountain an hundred miles to seek a vent. On your left approaches the Patowmac, in quest of a passage also. In the moment of their junction they rush together against the mountain, rend it asunder, and pass off to the sea. The first glance of this scene hurries our senses into the opinion, that this earth has been created in time, that the mountains were formed first, that the rivers began to flow afterwards, that in this place particularly they have been dammed up by the Blue Ridge of mountains, and have formed an ocean which filled the whole valley; that continuing to rise they have at length broken over at this spot, and have torn the mountain down from its summit to its base. The piles of rock on each hand, but particularly on the Shenandoah, the evident marks of their disrupture and avulsion from their beds by the most powerful agents of Nature, corroborate the impression. But the distant finishing which Nature has given to the picture is of a very different character. It is a true contrast to the foreground. It is as placid and delightful as that is wild and tremendous. For the mountain being cloven asunder, she presents to your eye, through the cleft, a small catch of smooth blue horizon, at an infinite distance in the plain country, inviting you, as it were, from the riot and tumult roaring around, to pass through the breach and participate of the calm below. Here the eye ultimately composes itself; and that way too the road happens actually to lead. You cross the Patowmac above the junction, pass along its side through the base of the mountain for three miles, its terrible precipices hanging in fragments over you, and within about 20 miles reach Frederic Town, and the fine country round that. This scene is worth a voyage across the Atlantic. Yet here, as in the neighborhood of the Natural Bridge, are people who have passed their lives within half a dozen miles, and have never been to survey these monuments of a war between rivers and mountains, which must have shaken the earth itself to its centre. [i] (2)

The height of our mountains has not yet been estimated with any degree of exactness. The Alleghaney being the great ridge which divides the waters of the Atlantic from those of the Missisipi, its summit is doubtless more elevated above the ocean than that of any other mountain. But its relative height, com- pared with the base on which it stands, is not so great as that of some others, the country rising behind the successive ridges like the steps of stairs. The mountains of the Blue Ridge, and of these the Peaks of Otter, are thought to be of a greater height, measured from their base, than any others in our country, and perhaps in North America. From data, which may found a tolerable conjecture, we suppose the highest peak to be about 4,000 feet perpendicular, which is not a fifth part of the height of the mountains of South America, [ii] nor one-third of the height which would be necessary in our latitude to pre- serve ice in the open air unmelted through the year. The ridge of mountains next beyond the Blue Ridge, called by us the North Mountain, is of the greatest extent; for which reason they were named by the Indians the Endless mountains.

[To what is here said on the height of mountains, subsequent information has enabled me to furnish some additions and corrections.

General Williams, nephew of Dr. Franklin, on a journey from Richmond by the Warm and Red Springs to the Alleghaney, has estimated by barometrical observations the height of some of our ridges of mountains above the tide-water, as follows:

The Eastern base of the Blue Ridge subjacent to Rockfish Gap: 100 ft
Summit of the mountain adjacent to that Gap: 1,822 ft.
The valley constituting the Eastern basis of the Warm Spring Mountain: 943 ft.
Summit of the Warm Spring Mountain : 2,247 ft.
The Western valley of the Warm Spring Mountain, being the Eastern base of the Alleghaney: 949 ft.
Summit of the Alleghaney, 6 miles Southwest of the Red Springs: 2,760 ft.
In November, 1815, with a Ramsden's theodolite of 3-1/2 inches radius, with nonius divisions to 3', and a base of 1-1/4 mile on the low grounds of Otter River, distant 4 miles from the summits of the two peaks of Otter, I measured geometrically their heights above the water of the river at its base, and found that of the sharp or South peak: 2,946-1/2 ft.
That of the flat or North peak: 3,103-1/2 ft.


As we may with confidence say that the base of the peaks is at least as high above the tide-water at Richmond as that of the Blue Ridge at Rockfish Gap, (being 40 miles farther westward,) and their highest summit of course 3,203-1/2 feet above that tide-water, it follows that the summit of the highest peak is 343-1/2 feet higher than that of the Alleghaney, as measured by General Williams.

The highest of the White Mountains in New Hampshire, by barometrical estimate made by Captain Partridge, was found to be 4,885 feet from its base, and the highest of the Catskill mountains in New York 3,105 feet.

Two observations, with an excellent pocket sextant, gave a mean of 37° 28' 50" for the latitude of the sharp peak of Otter.

Baron Humboldt states that in latitude 37°, (which is nearly over medium parallel,) perpetual snow is no where known so low as 1,200 toises=7,671 feet above the level of the sea, and in sesquialtoral ratio nearly to the highest peak of Otter.]

A substance supposed to be Pumice, found floating on the Missisipi, has induced a conjecture, that there is a volcano on some of its waters; and as these are mostly known to their sources, except the Missoiuri, our expectations of verifying the conjecture would of course be led to the mountains which divide the waters of the Mexican Gulf from those of the South Sea; but no volcano having ever yet been known at such a distance from the sea, we must rather suppose that this floating substance has been erroneously deemed Pumice. [iii]

_______________

Notes:

i. Herodotus, 1. 7, c. 129, after stating that Thessaly is a plain country surrounded by high mountains, from which there is no outlet but the fissure through which the Peneus flows, and that according to ancient tradition it had once been an entire lake, supposes that fissure to have been made by an earthquake rending the mountain asunder.

ii. 1. Epoques, 434. Musschenbroek, § 2,312. 2. Epoques, 317.

iii. 2. Epoques, 91, 112.
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Re: Notes on the State of Virginia, by Thomas Jefferson

Postby admin » Wed Jul 29, 2015 3:55 am

QUERY V.

ITS CASCADES AND CAVERNS? [i]


The only remarkable cascade in this [ii] country, is that of the Falling Spring in Augusta. It is a water of James River, where it is called Jackson's River, rising in the Warm Spring mountains, about 20 miles Southwest of the Warm Spring, and flowing from that valley. About three quarters of a mile from its source, it falls over a rock 200 feet into the valley below. The sheet of water is broken in its breadth by the rock in two or three places, but not at all in its height. Between the sheet and rock at the bottom you may walk across dry. This cataract will bear no comparison with that of Niagara, as to the quantity of water composing it; the sheet being only 12 or 15 feet wide above, and somewhat more spread below; but it is half as high again, the latter being only 156 feet, according to the mensuration made by order of M. Vaudreuil, Governor of Canada, and 130 according to a more recent account.

In the Lime Stone country there are many caverns of very considerable extent. The most noted is called Madison's Cave, [iii] and is on the North side of the Blue Ridge, near the intersection of the Rockingham and Augusta line with the South fork of the Southern river of Shenandoah. It is in a hill of about 200 feet perpendicular height, the ascent of which on one side is so steep, that you may pitch a biscuit from its summit into the river which washes its base. The entrance of the cave is in this side about two-thirds of the way up. It extends into the earth about 300 feet, branching into subordinate caverns, sometimes ascending a little, but more generally descending, and at length terminates in two different places at basons of water of unknown extent, and which I should judge to be nearly on a level with the water of the river; however, I do not think they are formed by refluent water from that, because they are never turbid; because they do not rise and fall in correspondence with that in times of flood, or of drought, and because the water is always cool. It is probably one of the many reservoirs with which the interior parts of the earth are supposed to abound, and which yield supplies to the fountains of water, distinguished from others only by its being accessible. The vault of this cave is of solid lime stone, from 20 to 40 or 50 feet high, through which water is continually percolating. This, trickling down the sides of the cave, has incrusted them over in the form of elegant drapery; and dripping from the top of the vault generates on that, and on the base below, stalactites of a conical form, some of which have met arid formed massive columns.

Another of these caves is near the North Mountain, in the county of Frederick, on the lands of Mr. Zane. The entrance into this is on the top of an extensive ridge. You descend 30 or 40 feet, as into a well, from whence the cave then extends, nearly horizontally, 400 feet into the earth, preserving a breadth of from 20 to 50 feet, and a height of from 5 to 12 feet. After entering this cave a few feet, the mercury, which in the open air was at 50°, rose to 57° of Farenheit's thermometer, answering to 11° of Reaumur's, and it continued at that to the remotest parts of the cave. The uniform temperature of the cellars of the observatory of Paris, which are 90 feet deep, and of all subterranean cavities of any depth, where no chymical agents may be supposed to produce a factitious heat, has been found to be 10° of Reaumur, equal to 54-1/2° of Farenheit. The temperature of the cave above mentioned so nearly corresponds with this, that the difference may be ascribed to a difference of instruments.

At the Panther Gap, in the ridge which divides the waters of the Cow and the Calf Pasture, is what is called the Blowing Cave. It is in the side of a hill, is of about 100 feet diameter, and emits constantly a current of air of such force, as to keep the weeds prostrate to the distance of 20 yards before it. This current is strongest in dry frosty weather, and in long spells of rain weakest. Regular inspirations and expirations of air, by caverns and fissures, have been probably enough accounted for, by supposing them combined with intermitting fountains; as they must of course inhale air while their reservoirs are emptying themselves, and again emit it while they are filling. But a constant issue of air, only varying in its force as the weather is dryer or damper, will require a new hypothesis. [iv] There is another Blowing Cave in the Cumberland Mountain, about a mile from where it crosses the Carolina line. All we know of this is, that it is not constant, and that a fountain of water is- sues from it.

The Natural Bridge, the most sublime of Nature's works, though not comprehended under the present head, must not be pretermitted. It is on the ascent of a hill, which seems to have been cloven through its length by some great convulsion. The fissure just at the bridge is, by some admeasurements, 270 feet deep, by others only 205. It is about 45 feet wide at the bottom, and 90 feet at the top; this of course determines the length of the bridge, and its height from the water. Its breadth in the middle is about 60 feet, but more at the ends, and the thickness of the mass at the summit of the arch about 40 feet. A part of this thickness is constituted by a coat of earth, which gives growth to many large trees. The residue, with the hill on both sides, is one solid rock of lime stone. The arch approaches the semi-elliptical form; but the larger axis of the ellipsis, which would be the cord of the arch, is many times longer than the semi-axis which gives its height. Though the sides of this bridge are provided in some parts with a parapet of fixed rocks, yet few men have resolution to walk to them and look over into the abyss. You involuntarily fall on your hands and feet, creep to the parapet and peep over it. Looking down from this height about a minute gave me a violent headache. This painful sensation is relieved by a short but pleasing view of the Blue Ridge along the fissure downwards, and upwards by that of the short hills, which, with the Purgatory Mountain, is a divergence from the North Ridge; and descending then to the valley below, the sensation becomes delightful in the extreme. It is impossible for the emotions arising from the sublime to be felt beyond what they are here : so beautiful an arch, so elevated, so light, and springing as it were up to heaven, the rapture of the spectator is really indescribable. The fissure continues deep and narrow, and following the margin of the stream upwards, about three-eighths of a mile, you arrive at a lime stone cavern, less remarkable however for height and extent than those before described. Its entrance into the hill is but a few feet above the bed of the stream. This bridge is in the county of Rockbridge, to which it has given name, and affords a public and commodious passage over a valley, which cannot be crossed elsewhere for a considerable distance. The stream passing under it is called Cedar Creek. It is a water of James River, and sufficient in the dryest seasons to turn a grist mill, though its fountain is not more than two miles above. [v]

[Note. — This description was written after a lapse of several years from the time of my visit to the bridge, and under an error of recollection which requires apology, for it is from the bridge itself that the mountains are visible both ways, and not from the bottom of the fissure, as my impression then was. The statement therefore in the former editions needs the corrections here given to it. August 16, 1817.]

_______________

Notes:

i. See Map No. 1, App. iv.

ii. Bouguer mentions a cascade of two or three hundred toises height of the Bogota, a considerable river passing by Santa Fe. The cataract is vertical, and is about 15 or 16 leagues below Santa Fe. — Bouguer, xci. Buffon mentions one of 300 feet at Terni, in Italy. 1. Epoques, 470.

iii. See Map No. 2, App. iv.

iv. See Musschenbroek, § 2,604.

v. Don Ulloa mentions a break similar to this in the province of Angaraez, in South America. It is from 16 to 22 feet wide, 111 feet deep, and of 1.3 miles continuance, English measures. Its breadth at top is not sensibly greater than at bottom. But the following fact is remarkable, and will furnish some light for conjecturing the probable origin of our Natural Bridge. " Esta caxa, o cauce esta cortada en pena viva con tanta precision, que las desigualdades del un lado entrantes, corresponden a las del otro lado salientes, como si aquella altura se hubiese abierto expresamente, con sus bueltas y tortuosidades, para darle transito a los aguas por entre los dos murallones que la forman; siendo tal su igualdad, que si llegasen a juntarse se endentarian uno con otro sin dexar hueco." Not. Amer. II. § 10. Don Ulloa inclines to the opinion, that this channel has been effected by the wearing of the water which runs through it, rather than that the mountain should have been broken open by any convulsion of Nature. But if it had been worn by the running of water, would not the rocks which form the sides have been worn plane? or if, meeting in some parts with veins of harder stone, the water had left prominences on the one side, would not the same cause have sometimes, or perhaps generally, occasioned prominences on the other side also? Yet Don Ulloa tells us that on the other side there are always corresponding cavities, and that these tally with the prominences so perfectly, that were the two sides to come together, they would fit in all their indentures without leaving any void. I think that this does not resemble the effect of running water, but looks rather as if the two sides had parted asunder. The sides of the break, over which is the Natural Bridge of Virginia, consisting of a veiny rock which yields to Time, the correspondence between the salient and reentering inequalities, if it existed at all, has now disappeared. This break has the advantage of the one described by Don Ulloa in its finest circumstance; no portion in that instance having held together, during the separation of the other parts, so as to form a bridge over the abyss.

Another is mentioned by Clavigero: "Il ponte di dio. Cosi chiamano un vasto volume di terra traversato sul profondo fiume Atoyaque presso al villaggio Moleasac, cento miglia in circa da Messico verso Scirocco, sopra il quale passano comodamente icarri e le carrozze. Si puo credere, che sia stato un frammento della vicina montagna, da qualche antico tremuoto strappato." Storia del Messico, L. 1., § 3.
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Re: Notes on the State of Virginia, by Thomas Jefferson

Postby admin » Wed Jul 29, 2015 3:55 am

PART 1 OF 2

QUERY VI.

A NOTICE OF THE MINES AND OTHER SUBTERRANEOUS RICHES; ITS TREES, PLANTS, FRUITS, &C.?


I knew a single instance of gold found in this State. It was interspersed in small specks through a lump of ore, of about four pounds weight, which yielded seventeen pennyweight of gold, of extraordinary ductility. This ore was found on the North side of Rappahanock, about four miles below the falls. I never heard of any other indication of gold in its neighborhood.

On the Great Kanhaway, opposite to the mouth of Cripple Creek, and about 25 miles from our Southern boundary, in the county of Montgomery, are mines of lead. The metal is mixed, sometimes with earth, and sometimes with rock, which requires the force of gunpowder to open it; and is accompanied with a portion of silver, too small to be worth separation under any process hitherto attempted there. The proportion yielded is from 50 to 80 lb of pure metal from 100 lb of washed ore. The most common is that of 60 to the 100 lb. The veins are at some times most flattering; at others they disappear suddenly and totally. They enter the side of the hill, and proceed horizontally. Two of them are wrought at present by the public, the best of which is 100 yards under the hill. These would employ about 50 laborers to advantage. We have not, however, more than 30 generally, and these cultivate their own corn. They have produced 60 tons of lead in the year; but the general quantity is from 20 to 25 tons. The present furnace is a mile from the ore bank, and on the opposite side of the river. The ore is first wagoned to the river, a quarter of a mile, then laden on board of canoes and carried across the river, which is there about 200 yards wide, and then again taken into wagons and carried to the furnace. This mode was originally adopted, that they might avail themselves of a good situation on a creek for a pounding mill; but it would be easy to have the furnace and pounding mill on the same side of the river, which would yield water, without any dam, by a canal of about half a mile in length. From the furnace the lead is transported 130 miles along a good road, leading through the peaks of Otter to Lynch's Ferry, or Winston's, on James River, from whence it is carried by water about the same distance to Westham. This land carriage may be greatly shortened by delivering the lead on James River, above the Blue Ridge, from whence a ton weight has been brought on two canoes. The Great Kanhaway has considerable falls in the neighborhood of the mines. About seven miles below are three falls, of three or four feet perpendicular each; and three miles above is a rapid of three miles continuance, which has been compared in its descent to the great fall of James River. Yet it is the opinion that they may be laid open for useful navigation, so as to reduce very much the portage between the Kanhaway and James River.

A valuable lead mine is said to have been lately discovered in Cumberland, below the mouth of Red River. The greatest, however, known in the Western country are on the Missisipi, extending from the mouth of Rock River, 150 miles upwards. These are not wrought, the lead used in that country being from the banks on the Spanish side of the Missisipi, opposite to Kaskaskia.

A mine of copper was once opened in the county of Amherst, on the North side of James River, and another in the opposite country, on the South side. However, either from bad management or the poverty of the veins, they were discontinued. We are told of a rich mine of native copper on the Ouabache, below the upper Wiaw.

The mines of iron worked at present are Callaway's, Ross's, and Ballendine's, on the South side of James River; Old's on the North side, in Albemarle; Millar's, in Augusta, and Zane's, in Frederick. These two last are in the valley between the Blue Ridge and North Mountain. Callaway's, Ross's, Millar's, and Zane's, make about 150 tons of bar iron each in the year. Ross's makes also about 1,600 tons of pig iron annually; Ballendine's 1,000; Callaway's, Millar's, and Zane's, about 600 each. Besides these, a forge of Mr. Hunter's, at Fredericksburgh, makes about 300 tons a year of bar iron, from pigs imported from Maryland; and Taylor's forge, on Neapsco of Patowmac, works in the same way, but to what extent I am not informed. The indications of iron in other places are numerous, and dispersed through all the middle country. The toughness of the cast iron of Ross's and Zane's furnaces is very remarkable. Pots and other utensils, cast thinner than usual, of this iron, may be safely thrown into or out of the wagons in which they are transported. Salt pans made of the same, and no longer wanted for that purpose, cannot be broken up, in order to be melted again, unless previously drilled in many parts.

In the Western country we are told of iron mines between the Muskingum and Ohio; of others on Kentuckey, between the Cumberland and Barren rivers, between Cumberland and Tanissee, on Reedy Creek, near the Long Island, and on Chestnut Creek, a branch of the Great Kanhaway, near where it crosses the Carolina line. What are called the iron banks, on the Missisipi, are believed, by a good judge, to have no iron in them. In general, from what is hitherto known of that country, it seems to want iron.

Considerable quantities of black lead are taken occasionally for use from Winterham, in the county of Amelia. I am not able, however, to give a particular state of the mine. There is no work established at it, those who want, going and procuring it for themselves.

The country on James River, from 15 to 20 miles above Richmond, and for several miles northward and southward, is replete with mineral coal of a very excellent quality. Being in the hands of many proprietors, pits have been opened, and before the interruption of our commerce, were worked to an extent equal to the demand.

In the Western country coal is known to be in so many places, as to have induced an opinion that the whole tract between the Laurel Mountain, Missisipi, and Ohio, yields coal. It is also known in many places on the North side of the Ohio. The coal at Pittsburg is of very superior quality. A bed of it at that place has been afire since the year 1765. Another coal hill on the Pike Run of Monongahela has been afire ten years; yet it has burnt away about twenty yards only.

I have known one instance of an Emerald found in this country. Amethysts have been frequent, and chrystals common; yet not in such numbers any of them as to be worth seeking.

There is very good marble, and in very great abundance, on James River, at the mouth of Rockfish. The samples I have seen, were some of them of a white as pure as one might expect to find on the surface of the earth; but most of them were variegated with red, blue and purple. None of it has been ever worked. It forms a very large precipice, which hangs over a navigable part of the river. It is said there is marble at Kentuckey.

But one vein of lime stone is known below the Blue Ridge. Its first appearance in our country is in Prince William, two miles below the Pignut Ridge of mountains; thence it passes on nearly parallel with that, and crosses the Rivanna about five miles below it, where it is called the Southwest ridge. It then crosses Hardware, above the mouth of Hudson's Creek, James River at the mouth of Rockfish, at the marble quarry before spoken of, probably runs up that river to where it appears again at Ross's iron works, and so passes off southwestwardly by Flat Creek of Otter River. It is never more than one hundred yards wide. From the Blue Ridge westwardly, the whole country seems to be founded on a rock of lime stone, besides infinite quantities on the surface, both loose and fixed. This is cut into beds, which range, as the mountains and sea-coast do, from Southwest to Northeast, the lamina of each bed declining from the horizon towards a parallelism with the axis of the earth. Being struck with this observation, I made, with a quadrant, a great number of trials on the angles of their declination, and found them to vary from 22° to 60°, but averaging all my trials, the result was within one-third of a degree of the elevation of the pole or latitude of the place, and much the greatest part of them taken separately were little different from that, by which it appears that these laminae are in the main parallel with the axis of the earth. In some instances, indeed, I found them perpendicular, and even reclining the other way; but these were extremely rare, and always attended with signs of convulsion, or other circumstances of singularity, which admitted a possibility of removal from their original position. These trials were made between Madison's Cave and the Patowmac. We hear of lime stone on the Missisipi and Ohio, and in all the mountainous country between the Eastern and Western waters, not on the mountains themselves, but occupying the valleys between them.

Adjacent to the vein of lime stone first mentioned, or at least to some parts of it, is a vein of slate of greater breadth than that of the lime stone, sometimes mixed with it, some times a small distance apart from it. The neighborhood of these veins of lime stone, and slate, and of lime stone and schist, between the North Mountain and Blue Ridge, coincides with the following observations of Bouguer, while in Peru: "Le marbre est tres commun sur le bord de plusieurs de ces rivieres: on y voit aussi des rochers d' ardoise & j'ai souvent eu occasion d'y observer la grande affinity qu 'il y a entre ces deux sortes de pierre. J'avois deja fait cette remarque dans la Cordeliere. Les rochers de marbre et d' ardoise s 'y touchent souvent, et j 'en ai vu qui etoit ardoise par une extremite et marbre parfait par l'autre. Toutes les fois qui'il survient un nouveau suc pierreux analogue a l' ardoise et qui en unit les feuilles, il rend tout le rocher plus compacte et plus dur; le rocher cesse d' etre de l' ardoise pour devenir du marbre. Une pierre egalement distribuee par feuilles qu'on nomme schite, est aussi sujette a cette transformation. Quelquefois ce ne sont pas simplement ses feuilles qui se soudent entr' elles iin quartier de cette pierre se joint comme au hazard avec un autre. Si le tout est ensuite expose a l' action du gravier & des cailloux roules par un eau courante, et qu 'il recoive une sorte d' arrondissement qui le rende a peu pres cylindrique, il prend toutes les apparences d' un tronc d' arbre; et il est meme quelquefois tres difficile de ne s 'y pas tromper. Je fus tres fache de ne pouvoir porter avec moi une de ces-especes de tronc que je trouvai dans une ravine entre Guanacas et la Plata, au pied d'une colline nommee la Subida del Frayle. C 'etoit un morceau de marbre qui avoit 20 pouces de longueur sur 17 on 18 de diametre; on distinguoit comme les fibres du bois, la surface presente des noeuds de diverses formes; le contour meme du tronc etoit egalement propre a en imposer. Il y avoit un enfoncement d' un cote qui formoit un angle rentrant, et une saillie du cote oppose. Je ne scavois qu 'en penser, de meme que les personnes qui m 'accompagnoient. Je ne reussis enfin a me decider, qu 'en jettant les yeux sur d 'autres quartiers de schite qui etoient aupres, qui commencoient a prendre les memes apparences, mais qui n' etoient pas encore dans un etat a pouvoir jetter dans l' erreur, et qui au contraire m' eclairerent sur la nature du morceau de marbre. On pretend qu 'entre les different bois c 'est le gayac qui se petrifie le plus aisement. On m' assuroit que je verrois audessou de Mompox une croix dont tout le haut de l' arbre etoit encore de ce bois pendant que le bas etoit reellement de la pierre a fusil. Plusieurs personnes m' affirmerent en avoir tire du feu. Lorsque je passai dans cet endroit on me confirma la meme chose; mais on m' ajonta qu' une crue extraordinaire avoit fait tomber la croix dans la riviere, il y avoit 6 a 7 ans. Page xciii.

Near the Eastern foot of the North Mountain are immense bodies of schist, containing impressions of shells in a variety of forms. I have received petrified shells of very different kinds from the first sources of the Kentuckey, which bear no resemblance to any I have ever seen on the tide-waters. It is said [i] that shells are found in the Andes, in South America, 15,000 feet above the level of the ocean. This is considered by many, both of the learned and unlearned, as a proof of an universal deluge. To the many considerations opposing this opinion, the following may be added. The atmosphere, and all its contents, whether of water, air, or other matters, gravitate to the earth; that is to say, they have weight. Experience tells us that the weight of all these together never exceeds that of a column of mercury of 31 inches height, which is equal to one of rain water of 35 feet high. If the whole contents of the atmosphere then were water, instead of what they are, it would cover the globe but 35 feet deep; but as these waters as they fell would run into the seas, the superficial measure of which is to that of the dry parts of the globe as two to one, the seas would be raised only 52-1/2 feet above their present level, and of course would overflow the lands to that height only. [ii] In Virginia this would be a very small proportion even of the champaign country, the banks of our tide-waters being frequently, if not generally, of a greater height. Deluges beyond this extent then, as for instance, to the North Mountain or to Kentuckey, seem out of the laws of Nature. But within it they may have taken place to a greater or less degree, in proportion to the combination of natural causes which may be supposed to have produced them. History renders probable some instances of a partial deluge in the country lying round the Mediterranean sea. It has been often supposed, [iii] and is not unlikely, that that sea was once a lake. While such, let us admit an extraordinary collection of the waters of the atmosphere from the other parts of the globe to have been discharged over that and the countries whose waters run into it. Or without supposing it a lake, admit such an extraordinary collection of the waters of the atmosphere, and an influx of waters from the Atlantic Ocean, forced by long continued Western winds. That lake, or that sea, may thus have been so raised as to overflow the low lands adjacent to it, as those of Egypt and Armenia, which, according to a tradition of the Egyptians and Hebrews, were overflowed about 2,300 years before the Christian area: those of Attica, said to have been overflowed in the time of Ogyges, about 500 years later; and those of Thessaly, in the time of Deucalion, still 300 years posterior. [iv] But such deluges as these will not account for the shells found in the higher lands. A second opinion has been entertained, which is, that in times anterior to the records, either of history or tradition, the bed of the ocean, the principal residence of the shelled tribe, has, by some great convulsion of Nature, been heaved to the heights at which we now find shells and other remains of marine animals. The favorers of this opinion do well to suppose the great events on which it rests to have taken place beyond all the eras of history; for within these certainly none such are to be found; and we may venture to say further, that no fact has taken place, either in our own days, or in the thousands of years recorded in history, which proves the existence of any natural agents, within or without the bowels of the earth, of force sufficient to heave, to the height of 15,000 feet, such masses as the Andes. The difference between the power necessary to produce such an effect, and that which shuffled together the different parts of Calabria in our days, is so immense, that from the existence of the latter, we are not authorized to infer that of the former.

M. de Voltaire has suggested a third solution of this difficulty. (Quest. Encycl. Coquilles.) He cites an instance in Touraine, where, in the space of 80 years, a particular spot of earth had been twice metamorphosed into soft stone, which had become hard when employed in building. In this stone shells of various kinds were produced, discoverable at first only with the microscope, but afterwards growing with the stone. From this fact, I suppose he would have us infer, that besides the usual process for generating shells by the elaboration of earth and water in animal vessels. Nature may have provided an equivalent operation by passing the same materials through the pores of calcareous earths and stones; as we see calcareous drop stones generating every day by the percolation of water through lime stone, and new marble forming in the quarries from which the old has been taken out; and it might be asked whether it is more difficult for Nature to shoot the calcareous juice into the form of a shell, than other juices into the forms of chrystals, plants, animals, according to the construction of the vessels through which they pass? There is a wonder some- where. Is it greatest on this branch of the dilemma; on that which supposes the existence of a power, of which we have no evidence in any other case; or on the first, which requires us to believe the creation of a body of water, and its subsequent annihilation? The establishment of the instance cited by M. de Voltaire, of the growth of shells unattached to animal bodies, would have been that of his theory. But he has not established it. He has not even left it on ground so respectable as to have rendered it an object of enquiry to the literati of his own country. Abandoning this fact, therefore, the three hypotheses are equally unsatisfactory; and we must be contented to acknowledge that this great phenomenon is as yet unsolved. Ignorance is preferable to error; and he is less remote from the truth who believes nothing, than he who believes what is wrong.

There is great abundance (more especially when you approach the mountains) of stone, white, blue, brown, &c., fit for the chisel, good mill stone, such also as stands the fire, and slate stone. We are told of flint, fit for gun flints, on the Meherrin in Brunswic, on the Missisipi between the mouth of Ohio and Kaskaskia, and on others of the Western waters. Isinglass or mica is in several places; load stone also, and an asbestos, of a ligneous texture, is sometimes to be met with.

Marl abounds generally. A clay, of which, like the sturbridge in England, bricks are made, which will resist long the violent action of fire, has been found on Tuckahoe Creek of James River, and no doubt will be found in other places. Chalk is said to be in, Botetourt and Bedford. In the latter county is some earth, believed to be gypseous. Ochres are found in various parts.

In the lime stone country are many caves, the earthy floors of which are impregnated with nitre. On Rich Creek, a branch of the Great Kanhaway, about 60 miles below the lead mines, is a very large one, about 20 yards wide, and entering a hill a quarter or half a mile. The vault is of rock, from 9 to 15 or 20 feet above the floor. A Mr. Lynch, who gives me this ac- count, undertook to extract the nitre. Besides a coat of the salt which had formed on the vault and floor, he found the earth highly impregnated to the depth of seven feet in some places, and generally of three, every bushel yielding on an average three pounds of nitre. Mr. Lynch having made about 1,000 ft) of the salt from it, consigned it to some others, who have since made 10,000 ft). They have done this by pursuing the cave into the hill, never trying a second time the earth they have once exhausted, to see how far or soon it receives another impregnation. At least fifty of these caves are worked on the Greenbriar, There are many of them known on Cumberland River.

The country westward of the Alleghaney abounds with springs of common salt. The most remarkable we have heard of are at Bullet's Lick, the Big Bones, the Blue Licks, and on the North Fork of Holston. The area of Bullet's Lick is of many acres. Digging the earth to the depth of three feet, the water begins to boil up, and the deeper you go, and the dryer the weather, the stronger is the brine. A thousand gallons of water yield from a bushel to a bushel and a half of salt, which is about 80 lb of water to 1 lb of salt; but of sea water 25 lb yield 1 lb of salt. So that sea water is more than three times as strong as that of these springs. A Salt Spring has been lately discovered at the Turkey Foot on Yohogany, by which river it is overflowed, except at very low water. Its merit is not yet known. Duning's Lick is also as yet untried, but it is supposed to be the best on this side the Ohio. The Salt Springs on the margin of the Onondago Lake are said to give a saline taste to the waters of the lake.

There are several Medicinal Springs, some of which are indubitably efficacious, while others seem to owe their reputation as much to fancy and change of air and regimen as to their real virtues. None of them having undergone a chemical analysis in skilful hands, nor been so far the subject of observations as to have produced a reduction into classes of the disorders which they relieve, it is in my power to give little more than an enumeration of them.

The most efficacious of these are two springs in Augusta, near the first sources of James River, where it is called Jackson's River. They rise near the foot of the ridge of mountains, generally called the Warm Spring Mountain, but in the maps Jackson's mountains. The one is distinguished by the name of the Warm Spring, and the other of the Hot Spring. The Warm Spring issues with a very bold stream, sufficient to work a grist mill, and to keep the waters of its bason, which is 30 feet in diameter, at the vital warmth, viz: 96° of Farenheit's thermometer. The matter with which these waters is allied is very volatile; its smell indicates it to be sulphureous, as also does the circumstance of its turning silver black. They relieve rheumatisms. Other complaints also of very different natures have been removed or lessened by them. It rains here four or five days in every week.

The Hot Spring is about six miles from the Warm, is much smaller, and has been so hot as to have boiled an egg. Some believe its degree of heat to be lessened. It raises the mercury in Farenheit's thermometer to 112 degrees, which is fever heat. It sometimes relieves where the Warm Spring fails. A fountain of common water, issuing within a few inches of its margin, gives it a singular appearance. Comparing the temperature of these with that of the Hot Springs of Kamschatka, of which Krachininnikow gives an account, the difference is very great, the latter raising the mercury to 200°, which is within 12° of boiling water. These springs are very much resorted to in spite of a total want of accommodation for the sick. Their waters are strongest in the hottest months, which occasions their being visited in July and August principally.

The Sweet Springs are in the county of Botetourt, at the Eastern foot of the Alleghaney, about 42 miles from the Warm Springs. They are still less known. Having been found to relieve cases in which the others had been ineffectually tried, it is probable their composition is different. They are different also in their temperature, being as cold as common water, which is not mentioned however as a proof of a distinct impregnation. This is among the first sources of James River.

On Patowmac River, in Berkeley county, above the North Mountain, are Medicinal Springs, much more frequented than those of Augusta. Their powers, however, are less, the waters weakly mineralized, and scarcely warm. They are more visited, because situated in a fertile, plentiful, and populous country, better provided with accommodations, always safe from the Indians, and nearest to the more populous States.

In Louisa county, on the head waters of the South Anna branch of York River, are springs of some medicinal virtue. They are not much used however. There is a weak chalybeate at Richmond, and many others in various parts of the country, which are of too little worth, or too little note, to be enumerated after those before mentioned.

We are told of a Sulphur Spring on Howard's Creek of Greenbriar, and another at Boonsborough, on Kentuckey.

In the low grounds of the Great Kanhaway, 7 miles above the mouth of Elk River, and 67 above that of the Kanhaway itself, is a hole in the earth of the capacity of 30 or 40 gallons, from which issues constantly a gaseous stream so strong as to give to the sand about its orifice the motion which it has in a boiling spring. On presenting a lighted candle or torch within 18 inches of the hole, it flames up in a column of 18 inches diameter, and four or five feet height, which sometimes burns out within 20 minutes, and at other times has been known to continue three days, and then has been left still burning. [v] The flame is unsteady, of the density of that of burning spirits, and smells like burning pit coal. Water some- times collects in the bason, which is remarkably cold, and is kept in ebullition by the gas escaping through it. If the gas be fired in that state, the water soon becomes so warm that the hand cannot bear it, and evaporates wholly in a short time. This gaseous fluid is probably inflammable air, the hydrogene of the new chemistry, which we know will kindle on mixing with the oxygenous portion of the atmospheric air, and the application of flame. It may be produced by a decomposition of water or of pyrites, within the body of the hill. The circumjacent lands are the property of General Washington and of General Lewis.

There is a similar one on Sandy River, the flame of which is a column of about 12 inches diameter, and 3 feet high. General Clarke, who informs me of it, kindled the vapor, staid about an hour, and left it burning.

The mention of uncommon springs leads me to that of Syphon fountains. There is one of these near the intersection of the Lord Fairfax's boundary with the North Mountain, not far from Brock's Gap, on the stream of which is a grist mill, which grinds two bushels of grain at every flood of the spring. An- other, near the Cow Pasture River, a mile and a half below its confluence with the Bull Pasture River, and 16 or 17 miles from the Hot Springs, which intermits once in every twelve hours. One also near the mouth of the North Holston.

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We are told that during a great storm on the 25th of December, 1798, the Syphon Fountain, near the mouth of the North Holston, ceased, and a spring broke out about 100 feet higher up the hill. [vi] Syphon fountains have been explained by supposing the duct which leads from the reservoir to the surface of the earth to be in the form of a syphon, a, h, c, where it is evident that till the water rises in the reservoir to d, the level of the highest point of the syphon, it cannot flow through the duct, and it is known that when once it begins to flow it will draw off the water of the reservoir to the orifice a, of the syphon. If the duct be larger than the supply of the reservoir, possibly the force of the waters and loosening of the earth by them, during the storm above mentioned, may have opened a more direct duct as from e to f, horizontally or declining, which issued higher up the hill than the one fed by the syphon. In that case it becomes a common spring. Should this duct be again closed or diminished by any new accident, the syphon may begin to play again, and both springs be kept in action from the same reservoir.

After these may be mentioned the Natural Well, on the lands of a Mr. Lewis in Frederick county. It is somewhat larger than a common well; the water rises in it as near the surface of the earth as in the neighboring artificial wells, and is of a depth as yet unknown. It is said there is a current in it tending sensibly downwards. If this be true, it probably feeds some fountain, of which it is the natural reservoir, distinguished from others like that of Madison's Cave, by being accessible. It is used with a bucket and windlass, as an ordinary well.

A complete catalogue of the trees, plants, fruits, &c., is probably not desired. I will sketch out those which would principally attract notice, as being — 1, Medicinal; 2, Esculent; 3, Ornamental; or, 4, Useful for fabrication: adding the Linnaean to the popular names, as the latter might not convey precise information to a foreigner. I shall confine myself too to native plants:

1. Senna — Cassia ligustrina. Arsmart — Polygonum Sagittatum. Clivers, or goose grass — Galium spurium. Lobelia, of several species. Palma Christi — Ricinus. James Town weed (3) — Datura Stramonium. Mallow — Malva rotundifolia. Syrian mallow — Hibiscus moschentos. Hibiscus virginicus. Indian mallow — Sida rhombifolia, Sida abutilon. Virginia Marshmallow — Napaea hermaphrodita, Napsea dioica. Indian physic — Spiraea trifoliata, Euphorbia Ipecacuanhse. Pleurisy root — Asclepias decumbens. Virginia snake root — Aristolochia serpentaria. Black snake root — Actaea racemosa. Seneca rattlesnake root — Polygala Senega. Valerian — Valeriana locusta radiata. Gentiana, Saponaria, Villosa and Centaurium. Ginseng — Panax quinquefolium. Angelica — Angelica sylvestris. Cassava — Jatropha urens.

2. Tuckahoe — Lycoperdon tuber. Jerusalem artichoke — Helianthus tuberosus. Long potatoes — Convolvulas batatas. Granadillas, Maycocks, Maracocks — Passiflora incarnata. Panic — Panicum, of many species. Indian millet — Holcus laxus, Holcus striosus. Wild oat — Zizania aquatica. Wild pea — Dolichos of Clayton. Lupine — Lupinus perennis. Wild hop — Humulus lupulus. Wild cherry — Prunus Virginiana. Cherokee plum — Prunus sylvestris fructu majori. Clayton. Wild plum — Prunus sylvestris fructu minori. Clayton. Wild crab apple — Pyrus coronaria. Red mulberry — Morus rubra. Persimmon — Diospy- ros Virginiana. Sugar maple — Acer saccharinum. Scaly bark hiccory — Juglans alba cortice squamoso. Clayton. Common hiccory — Juglans alba, fructu minore rancido. Clayton. Paccan, or Illinois nut. Not described by Linnaeus Millar, or Clayton. [Were I to venture to describe this, speaking of the fruit from memory, and of the leaf from plants of two years growth, I should specify it as the Juglans alba, foliolis lanceolatis, acuminatis, serratis, tomentosis, fructu minore, ovato, compresso, vix insculpto dulci putamine, tenerrimo. It grows on the Illinois, Wabash, Ohio, and Missisipi. It is spoken of by Don Ulloa under the name of Pacanos, in his Noticias Americanas — Entret. 6.] Black walnut — Juglans nigra. White walnut — Juglans alba. Chesnut — Fagus castanea. Chinquapin — Fagus pumila. Hazlenut — Corylus avellana. Grapes — Vitis, various kinds, though only three described by Clayton. Scarlet Strawberries — Fragaria Virginiana of Millar. Whortleberries — Vaccinium uliginosum? Wild gooseberries — Ribes grossularia. Cranberries — Vaccinium oxycoccos. Black raspberries — Rubus occidentalis. Blackberries — Rubus fruticosus. Dewberries — Rubus csesius. Cloudberries — Robus chamaemorus.

3. Plane tree — Platanus occidentalis. Poplar — Liriodendron tulipifera, Populus lieterophylla. Black poplar — Populus nigra. Aspen — Populus tremula. Linden, or lime — Tilia Americana. Red flowering maple — Acer rubrum. Horsechesnut, or Buck's eye — Aesculus pavia. Catalpa — Bignonia catalpa. Umbrella — Magnolia tripetala. Swamp laurel — Magnolia glauca. Cucumber tree — Magnolia acuminata. Portugal bay — Laurus indica. Red bay — Laurus borbonia. Dwarf rose bay — Rhododendron maximum. Laurel of the Western country. Qu. species? Wild pimento — Laurus benzoin. Sassafras — Laurus sassafras. Locust — Robinia pseudo acacia. Honey locust — Gleditsia. I. ß. Dogwood — Cornus florida. Fringe, or snow drop tree — Chionanthus Virginica. Barberry — Berberis vulgaris. Red bud, or Judas tree — Cercis Canadensis. Holly — Ilex aquifolium. Cockspur hawthorn — Crataegus coccinea. Spindle tree — Euonymus Europoeus. Evergreen spindle tree — Euonymus Americanus. Itea Virginica. Elder — Sambucus nigra. Papaw — Annona triloba. Candleberry myrtle — Myrica cerifera. Dwarf laurel — Kalmia angustifolia, Kalmia latifolia, called ivy with us. Ivy — Hedera quinquefolia. Trumpet honeysuckle — Lonicera sempervirens. Upright honeysuckle — Azalea nudiflora, Azalea viscosa. Yellow jasmine — Bignonia sempervirens. Calycanthus floridus. American aloe — Agave Virginica. Sumach — Rhus. Qu. species? Poke — Phytolacca decandra. Long moss — Tillandsia Usneoides.

4. Reed — Arundo phragmitis. Virginia hemp — Acnida cannabina. Flax — Linum Virginianum. Black, or pitch pine — Pinus tseda. White pine — Pinus strobus. Yellow pine — Pinus Virginica. Spruce pine — Pinus foliis singularibus. Clayton. Hemlock spruce fir — Pinus Canadensis. Arbor vitse — Thuya occidentalis. Juniper — Juniperus virginica (called cedar with us.) Cypress — Cupressus disticha. White cedar — Cupressus Thyoides. Black oak — Quercus nigra. White oak — Quercus alba. Red oak — Quercus rubra. Willow oak — Quercus phellos. Chesnut oak — Quercus prinus. Black jack oak — Quercus aquatica. Clayton. Query? Ground oak — Quercus pumila. Clayton. Live oak — Quercus Virginiana. Millar. Black birch — Betula nigra. White birch — Betula alba. Beach — Fagus sylvatica. Ash — Fraxinus Americana, Fraxinus Novae Angliae. Millar. Elm — Ulmus Americana. "Willow — Salix. Query, species? Fluvialis. Bartr. 393. Sweet Gum — Liquidambar styraciflua.

The following were found in Virginia when first visited by the English; but it is not said whether of spontaneous growth, or by cultivation only. Most probably they were natives of more Southern climates, and handed along the continent from one nation to another of the savages:

Tobacco — Nicotiana. [vii] Maize — Zea mays, [viii] Round potatoes — Solanum tuberosum. Pumpkins — Cucurbita pepo. Cymlings — Cucurbita verrucosa. Squashes — Cucurbita melopepo. There is an infinitude of other plants and flowers, for an enumeration and scientific description of which I must refer to the Flora Virginica of our great botanist, Dr. Clayton, published by Gronovius at Leyden, in 1762. This accurate observer was a native and resident of this State, passed a long life in exploring and describing its plants, and is supposed to have enlarged the botanical catalogue as much as almost any man who has lived.

Besides these plants, which are native, our farms produce wheat, rye, barley, oats, buckwheat, and broom corn. The climate suits rice well enough wherever the lands do. Tobacco, hemp, flax, and cotton, are staple commodities. Indico yields two cuttings. The silk worm is a native, and the mulberry, proper for its food, grows kindly.

We cultivate also potatoes, both the long and the round, turnips, carrots, parsneps, pumpkins, and ground nuts, (Arachis.) Our grasses are Lucerne, St. Foin, Burnet, Timothy, ray, and orchard grass; red, white, and yellow clover; greensward, blue grass, and crab grass.

The gardens yield musk melons, water melons, tomatoes, ochre, pomegranates, figs, and the esculent plants of Europe.

The orchards produce apples, pears, cherries, quinces, peaches, nectarines, apricots, almonds, and plums.

Our quadrupeds have been mostly described by Linnaeus and Mons. de Buffon. Of these the mammoth, or big buffalo, as called by the Indians, must certainly have been the largest. Their tradition is, that he was carnivorous, and still exists in the Northern parts of America. A delegation of warriors from the Delaware tribe having visited the Governor of Virginia, during the present revolution, on matters of business, after these had been discussed and settled in council, the Governor asked them some questions relative to their country, and, among others, what they knew or had heard of the animal whose bones were found at the Saltlicks, on the Ohio.

Their chief speaker immediately put himself into an attitude of oratory, and with a pomp suited to what he conceived the elevation of his subject, informed him that it was a tradition handed down from their fathers: "That in ancient times a herd of these tremendous animals came to the Big Bone Licks, and began an universal destruction of the bear, deer, elks, buffaloes, and other animals, which had been created for the use of the Indians; that the Great Man above, looking down and seeing this, was so enraged that he seized his lightning, descended on the earth, seated himself on a neighboring mountain, on a rock, of which his seat and the print of his feet are still to be seen, and hurled his bolts among them till the whole were slaughtered, except the big bull, who, presenting his forehead to the shafts, shook them off as they fell; but missing one at length, it wounded him in the side; whereon, springing round, he bounded over the Ohio, over the Wabash, the Illinois, and finally over the great lakes, where he is living at this day." It is well known that on the Ohio, and in many parts of America further North, tusks, grinders, and skeletons of unparalleled magnitude, are found in great numbers, some lying on the surface of the earth, and some a little below it. A Mr. Stanley, taken prisoner by the Indians near the mouth of the Tanissee, relates that, after being transferred through several tribes, from one to another, he was at length carried over the mountains West of the Missouri to a river which runs westwardly; that these bones abounded there; and that the natives described to him the animal to which they belonged as still existing in the Northern parts of their country; from which description he judged it to be an elephant. Bones of the same kind have been lately found some feet below the surface of the earth, in salines opened on the North Holston, a branch of the Tanissee, about the latitude of 36-1/2° North. From the accounts published in Europe, I suppose it to be decided that these are of the same kind with those found in Siberia. [ix] Instances are mentioned of like animal remains found in the more Southern climates of both hemispheres; [x] hut they are either so loosely mentioned as to leave a doubt of the fact, so inaccurately described as not to authorize the classing them with the great Northern bones, or so rare as to found a suspicion that they have been carried] thither as curiosities from more Northern regions. So that on the whole there seem to be no certain vestiges of the existence of this animal further South than the salines last mentioned, [xi] It is remarkable that the tusks and skeletons have been ascribed by the naturalists of Europe to the elephant, while the grinders have been given to the hippopotamus, or river horse. [xii] Yet it is acknowledged that the tusks and skeletons are much larger than those of the elephant, and the grinders many times greater than those of the hippopotamus, and essentially different in form. Wherever these grinders are found, there also we find the tusks and skeleton; but no skeleton of the hippopotamus nor grinders of the elephant. It will not be said that the hippopotamus and elephant came always to the same spot, the former to deposit his grinders, and the latter his tusks and skeleton. For what became of the parts not deposited there? We must agree then that these remains belong to each other, that they are of one and the same animal, that this was not a hippopotamus, because the hippopotamus had no tusks nor such a frame, and because the grinders differ in their size as well as in the number and form of their points. That it was not an elephant, I think ascertained by proofs equally decisive. I will not avail myself of the authority of the celebrated [xiii] anatomist, who, from an examination of the form and structure of the tusks, has declared they were essentially different from those of the elephant, because another [xiv] anatomist, equally celebrated, has declared, on a like examination, that they are precisely the same. Between two such authorities I will suppose this circumstance equivocal. But, 1, The skeleton of the mammoth (for so the incognitum has been called) bespeaks an animal of six times the cubic volume of the elephant, as Mons. de Buffon has admitted. [xv] 2, The grinders are five times as large, are square, and the grinding surface studded with four or five rows of blunt points : whereas those of the elephant are broad and thin, and their grinding surface flat. [xvi] 3, I have never heard an instance, and suppose there has been none, of the grinder of an elephant being found in America. 4, From the known temperature and constitution of the elephant he could never have existed in those regions where the remains of the mammoth have been found. The elephant is a native only of the torrid zone and its vicinities: if with the assistance of warm apartments and warm clothing he has been preserved in life in the temperate climates of Europe, it has only been for a small portion of what would have been his natural period, and no instance of his multiplication in them has ever been known. But no bones of the mammoth, as I have before observed, have been ever found further South than the salines of the Holston, and they have been found as far North as the Arctic circle. Those, therefore, who are of opinion that the elephant and mammoth are the same, must believe, 1, That the elephant known to us can exist and multiply in the frozen zone; or, 2, That an internal fire may once have warmed those regions, and since abandoned them, of which, however, the globe exhibits no unequivocal indications; or, 3, That the obliquity of the ecliptic, when these elephants lived, was so great as to include within the tropics all those regions in which the bones are found; the tropics being as is before observed, the natural limits of habitation for the elephant. M. de Buffon considers the existence of elephant bones in Northern regions, where the animal itself is no longer found, as one of the leading facts which support his theory, that the earth was once in a liquid state, rendered so by the action of fire, that the process of cooling began at its poles, and proceeded gradually towards the torrid zone, that with this progress the animals of warm temperature retired towards the equator, and that in the present state of that progress the globe remains of sufficient warmth, for the elephant for instance, in the tropical regions, only to which therefore they have retired, as their last asylum, and where they must become extinct when the degree of warmth shall be reduced below that adapted to their constitution. How does it happen then that no elephants exist at present in the tropical regions of America, to which those of the Ohio must have retired, according to this theory? But if it be admitted that this obliquity has really decreased, and we adopt the highest rate of decrease yet pretended, that is, of one minute in a century, to transfer the Northern tropic to the Arctic circle, would carry the existence of these supposed elephants 250,000 years back; a period far beyond our conception of the duration of animal bones left exposed to the open air, as [these are in many instances. Besides, though these regions would then be supposed within the tropics, yet their winters would have been too severe for the sensibility of the elephant. They would have had too but one day and one night in the year, a circumstance to which we have no reason to suppose the nature of the elephant fitted. However, it has been demonstrated, that if a variation of obliquity in the ecliptic takes place at all, it is vibratory, and never exceeds the limits of 9 degrees, which is not sufficient to bring these bones within the tropics. One of these hypotheses, or some other equally voluntary and inadmissible to cautious philosophy, must be adopted to support the opinion that these are the bones of the elephant. For my own part, I find it easier to believe that an animal may have existed, resembling the elephant in his tusks and general anatomy, while his nature was in other respects extremely different. From the 30th degree of South latitude to the 30th of North, are nearly the limits which Nature has fixed for the existence and multiplication of the elephant known to us. Proceeding thence northwardly to 36-1/2 degrees, we enter those assigned to the mammoth. The further we advance North, the more their vestiges multiply as far as the earth has been explored in that direction; and it is as probable as otherwise, that this progression continues to the pole itself, if land extends so far. The centre of the frozen zone then may be the acme of their vigor, as that of the torrid is of the elephant. Thus Nature seems to have drawn a belt of separation between these two tremendous animals, whose breadth, indeed, is not precisely known, though at present we may suppose it about 6-1/2 degrees of latitude; to have assigned to the elephant the regions South of these confines, and those North to the mammoth, founding the constitution of the one in her extreme of heat, and that of the other in the extreme of cold. When the Creator has therefore separated their nature as far as the extent of the scale of animal life allowed to this planet would permit, it seems perverse to declare it the same, from a partial resemblance of their tusks and bones. But to whatever animal we ascribe these remains, it is certain such a one has existed in America, and that it has been the largest of all terrestrial beings. It should have sufficed to have rescued the earth it inhabited, and the atmosphere it breathed, from the imputation of impotence in the conception and nourishment of animal life on a large scale: to have stifled in its birth the opinion of a writer, the most learned too of all others in the science of animal history, that in the new world, "La nature vivante est beaucoup moins agissante, beaucoup moins forte:" that Nature is less active, less energetic on one side of the globe than she is on the other. [xvii] As if both sides were not warmed by the same genial sun; as if a soil of the same chemical composition was less capable of elaboration into animal nutriment; as if the fruits and grains from that soil and sun yielded a less rich chyle, gave less ex- tension to the solids and fluids of the body, or produced sooner in the cartilages, membranes, and fibres, that rigidity which restrains all further extension, and terminates animal growth. The truth is, that a pigmy and a Patagonian, a mouse and a mammoth, derive their dimensions from the same nutritive juices. The difference of increment depends on circumstances unsearchable to beings with our capacities. Every race of animals seems to have received from their Maker certain laws of extension at the time of their formation. Their elaborative organs were formed to produce this, while proper obstacles were opposed to its further progress. Below these limits they cannot fall, nor rise above them. What intermediate station they shall take may depend on soil, on climate, on food, on a careful choice of breeders. But all the manna of heaven would never raise the mouse to the bulk of the mammoth.

The opinion advanced by the Count de Buffon [xviii] is, 1, That the animals, common both to the old and new world, are smaller in the latter. 2, That those peculiar to the new are on a smaller scale. 3, That those which have been domesticated in both, have degenerated in America; and, 4, That on the whole it exhibits fewer species. And the reason he thinks is, that the heats of America are less; that more waters are spread over its surface by Nature, and fewer of these drained off by the hand of man. In other words, that heat is friendly, and moisture adverse to the production and development of large quadrupeds. I will not meet this hypothesis on its first doubtful ground, whether the climate of America be comparatively more humid? Because we are not furnished with observations sufficient to decide this question. And though, till it be decided, we are as free to deny, as others are to affirm the fact, yet for a moment let it be supposed. The hypothesis, after this supposition, proceeds to another; that moisture is unfriendly to animal growth. The truth of this is inscrutable to us by reasonings a priori. Nature has hidden from us her modus agendi. Our only appeal on such questions is to experience; and I think that experience is against the supposition. It is by the assistance of heat and moisture that vegetables are elaborated from the elements of earth, air, water, and fire. We accordingly see the more humid climates produce the greater quantity of vegetables. Vegetables are mediately or immediately the food of every animal; and in proportion to the quantity of food, we see animals not only multiplied in their numbers, but improved in their bulk, as far as the laws of their nature will admit. Of this opinion is the Count de Buffon himself in another part of his work: [xix] "En general il paroit que les pays un peu froids conviennent mieux a nos boeufs que les pays chauds, et qu'ils sont d'autant plus gros et plus grands que le climat est plus humide et plus abondans en paturages. Les boeufs de Danemarck, de la Podolie, de l'Ukraine et de la Tartarie qu'habitent les Calmouques sont les plus grands de tous.' [xx] Here then a race of animals, and one of the largest too, has been increased in its dimensions by cold and moisture, in direct opposition to the hypothesis, which supposes that these two circumstances diminish animal bulk, and that it is their contraries, heat and dryness, which enlarge it. But when we appeal to experience, we are not to rest satisfied with a single fact. Let us therefore try our question on more general ground. Let us take two portions of the earth, Europe and America for instance, sufficiently extensive to give operation to general causes; let us consider the circumstances peculiar to each, and observe their effect on animal nature. America, running through the torrid as well as temperate zone, has more heat, collectively taken, than Europe. But Europe, according to our hypothesis, is the dryest. They are equally adapted then to animal productions, each being endowed with one of those causes which befriend animal growth, and with one which opposes it. If it be thought unequal to compare Europe with America, which is so much larger, I answer, not more so than to com- pare America with the whole world. Besides, the purpose of the comparison is to try an hypothesis, which makes the size of animals depend on the heat and moisture of climate. If therefore we take a region, so extensive as to comprehend a sensible distinction of climate, and so extensive too as that local accidents, or the intercourse of animals on its borders, may not materially affect the size of those in its interior parts, we shall comply with those conditions which the hypothesis may reasonably demand. The objection would be the weaker in the present case, because any intercourse of animals which may take place on the confines of Europe and Asia, is to the advantage of the former, Asia producing certainly larger animals than Europe. Let us then take a comparative view of the quadrupeds of Europe and America, presenting them to the eye in three different tables, in one of which shall be enumerated those found in both countries; in a second those found in one only; in a third those which have been domesticated in both. To facilitate the comparison, let those of each table be arranged in gradation according to their sizes, from the greatest to the smallest, so far as their sizes can be conjectured. The weights of the large animals shall be ex- pressed in the English avoirdupoise pound and its decimals; those of the smaller in the ounce and its decimals. Those which are marked thus, [*] are actual weights of particular subjects, deemed among the largest of their species. Those marked thus [†], are furnished by judicious persons, well acquainted with the species, and saying, from conjecture only, what the largest individual they had seen would probably have weighed. The other weights are taken from Messrs. Buffon and D'Aubenton, and are of such subjects as came casually to their hands for dissection. This circumstance must be remembered where their weights and mine stand opposed; the latter being stated, not to produce a conclusion in favor of the American species, but to justify a suspension of opinion until we are better informed, and a suspicion in the mean time that there is no uniform difference in favor of either, which is all I pretend.

A COMPARATIVE VIEW OF THE QUADRUPEDS OF EUROPE AND OF AMERICA.

I. ABORIGINALS OF BOTH.

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II. ABORIGINALS OF ONE ONLY.

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III. DOMESTICATED IN BOTH.

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I have not inserted in the first table the [xxi] phoca nor leather-winged bat, because the one living half the year in the water, and the other being a winged animal, the individuals of each species may visit both continents.

Of the animals in the first table, Mons. de Buffon himself informs us, [xxii] that the roe, the beaver, the otter, and shrew mouse, though of the same species, are larger in America than Europe. This should therefore have corrected the generality of his expressions; [xxiii] and elsewhere, that the animals common to the two countries, are considerably less in America than in Europe: "& cela sans aucune exception." He tells us too, [xxiv] that on examining a bear from America, he remarked no difference: " Dans la forme de cet ours d' Amerique compart a celui d' Europe." But adds from Bartram's journal, that an American bear weighed 400 lb English, equal to 367 lb French; whereas we find the European bear, examined by Mons. D'Aubenton, [xxv] weighed but 141 lb French. Kalm tells us that the moose, orignal, or palmated elk of America, is as high as a tall horse; and Catesby, that it is about the bigness of a middle-sized ox. [xxvi] I have seen a skeleton 7 feet high, and from good information believe they are often considerably higher. The Elk of Europe is not two-thirds of his height. The wesel is larger in America than in Europe, as may be seen by comparing its dimensions as reported by Mons. D' Aubenton and Kalm. [xxvii] The latter tells us that the lynx, badger, red fox, and flying .squirrel, are the same in America as in Europe; by which expression I understand they are the same in all material circumstances, in size as well as others; for if they were smaller, they would differ from the European. [xxviii] Our grey fox is, by Catesby's account, little different in size and shape from the European fox. [xxix] I presume he means the red fox of Europe, as does Kalm, where he says, [xxx] that in size "they do not quite come up to our foxes." For proceeding next to the red fox of America, he says " they are entirely the same with the European sort;" which shews he had in view one European sort only, which was the red. So that the result of their testimony is, that the American grey fox is somewhat less than the European red; which is equally true of the grey fox of Europe, as may be seen by comparing the measures of the Count de Buffon and Mons. D'Aubenton. [xxxi] The white bear of America is as large as that of Europe. The bones of the mammoth, which have been found in America, are as large as those found in the old world. It may be asked, why I insert the mammoth, as if it still existed? I ask in return why I should omit it, as if it did not exist? Such is the economy of Nature, that no instance can be produced of her having permitted any one race of her animals to become extinct; of her having formed any link in her great work so weak as to be broken. To add to this, the traditionary testimony of the Indians, that this animal still exists in the Northern and Western parts of America^ would be adding the light of a taper to that of the meridian sun. Those parts still remain in their aboriginal state, un- explored and undisturbed by us, or by others for us. He may as well exist there now, as he did formerly, where we find his bones. If he be a carnivorous animal, as some anatomists have conjectured, and the Indians affirm, his early retirement may be accounted for from the general destruction of the wild game by the Indians, which commences in the first instant of their connection with us, for the purpose of purchasing match- coats, hatchets, and fire locks, with their skins. There remain then the renne, the buffalo, red deer, fallow deer, wolf, glutton, wild cat, monax, vison, hedgehog, martin, and water rat, of the comparative sizes of which we have not sufficient testimony. It does not appear that Messrs. de Buffon and D' Aubenton have measured, weighed, or seen those of America. It is said of some of them, by some travelers, that they are smaller than the European. But who were these travelers? Have they not been men of a very different description from those who have laid open to us the other three quarters of the world? Was natural history the object of their travels? Did they measure or weigh the animals they speak of? or did they not judge of them by sight, or perhaps even from report only? Were they acquainted with the animals of their own country, with which they undertake to compare them? Have they not been so ignorant as often to mistake the species? [xxxii] A true answer to these questions would probably lighten their authority, so as to render it insufficient for the foundation of an hypothesis. How unripe we yet are, for an accurate comparison of the animals of the two countries, will appear from the work of Mons. de Buffon. The ideas we should have formed of the sizes of some animals, from the information he had received at his first publications concerning them, are very different from what his subsequent communications give us. And indeed his candor in this can never be too much praised. One sentence of his book must do him immortal honor.

"J' aime autant une personne qui me releve d' une erreur, qu'une autre qui m' apprend une verite, parce qu'en effet une erreur corrigee est une verity." [xxxiii] He seems to have thought the Cabiai he first examined wanted little of its full growth. "Il n'etoit pas encore tout-a-fait adulte." [xxxiv] Yet he weighed but 46-1/2 lb, and he found afterwards that these animals, when full grown, weigh 100 lb. [xxxv] He had supposed, from the examination of a jaguar, said to be two years old, which weighed but 16 lb 12 oz., that, when he should have acquired his full growth, he would not be larger than a middle-sized dog. [xxxvi] But a subsequent account raises his weight to 200 lb. [xxxvii] Further information will, doubtless, produce further corrections. The wonder is, not that there is yet something in this great work to correct, but that there is so little. The result of this view then is, that of 26 quadrupeds common to both countries, 7 are said to be larger in America, 7 of equal size, and 12 not sufficiently examined. So that the first table impeaches the first member of the assertion, that of the animals common to both countries, the American are smallest: "Et cela sans aucune exception." It shews it not just, in all the latitude in which its author has advanced it, and probably not to such a degree as to found a distinction between the two countries.
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Re: Notes on the State of Virginia, by Thomas Jefferson

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PART 2 OF 2

Proceeding to the second table, which arranges the animals found in one of the two countries only, Mons. de Buffon observes that the tapir, the elephant of America, is but of the size of a small cow. To preserve our comparison, I will add that the wild boar, the elephant of Europe, is little more than half that size. I have made an elk, with round or cylindrical horns, an animal of America, and peculiar to it, because I have seen many of them myself, and more of their horns; and because I can say from the best information, that in Virginia this kind of elk has abounded much, and still exists in smaller numbers; the palmated kind is confined to the more Northern latitudes. [xxxviii] I have made our hare or rabbit peculiar, believing it to be different from both the European animals of those denominations, and calling it therefore by its Algonquin name Whabus, to keep it distinct from these, [xxxix] Kalm is of the same opinion. I have enumerated the squirrels according to our own knowledge, derived from daily sight of them, because I am not able to reconcile with that the European appellations and descriptions. I have heard of other species, but they have never come within my own notice. These, I think, are the only instances in which I have departed from the authority of Mons. de Buffon in the construction of this table. I take him for my ground work, because I think him the best informed of any naturalist who has ever written. The result is, that there are 18 quadrupeds peculiar to Europe; more than four times as many, to wit, 74, peculiar to America; that the [xl] first of these 74 weighs more than the whole column of Europeans; and consequently this second table disproves the second member of the assertion, that the animals peculiar to the new world are on a smaller scale, so far as that assertion relied on European animals for support; and it is in full opposition to the theory which makes the animal volume to depend on the circumstances of heat and moisture.

The third table comprehends those quadrupeds only which are domestic in both countries. That some of these, in some parts of America, have become less than their original stock, is doubtless true; and the reason is very obvious. In a thinly peopled country, the spontaneous productions of the forests and waste fields are sufficient to support indifferently the domestic animals of the farmer, with a very little aid from him in the severest and scarcest season. He therefore finds it more convenient to receive them from the hand of Nature in that indifferent state, than to keep up their size by a care and nourishment which would cost him much labor. If, on this low fare, these animals dwindle, it is no more than they do in those parts of Europe where the poverty of the soil, or poverty of the owner, reduces them to the same scanty subsistence. It is the uniform effect of one and the same cause, whether acting on this or that side of the globe. It would be erring therefore against that rule of philosophy, which teaches us to ascribe like effects to like causes, should we impute this diminution of size in America to any imbecility or want of uniformity in the operations of Nature. It may be affirmed with truth that, in those countries, and with those individuals of America, where necessity or curiosity has produced equal attention as in Europe to the nourishment of animals, the horses, cattle, sheep and hogs of the one continent are as large as those of the other. There are particular instances, well attested, where individuals of this country have imported good breeders from England, and have improved their size by care in the course of some years. To make a fair comparison between the two countries, it will not answer to bring together animals of what might be deemed the middle or ordinary size of their species; because an error in judging of that middle or ordinary size would vary the result of the comparison. Thus Monsieur D'Aubenton considers a horse of 4 feet 5 inches high, and 400 lb weight, French, equal to 4 feet 8.6 inches, and 436 lb English, as a middle-sized horse. [xli] Such a one is deemed a small horse in America. The extremes must therefore be resorted to. The same anatomist dissected a horse of 5 feet 9 inches height, French measure, equal to 6 feet 1.7 English, [xlii] This is near 6 inches higher than any horse I have seen; and could it be supposed that I had seen the largest horses in America, the conclusion would be, that ours have diminished, or that we have bred from a smaller stock. In Connecticut and Rhode Island, where the climate is favorable to the production of grass, bullocks have been slaughtered which weighed 2,500, 2,200, and 2,100 lb nett; and those of 1,800 lb have been frequent. I have seen a hog [xliii] weigh 1,050 lb after the blood, bowels and hair had been taken from him. Before he was killed an attempt was made to weigh him with a pair of steelyards, graduated to 1,200 ft, but he weighed more. Yet this hog was probably not within fifty generations of the European stock. I am well informed of another which weighed 1,100 lb gross. Asses have been still more neglected than any other domestic animal in America. They are neither fed nor housed in the most rigorous season of the year. Yet they are larger than those measured by Mons. D'Aubenton, of 3 feet 7-1/3 inches, 3 feet 4 inches, and 3 feet 2-1/2 inches; the latter weighing only 215.8 lb. [xliv] These sizes, I suppose, have been produced by the same negligence in Europe, which has produced a like diminution here. Where care has been taken of them on that side of the water, they have been raised to a size bordering on that of the horse; not by the heat and dryness of the climate, but by good food and shelter. Goats have been also much neglected in America. Yet they are very prolific here, bearing twice or three times a year, and from one to five kids at a birth. Mons. de Buffon has been sensible of a difference in this circumstance in favor of America, [xlv] But what are their greatest weights I cannot say. A large sheep here weighs 100 lb. I observe Mons. D'Aubenton calls a ram of 62 lb one of the middle size. [xlvi] But to say what are the extremes of growth in these and the other domestic animals of America, would require information of which no one individual is possessed. [xlvii] The weights actually known and stated in the third table preceding, will suffice to shew that we may conclude, on probable grounds, that, with equal food and care, the climate of America will preserve the races of domestic animals as large as the European stock from which they are derived; and consequently that the third member of Mons. de Buffon's assertion, that the domestic animals are subject to degeneration from the climate of America, is as probably wrong as the first and second were certainly so.

That the last part of it is erroneous, which affirms that the species of American quadrupeds are comparatively few, is evident from the tables taken all together. By these it appears that there are an hundred species aboriginal of America. [xlviii] Mons. de Buffon supposes about double that number existing on the whole earth. Of these, Europe, Asia, and Africa, furnish suppose 126; that is, the 26 common to Europe and America, and about 100 which are not in America at all. The American species then are to those of the rest of the earth, as 100 to 126, or 4 to 5. But the residue of the earth being double the extent of America, the exact proportion would have been but as 4 to 8. [xlix]

Hitherto I have considered this hypothesis as applied to brute animals only, and not in its extension to the man of America, whether aboriginal or transplanted, [l] It is the opinion of Mons. de Buffon that the former furnishes no exception to it: [li] "Quoique le sauvage du nouveau monde soit a-peu-pres de meme stature que l'homme de notre monde, cela ne suffit pas pour qu'il puisse faire une exception au fait general du rapetissement de la nature vivante dans tout ce continent: le sauvage est foible & petit par les organes de la generation; il n'a ni poil, ni barbe, & nulla ardeur pour sa femelle: quoique plus leger que l' Europeen parce qu'il a plus d'habitude a courir, il est cependant beaucoup moins fort de corps; il est aussi bien moins sensible, & cependant plus craintif & plus lache; il n'a nulle vivacite, nulle activite dans l'ame; celle du corps est moins un exercice, un mouvement volontaire qu'une necessite d'action causee par le besoin; otez lui la faim & la soif, vous detruirez en meme temps le principe actif de tous ses mouvemens; il demeurera stupidement en repos sur ses jambes ou couche pendant des jours en tiers. Il ne faut pas aller chercher plus loin la cause de la vie dispersee des sauvages & de leur eloignement pour la societe; la plus precieuse etincelle du feu de la nature leur a ete refusee; ils manquent d'ardeur pour leur femelle, & par consequent d'amour pour leur semblables; ne connoissant pas l'attachement le plus vif, le plus tendre de tous, leurs autres sentimens de ce genre sont froids & languissans; ils aiment foiblement leurs peres and leurs enfans; la societe la plus intime de toutes, celle de la meme famille, n'a done chez eux que de foibles liens; la societe d'une famille a l'autre n'en a point du tout; des lors nulle reunion, nulle republique, nulle etat social. La physique de l'amour fait chez eux le moral des moeurs; leur coeur est glace, leur societe froide, & leur empire dur. lls ne regardent leurs femmes que comme des servantes de peine ou des betes de somme qu'ils chargent, sans menagement, du fardeau de leur chasse, & qu'ils forcent sans pitie, sans reconnoissance, a des ouvrages qui souvent sont audessus de leurs forces; ils n'ont que peu d'enfans; ils en ont peu de soin; tout se ressent de leur premier defaut; ils sont indifferents parce qu'ils sont peu puissans, & cette indifference pour le sexe est la tache originelle qui fletrit la nature, qui l'empeche de s'epanouir, & qui detruisant les germes de la vie, coupe en meme temps la racine de la societe. L'homme ne fait done point d'exception ici. La nature en lui refusant les puissances de l'amour l'a plus maltraite & plus rapetise qu'aucun des animaux." An afflicting picture indeed, which, for the honor of human nature, I am glad to believe has no original. Of the Indian of South America I know nothing, for I would not honor with the appellation of knowledge what I derive from the fables published of them. These I believe to be just as true as the fables of Aesop. This belief is founded on what I have seen of man, white, red, and black, and what has been written of him by authors, enlightened themselves, and writing amidst an enlightened people. The Indian of North America being more within our reach, I can speak of him somewhat from my own knowledge, but more from the information of others better acquainted with him, and on whose truth and judgment I can rely. From these sources I am able to say, in contradiction to this representation, [lii] that he is neither more defective in ardor, nor more impotent with his female, than the white reduced to the same diet and exercise; that he is brave, when an enterprise depends on bravery; [liii] education with him making the point of honor consist in the destruction of an enemy by stratagem, and in the preservation of his own person free from injury; or perhaps this is nature; while it is education which teaches us to [liv] honor force more than finesse; that he will defend himself against an host of enemies, always choosing to be killed rather than to [lv] surrender, though it be to the whites, who he knows will treat him well; that in other situations also he meets death with more deliberation, and endures tortures with a firmness unknown almost to religious enthusiasm with us; that he is affectionate to his children, careful of them, and indulgent in the extreme; that his affections comprehend his other connections, weakening, as with us, from circle to circle, as they recede from the centre; that his friendships are strong and faithful to the uttermost [lvi] extremity; that his sensibility is keen, even the warriors weeping most bitterly on the loss of their children, though in general they endeavor to appear superior to human events; that his vivacity and activity of mind is equal to ours in the same situation; hence his eagerness for hunting, and for games of chance. The women are submitted to unjust drudgery. This I believe is the case with every barbarous people. With such, force is law. The stronger sex therefore imposes on the weaker. It is civilization alone which replaces women in the enjoyment of their natural equality. That first teaches us to subdue the selfish passions, and to respect those rights in others which we value in ourselves. Were we in equal barbarism, our females would be equal drudges. The man with them is less strong than with us, but their woman stronger than ours; and both for the same obvious reason; because our man and their woman is habituated to labor, and formed by it. With both races the sex which is indulged with ease is least athletic. An Indian man is small in the hand and wrist for the same reason for which a sailor is large and strong in the arms and shoulders, and a porter in the legs and thighs. They raise fewer children than we do. The causes of this are to be found, not in a difference of nature, but of circumstance. The women very frequently attending the men in their parties of war and of hunting, child-bearing becomes extremely inconvenient to them. It is said, therefore, that they have learnt the practice of procuring abortion by the use of some vegetable; and that it even extends to prevent conception for a considerable time after. [lvii] During these parties they are exposed to numerous hazards, to excessive exertions, to the greatest extremities of hunger. Even at their homes the nation depends for food, through a certain part of every year, on the gleanings of the forest; that is, they experience a famine once in every year. With all animals, if the female be badly fed, or not fed at all, her young perish; and if both male and female be reduced to like want, generation becomes less active, less productive. To the obstacles then of want and hazard, which Nature has op- posed to the multiplication of wild animals, for the purpose of restraining their numbers within certain bounds, those of labor and of voluntary abortion are added with the Indian. No wonder then if they multiply less than we do. Where food is regularly supplied, a single farm will shew more of cattle than a whole country of forests can of buffaloes. The same Indian women, when married to white traders, who feed them and their children plentifully and regularly, who exempt them from excessive drudgery, who keep them stationary and unexposed to accident, produce and raise as many children as the white women. [lviii] Instances are known, under these circum- stances, of their rearing a dozen children. An inhuman practice once prevailed in this country of making slaves of the Indians. This practice commenced with the Spaniards with the first discovery of America. — [See Herrera. Amer. Vesp.] It is a fact well known with us, that the Indian women so enslaved produced and raised as numerous families as either the whites or blacks among whom they lived. It has been said that Indians have less hair than the whites, except on the head. But this is a fact of which fair proof can scarcely be had. [lix] With them it is disgraceful to be hairy on the body. They say it likens them to hogs. They there- fore pluck the hair as fast as it appears. But the traders who marry their women, and prevail on them to discontinue this practice, say that Nature is the same with them as with the whites. Nor, if the fact be true, is the consequence necessary which has been drawn from it. Negroes have notoriously less hair than the whites; yet they are more ardent. But if cold and moisture be the agents of Nature for diminishing the races of animals, how comes she all at once to suspend their operation as to the physical man of the new world, whom the Count acknowledges to be "a peu pres de meme stature que l'homme de notre monde," and to let loose their influence on his moral faculties? How has this "combination of the elements and other physical causes, so contrary to the enlargement of animal nature in this new world, these obstacles to the developement and formation of great germs," been arrested and suspended, so as to permit the human body to acquire its just dimensions, and by what inconceivable process has their action been directed on his mind alone? [lx] To judge of the truth of this, to form a just estimate of their genius and mental powers, more facts are wanting, and great allowance to be made for those circumstances of their situation which call for a display of particular talents only. This done, we shall probably find that they are formed in mind as well as in body, on the same module with the "Homo sapiens Europaeus." [lxi] The principles of their society forbidding all compulsion, they are to be led to duty and to enterprise by personal influence and persuasion. Hence eloquence in council, bravery and address in war, become the foundations of all consequence with them. To these acquirements all their faculties are directed. Of their bravery and address in war we have multiplied proofs, because we have been the subjects on which they were exercised. Of their eminence in oratory we have fewer examples, because it is displayed chiefly in their own councils. Some, however, we have of very superior lustre. I may challenge the whole orations of Demosthenes and Cicero, and of any more eminent orator, if Europe has furnished more eminent, to produce a single passage, superior to the speech of Logan, a Mingo chief, to Lord Dunmore, when Governor of this State. And, as a testimony of their talents in this line, I beg leave to introduce it, first stating the incidents necessary for understanding it. In the Spring of the year 1774, a robbery and murder were committed on an inhabitant of the frontiers of Virginia, by two Indians of the Shawanee tribe. The neighboring whites, according to their custom, undertook to punish this outrage in a summary way. Col. Cresap, a man infamous for the many murders he had committed on those much-injured people, collected a party, and proceeded down the Kanhaway in quest of vengeance. Unfortunately a canoe of women and children, with one man only, was seen coming from the opposite shore, unarmed, and unsuspecting a hostile attack from the whites. Cresap and his party concealed themselves on the bank of the river, and the moment the canoe reached the shore, singled out their objects, and at one fire killed every person in it. This happened to be the family of Logan, who had long been distinguished as a friend of the whites. This unworthy return provoked his vengeance. He accordingly signalized himself in the war which ensued. In the Autumn of the same year, a decisive battle was fought at the mouth of the Great Kanhaway, between the collected forces of the Shawanees, Mingoes, and Delawares, and a detachment of the Virginia militia. The Indians were defeated, and sued for peace. Logan however disdained to be seen among the suppliants. But, lest the sincerity of a treaty should be distrusted, from which so distinguished a chief absented himself, he sent by a messenger the following speech to be delivered to Lord Dunmore. "I appeal to any white man to say if ever he entered Logan's cabin hungry, and he gave him not meat; if ever he came cold and naked, and he clothed him not. During the course of the last long and bloody war, Logan remained idle in his cabin, an advocate for peace. Such was my love for the whites, that my countrymen pointed as they passed, and said, 'Logan is the friend of white men.' I had even thought to have lived with you, but for the injuries of one man. Col. Cresap, the last Spring, in cold blood, and unprovoked, murdered all the relations of Logan, not sparing even my women and children. There runs not a drop of my blood in the veins of any living creature. This called on me for revenge. I have sought it: I have killed many: I have fully glutted my vengeance. For my country, I rejoice at the beams of peace. But do not harbor a thought that mine is the joy of fear. Logan never felt fear. He will not turn on his heel to save his life. Who is there to mourn for Logan? Not one." [lxii]

Before we condemn the Indians of this continent as wanting genius, we must consider that letters have not yet been introduced among them, [lxiii] Were we to compare them in their present state with the Europeans North of the Alps, when the Roman arms and arts first crossed those mountains, the comparison would be unequal, because, at that time, those parts of Europe were swarming with numbers; because numbers produce emulation, and multiply the chances of improvement, and one improvement begets another. Yet I may safely ask, How many good poets, how many able mathematicians, how many great inventors in arts or sciences, had Europe North of the Alps then produced? And it was sixteen centuries after this before a Newton could be formed. I do not mean to deny that there are varieties in the race of man, distinguished by their powers both of body and mind. I believe there are, as I see to be the case in the races of other animals. I only mean to suggest a doubt, whether the bulk and faculties of animals depend on the side of the Atlantic on which their food happens to grow, or which furnishes the elements of which they are compounded? Whether Nature has enlisted herself as a Cis or Trans-Atlantic partizan? I am induced to suspect there has been more eloquence than sound reasoning displayed in support of this theory; that it is one of those cases where the judgment has been seduced by a glowing pen; and whilst I render every tribute of honor and esteem to the celebrated Zoologist, who has added, and is still adding, so many precious things to the treasures of science, I must doubt whether in this instance he has not cherished error also, by lending her for a moment his vivid imagination and bewitching language. [lxiv] (4.)

So far the Count de Buffon has carried this new theory of the tendency of Nature to belittle her productions on this side the Atlantic. Its application to the race of whites, trans- planted from Europe, remained for the Abbe Raynal. "On doit etre etonne (he says) que 1' Amerique n'ait pas encore produit un bon poete, un habile mathematicien, un homme de genie dans un seul art, ou une seule science." 7. Hist. Philos. p. 92 ed. Maestricht. 1774. " America has not yet produced one good poet." When we shall have existed as a people as long as the Greeks did before they produced a Homer, the Romans a Virgil, the French a Racine and Voltaire, the English a Shakespeare and Milton, should this reproach be still true, we will enquire from what unfriendly causes it has proceeded, that the other countries of Europe and quarters of the earth shall not have inscribed any name in the roll of poets. [lxv] But neither has America produced "one able mathematician, one man of genius in a single art or a single science." In war we have produced a Washington, whose memory will be adored while liberty shall have votaries, whose name will triumph over time, and will in future ages assume its just station among the most celebrated worthies of the world, when that wretched philosophy shall be forgotten, which would have arranged him among the degeneracies of Nature. In physics we have produced a Franklin, than whom no one of the present age has made more important discoveries, nor has enriched philosophy with more or more ingenious solutions of the phenomena of Nature. We have supposed Mr. Rittenhouse second to no astronomer living; that in genius he must be the first, because he is self-taught. As an artist he has exhibited as great a proof of mechanical genius as the world has ever produced. He has not indeed made a world; but he has by imitation approached nearer its Maker than any man who has lived from the creation to this day. [lxvi] As in philosophy and war, so in government, in oratory, in painting, in the plastic art, we might show that America, though but a child of yesterday, has already given hopeful proofs of genius, as well of the nobler kinds, which arouse the best feelings of man, which call him into action, which substantiate his freedom, and conduct him to happiness, as of the subordinate, which serve to amuse him only. We therefore suppose that this reproach is as unjust as it is unkind; and that of the geniuses which adorn the present age, America contributes its full share. For comparing it with those countries, where genius is most cultivated, where are the most excellent models for art, and scaffoldings for the attainment of science, as France and England for instance, we calculate thus: The United States contain three millions of inhabitants; France twenty millions; and the British Islands ten. We produce a Washington, a Franklin, a Rittenhouse. France then should have half a dozen in each of these lines, and Great Britain half that number, equally eminent. It may be true that France has: we are but just becoming acquainted with her, and our acquaintance so far gives us high ideas of the genius of her inhabitants. It would be injuring too many of them to name particularly a Voltaire, a Buffon, the constellation of Encyclopedists, the Abbe Raynal himself, &c., &c. We therefore have reason to believe she can produce her full quota of genius. The present war having so long cut off all communication with Great Britain, we are not able to make a fair estimate of the state of science in that country. The spirit in which she wages war is the only sample before our eyes, and that does not seem the legitimate offspring either of science or of civilization. The sun of her glory is fast descending to the horizon. Her philosophy has crossed the Channel, her freedom the Atlantic, and herself seems passing to that awful dissolution, whose issue is not given human foresight to scan. [lxvii]

Having given a sketch of our minerals, vegetables, and quadrupeds, and being led by a proud theory to make a comparison of the latter with those of Europe, and to extend it to the Man of America, both aboriginal and emigrant, I will proceed to the remaining articles comprehended under the present query.

Between ninety and an hundred of our birds have been described by Catesby. His drawings are better as to form and attitude, than coloring, which is generally too high. They are the following:

Image

Besides these, we have

Image

And doubtless many others which have not yet been described and classed.

To this catalogue of our indigenous animals, I will add a short account of an anomaly of Nature, taking place sometimes in the race of negroes brought from Africa, who, though black themselves, have, in rare instances, white children, called Albinos. I have known four of these myself, and have faithful accounts of three others. The circumstances in which all the individuals agree are these. They are of a pallid cadaverous white, untinged with red, without any colored spots or seams; their hair of the same kind of white, short, coarse, and curled as is that of the negro; all of them well formed, strong, healthy, perfect in their senses, except that of sight, and born of parents who had no mixture of white blood. Three of these Albinos were sisters, having two other full sisters, who were black. The youngest of the three was killed by lightning, at twelve years of age. The eldest died at about 27 years of age, in childbed, with her second child. The middle one is now alive in health, and has issue, as the eldest had, by a black man, which issue was black. They are uncommonly shrewd, quick in their apprehensions and in reply. Their eyes are in a perpetual tremulous vibration, very weak, and much affected by the sun; but they see better in the night than we do. They are of the property of Colonel Skipwith, of Cumberland. The fourth is a negro woman, whose parents came from Guinea, and had three other children, who were of their own color. She is freckled, her eye sight so weak, that she is obliged to wear a bonnet in the Summer; but it is better in the night than day. She had an Albino child by a black man. It died at the age of a few weeks. These were the property of Colonel Carter, of Albemarle. A sixth instance is a woman of the property of a Mr. Butler, near Petersburgh. She is stout and robust, has issue a daughter, jet black, by a black man. I am not informed as to her eye sight. The seventh instance is of a male belonging to a Mr. Lee, of Cumberland. His eyes are tremulous and weak. He is tall of stature, and now advanced in years. He is the only male of the Albinos which have come within my information. Whatever be the cause of the disease in the skin, or in its coloring matter, which produces this change, it seems more incident to the female than male sex. To these I may add the mention of a negro man within my own knowledge, born black, and of black parents; on whose chin, when a boy, a white spot appeared. This continued to increase till he became a man, by which time it had extended over his chin, lips, one cheek, the under jaw and neck on that side. It is of the Albino white, without any mixture of red, and has for several years been stationary. He is robust and healthy, and the change of color was not accompanied with any sensible disease, either general or topical.

Of our fish and insects there has been nothing like a full description or collection. More of them are described in Catesby than in any other work. Many also are to be found in Sir Hans Sloane's Jamaica, as being common to that and this country. The honey bee is not a native of our continent. Marcgrave indeed mentions a species of honey bee in Brasil. [lxxii] But this has no sting, and is therefore different from the one we have, which resembles perfectly that of Europe. The Indians concur with us in the tradition that it was brought from Europe; but when, and by whom, we know not. The bees have generally extended themselves into the country, a little in advance of the white settlers. [lxxiii] The Indians, therefore, call them the white man's fly, and consider their approach as indicating the approach of the settlements of the whites. A question here occurs, how far northwardly have these insects been found ? That they are unknown in Lapland, I infer from Scheffer's information that the Laplanders eat the pine bark, prepared in a certain way, instead of those things sweetened with sugar. " Hoc comedunt pro rebus saccharo conditis." — Scheff. Lapp., chap. 18. Certainly, if they had honey, it would be a better substitute for sugar than any preparation of the pine bark. Kalm tells us the honey bee cannot live through the Winter in Canada. [lxxiv] They furnish then an additional proof of the remarkable fact first observed by the Count de Buffon, and which has thrown such a blaze of light on the field of natural history, that no animals are found in both continents, but those which are able to bear the cold of those regions where they probably join.

We have it from the Indians also that the common domestic fly is not originally of America, but came with the whites from Europe. [lxxv]

_______________

Notes:

i. On whose authority has it been said? Bouguer, the best witness respecting the Andes, speaking of Peru, says "on n'y distingue aucun vestige des grandes inondations qui ont laisse tant de marques dans toutes les autres regions. J 'ai fait tout mon possible pour y decouvrir quelque coquille, mais toujours inutilement. Apparamment que les montagnes du Perou sont trop hautes." Bouguer, xv.

See 4 Clavigero, Diss. 3, § 1. See 2. Epoques 268. 1. Epoques 415.

ii. 2. Epoques, 378.

iii. 2. Buffon Epoques, 96.

iv. Five deluges are enumerated by Xenophon, the author of the tract de Equivocis in these words: "Inundationes plures fuere. Prima novimestris inundatio terrarum, sub prisco Ogyge. Secunda niliaca menstrua, sub Aegyptiis Hercule et Prometheo. Bimestris nutem, sub Ogygo Attico in Achaia. Trimestris Thessalica, sub Deucalione. Par Pharonica, sub Proteo Aegyptio in raptu Helenae."

v. 2. Epoques, 138, 139.

vi. See Pleasant's Argus, August 16, '99; that this disappeared December 25, '98, on which day a spring broke out 100 feet higher up the hill.

vii. Qu. If known in Europe before the discovery of America? Ramusic supposes this to be the grain described by Diod. Sic. L. 2, in his account of the travels of Iambulus, in the following passage: Image Image [Ceci bianchi. — Ital. Ers. Franc] Image Image Image Image Ramusic says of the Maize "in Italia, a i tempi nostri, [1550,] e stato, veduto 'la prima volta,' and the island in which it was found by Iambulus was Sumatra. — 1. Ramus. 174. The Maison rustique says that Turkey Corn came first from the West Indies into Turkey, and from thence into France." — L. 5, c. 17. Zimmerman says : "Il tire son origine des pays chauds de l'Amerique." — Zoologie geographique, page 24. " Il frumentone fu dalla America in Ispagne, e quindi in altri paesi della Europa." "Dalli Spagnuoli di Europa e di America e chiamato il frumentone col nome Maiz, preso dalla lingua Haitina che si parlava nella isola oggidi appellata Spagnuola, o sia di S. Domenico." — Clavigero I., 56. " Il frumentone, biada dalla providenza accordata a quella parte del mondo in vece del frumento dell Europa, del riso del Asia, e del miglio d' Africa." — 2. Clavig. 218. Acosta classes Indian Corn with the plants peculiar to America, observing that it is called "trigo de las Indias" in Spain, and "Grano de Turquia" in Italy. He says, " De donde fue el Mayz a Indias, y porque este grano tan provechoso le llaman en Italia Grano de Turquia mejor sabre preguntarlo, que dezirlo. Porque en efecto en los antiques no hallo rastro deste genero, aunque el Milio que Plinio escrive aver venido a Italia de la India diez anos avia, quando escrivio, tiene alguna similitud con el Mayz, en lo que dize que es grano, y que nace en cana, y se cubre de hoja, y que tiene al remate como cabellos, y el ser fertilissimo, todo lo qual no quadra con el Mijo, que comunmente entienden por Milio, en fin, repartio el Criador a todas partes su gobierno: a este orbe dio el triga que es el principal sustento de los hombres: a aquel de Indias dio el Mayz, que tras el trigo tiene el segundo lugar, para sustenta de hombres, y animales. — Acosta 4, 16.

viii. "Les pommes de terre sont indigenes en Guiane." — Zimmerman Zool. Geogr. 26. "La Papa fu portata in Messico dall' America Meridionale, suo proprio paese." — 1. Clavigero 58.

ix. Clavigero says: "Non mi sovviene che appo qualche nazione Americana vi sia memoria o degli elafanti, o degl ippopotami, o d' altri quadrupedi di si fatta grandezza. Non so che fin ora, fra tanti scavamenti fatta nella Nuova Spagna, siasi mai scoperto un carcamo d' Ippopotamo, e quel ch' e piu, ne anche un dente d' elefante. — 125.

x. 2. Epoques, 276, in Mexico; but, 1. Epoques, 250, denies the fact as to S. America.

xi. 22. Buflfon, 233; 2. Epoques, 230.

xii. 2. Epoques, 232. Buffon pronounces it is not the grinder either of the elephant or hippopotamus, mais d' une espece la premiere et la plus grande de tous les animaux terrestres, qui est perdue.

xiii. Hunter.

xiv. D'Aubenton.

xv. Xviii. 178; xxii. 121.

xvi. Qu? See 2. Epoques de Buffon, 231, 234.

xvii. Buffon, xviii. 122; Ed. Paris, 1764.

xviii. Xviii. 100, 156. "La terre est demeuree froide, impuissante a produire les principes actife, a developer les germes des plus grands quadrupedes, auxquels il faut, pour croitre et se multiplier, toute la chaleur, toute l'activite que le soleil peut donner a la terre, amoureuse." — Xviii. 156. "L'ardeur des hommes et la grandeur des animaus dependent de la salubrite et de la chaleur de l'air. — Ib. 160.

xix. Viii. 134.

xx. "Tout ce qu' il y a de colossal et de grand dans la nature, a ete forme dans les terres du Nord." 1. Epoques 255. " C'est dans les regions de notre Nord que la nature vivante s'est clevee a sea plus grandes dimensions. — Ib. 263.

*. There exists in the Western and mountainous parts of Pennsylvania an animal which seems to be nearer the hare than our whabus. The meat is black, and an individual weighed 39-1/2 oz. avoird., while the whabus is an animal of white meat, and weighs about 29 oz.; the fur of the former is white, as is the case with most animals in countries abounding with snow.

xxi. It is said that this animal is seldom seen above 30 miles from shore, or beyond the 56th degree of latitude. The interjacent islands between Asia and America admit his passing from one continent to the other without exceeding these bounds. And, in fact, travelers tell us that these islands are places of principal resort for them, and especially in the season of bringing forth their young.

xxii. Xxvii. 130; xxx. 213; 5. Sup. 201.

xxiii. xviii. 145.

xxiv. Quadrup. viiii. 334; edit. Paris, 1777.

xxv. xvii. 82.

xxvi. This sentence in the first edition began as follows: "Kalm tells us that the Black Moose or Renne of America is as high as a tall horse," &c. The author corrected it as in the text, appending a marginal note in these words: "This is not correct. Kalm considers the Moose as the Elk, and not as the Renne. Musu is the Algonkin name of the Orignal, or Elk. — I. xxvii."

xxvii. Xv. 42.

xxviii. I. 359. 1.48, 221, 251. II.52.

xxix. II. 78.

xxx. I. 220.

xxxi. Xxvii. 63.; xiv. 119. Harris, II. 387. Buffon, Quad, ix., 1.

xxxii. Even Amer. Vesp. says he saw lions and wild boars in America. — Letters, page 77. He saw a serpent 8 braccie long, and as thick as his own waist — 111.

xxxiii. Quad. ix. 158.

xxxiv. xxv. 184.

xxxv. Quad. ix. 132.

xxxvi. xix. 2.

xxxvii. Quad. ix. 41.

xxxviii. The descriptions of Theodat, Denys, and La Hontan, cited by Mons. de Buffon, under the article Elan, authorize the supposition, that the flat-horned elk is found in the Northern parts of America. It has not however extended to our latitudes. On the other hand, I could never learn that the round-horned elk has been seen further North than the Hudson's River. This agrees with the former elk in its general character, being, like that, when compared with a deer, very much larger, its ears longer, broader, and thicker in proportion, its hair much longer, neck and tail shorter, having a dewlap before the breast, (caruncula gutturalis Linnaei,) a white spot often, if not always, of a foot diameter, on the hinder part of the buttocks round the tail; its gait a trot, and attended with a rattling of the hoofs; but distinguished from that decisively by its horns, which are not palmated, but round and pointed. This is the animal described by Catesby as the Cervus major Americanus, the Stag of America, le Cerf de l' Amerique. But it differs from the Cervus as totally as does the palmated elk from the dama. And in fact it seems to stand in the same relation to the palmated elk as the red deer does to the fallow. It has abounded in Virginia, has been seen, within my knowledge, on the Eastern side of the Blue Ridge since the year 1765, is now common beyond those mountains, has been often brought to us and tamed, and their horns are in the hands of many. I should designate it as the "Alces Americanus cornibus teretibus." It were to be wished that naturalists, who are acquainted with the renne and elk of Europe, and who may hereafter visit the Northern parts of America, would examine well the animals called there by the names of grey and black moose, caribou, orignal, and elk. Mons. de Buffon has done what could be done, from the materials in his hands, towards clearing up the confusion introduced by the loose application of these names among the animals they are meant to designate. He reduces the whole to the renne and flat-horned elk. From all the information I have been able to collect, I strongly suspect they will be found to cover three, if not four distinct species of animals. I have seen skins of a moose, and of the caribou: they differ more from each other, and from that of the round-horned elk, than I ever saw two skins differ, which belonged to different individuals of any wild species. These differences are in the color, length, and coarseness of the hair, and in the size, texture, and marks of the skin. Perhaps it will be found that there is — 1, The moose, black and grey; the former being said to be the male, and the latter the female. 2, The caribou or renne. 3, The flat-horned elk, or orignal. 4, The round-horned elk. Should this last, though possessing so nearly the characters of the elk, be found to be the same with the Cerf d' Ardennes or Brandhirtz of Germany, still there will remain the three species first enumerated. See Catesby and Kalm — reason to believe that the Moose is the palmated elk or orignal.

xxxix. Kalm II. 340; I. 82.

xl. The Tapir is the largest of the animals peculiar to America. I collect his weight thus. Mons. de Buffon says, xxiii. 274, that he is of the size of a Zebu, or a small cow. He gives us the measures of a Zebu, ib. 94, as taken by himself, viz : 5 feet 7 inches from the muzzle to the root of the tail, and 5 feet 1 inch circumference behind the fore legs. A bull, measuring in the same way 6 feet 9 inches, and 5 feet 2 inches, weighed 600 lb.. — viii. 153. The Zebu then, and of course the Tapir, would weigh about 500 lb. But one individual, of every species of European peculiars, would probably weigh less than 400 ft. These are French measures and weights.

xli. Vii. 432.

xlii. vii. 474.

xliii. In Williamsburg, April, 1769.

xliv. Viii. 48, 65, 66.

xlv. xviii. 96.

xlvi. ix. 41.

xlvii. Perros en la Espanola han crecido en numero y en grandeza, desuerte que plaga de aquella isla. — Acosta iv. 33.

xlviii. Xxx. 219; xviii. 121.

xlix. 1. Epoques, 378.

l. 1. Clavigero, 118.

li. xviii. 146.

lii. Amer. Vesp. 13: "Fuora di misura lussurioai, &c. — 108.

liii. Amer. Vesp. 30, 31, 39, 75: "Di buono sforzo, e di grande animo."— Ib. 78.

liv. Sol Rodomonte sprezza di venire Se non, dove la via meno e sicura. — Ariosto 14, 117.

lv. In so judicious an author as Don Ulloa, and one to whom we are indebted for the most precise information we have of South America, I did not expect to find such assertions as the following: "Los Indios vencidos son los mas cobardes y pusilanimes que se peuden ver: se hacen inocentes, se humillan hasta el desprecio, disculpan su inconsiderado arrojo, y con las suplicas y los ruegos dan seguras pruebas de su pusilanimidad. — 6 lo que refieren las historias de la Conquista, sobre sus grandes acciones, es en un sentido figuardo, 6 el caracter de estas gentes no es ahora segun era entonces; pero lo que no tiene duda es, que las Naciones de la parte Septentrional subsisten en la misma libertad que siempre han tenido, sin haber sido sojuzgados por algun Principe extrano, y que viven segun su regimen y costumbres de toda la vida, sin que haya babido motivo para que muden de caracter; y en estos se ve lo mismo. que sucede en los del Peru, y de toda la America Meridional, reducidos, y que nunca lo han estado." Noticias Americanas. — Entretenimiento xviii. § 1. Don Ulloa here admits that the authors who have described the Indians of South America, before they were enslaved, had represented them as a brave people, and therefore seems to have suspected that the cowardice which he bad observed in those of the present race might be the effect of subjugation. But, supposing the Indians of North America to be cowards also, he concludes the ancestors of those of South America to have been so too, and therefore that those authors have given fictions for truths. He was probably not acquainted himself with the Indians of North America, and had formed his opinion of them from hearsay. Great numbers of French, of English, and of Americans, are perfectly acquainted with these people. Had he had an opportunity of enquiring of any of these, they would have told him that there never was an instance known of an Indian begging his life when in the power of his enemies : on the contrary, that he courts death by every possible insult and provocation. His reasoning then would have been reversed thus: "Sinco the present Indian of North America is brave, and authors tells us that the ancestors of those of South America were brave also, it must follow that the cowardice of their descendants is the effect of subjugation and ill treatment." For he observes ib. § 27, that "Los obrages los aniquilan por la inhumanidad con que se les trata."

lvi. A remarkable instance of this appeared in the case of the late Colonel Byrd, who was sent to the Cherokee nation to transact some business with them. It happened that some of our disorderly people had just killed one or two of that nation. It was therefore proposed in the council of the Cherokees that Colonel Byrd should be put to death in revenge for the loss of their countrymen. Among them was a chief called Silouee, who, on some former occasion, had contracted an acquaintance and friendship with Colonel Byrd. He came to him every night in his tent, and told him not to be afraid, they should not kill him. After many days deliberation, however, the determination was, contrary to Silouee's expectation, that Byrd should be put to death, and some warriors were dispatched as executioners, Silouee attended them, and when they entered the tent he threw himself between them and Byrd, and said to the warriors, " This man is my friend; before you get at him you must kill me." On which they returned, and the council respected the principle so much as to recede from their determination.

"Vivono cento cinquanta anni." — Amer. Vesp. 111.

lvii. Amer. Vesp. 13.

lviii. Amer. Vesp. 13. "Sono donne molto generative," &c.

lix. Amer. Vesp. 9.

lx. Xviii. 145.

lxi. Linn. Syst. Definition of a Man.

lxii. See letter of J. B. Gibson in Appendix iv.

lxiii. 1. Clavigero, 120.

lxiv. No writer, equally with M. de Buffon, proves the power of eloquence and uncertainty of theories. He takes any hypothesis whatever, or its reverse, and furnishes explanations equally specious and persuasive. Thus in his xviii. volume, wishing to explain why the largest animals are found in the torrid zone, he assumes heat as the efficient principle of the animal volume. Speaking of America, he says: "La terre y est froide impuissante a produire les principes actifs, a developer les germes des plus grandes quadrupedes auxquels il faut, pour croitre et se multiplier, toute la chaleur toute l'activite que le soleil peut donner a la terre amoureuse." — Page 156. " L'ardeur des hommes, et la grandeur des animaux dependent de la salubrite, et de la chaleur de l'air." — Ib. 160. In his Epochs again when it is become convenient to his theory to consider the bones of the Mammoth found in the coldest regions, as the bones of the elephant, and necessary to explain how the elephant there should have been six times as large as that of the torrid zone, it is cold which produces animal volume. "Tout ce qu' il y a de colossal et de grand dans la nature, a ete forme dans les terres du Nord." — 1. Epoques, 255. " C'est dans les regions de notre Nord que la nature vivante s'es't elevee a ses plus grandes dimensions." — Ib. 263.

lxv. Has the world as yet produced more than two poets, acknowledged to be such by all nations ? An Englishman only reads Milton with delight, an Italian Tasso, a Frenchman the Henriade, a Portuguese Camouens; but Homer and Virgil have been the rapture of every age and nation; they are read with enthusiasm in their originals by those who can read the originals, and in translations by those who cannot.

lxvi. There are various ways of keeping truth out of sight. Mr. Rittenhouse's model of the planetary system has the plagiary appellation of an Orrory; and the quadrant invented by Godfrey, an American also, and with the aid of which the European nations traverse the globe, is called Hadley's quadrant. Huyghens gave the first description of an instrument of the former kind, under the name of Automatum Planetarium. — 2. Montucla, 485.

lxvii. In a later edition of the Abbe Raynal's work, he has withdrawn his censure from that part of the new world inhabited by the Federo-Americans; but has left it still on the other parts. North America has always been more accessible to strangers than South. If he was mistaken then as to the former, he may be so as to the latter. The glimmerings which reach us from South America enable us only to see that its inhabitants are held under the accumulated pressure of slavery, superstition and ignorance. Whenever they shall be able to rise under this weight, and to show themselves to the rest of the world, they will probably show they are like the rest of the world. We have not yet sufficient evidence that there are more lakes and fogs in South America than in other parts of the earth. Amer. Vesp., 115. Quivi il cielo e l'aere e rare volte adombrato dalle nuvole, quasi sempre i giorni sono sereni? As little do we know what would be their operation on the mind of man. That country has been visited by Spaniards and Portuguese chiefly, and almost exclusively. These, going from a country of the old world remarkably dry in its soil and climate, fancied there were more lakes and fogs in South America than in Europe. An inhabitant of Ireland, Sweden, or Finland, would have formed the contrary opinion. Had South America then been discovered and seated by a people from a fenny country, it would probably have been represented as much drier than the old world. A patient pursuit of facts, and cautious combination and comparison of them, is the drudgery to which man is subjected by his Maker, if he wishes to attain sure knowledge.

lxviii. Clavigero, 85.

lxix. The Pheasant is rarely or not at all found beyond North Carolina. The grouse is first seen in the upper parts of Maryland, in Pennsylvania, and the country North of Ohio, and thence northwardly.==[Capt. Mer. Lewis.]

lxx. Clavigero says that in Mexico "vi sono i rinomati rossignoli."--I.88.

lxxi. The Bald Coot, or Coot, is the Fulica of Linnaeus, and the Foulque of the Encyclop. Meth., differing from the description of the latter only in the color of its feet and legs, which are olive green, without any circle of red, and that of the bill a faint carnation, brown at the point, and the membrane on the forehead of a very dark purple. It is distinguished from the Gallinula chloropis, Poule d'eau, Water-hen, Hydro-gallina, chiefly by the festooned web bordering the toes.

lxxii. See Herrera, Dec. 1, 1. 10, c. 8. " Descubierta Yucatan, se hallo abundancia de cera y miel." — And ib. c. 9. " Ay abispas y abexas, como las de Castilla, aunque estas son menores, y pican con mas furia." — Id. Dec. 2, 1. 3, c. 1.

lxxiii. See 1 Clavigero, 107. " En los terminos de Guayaquil ay abejas, que enxambran y crian miel en el bucco de los arboles son poco mayores que moscas, la cera y miel que labran es rubia y aunque tiene buengusto no es tal como el de Castilla. — Herr. 5, 10, 10.

lxxiv. I. 126.

lxxv. We have the same account from South America. Condamine in his Voyage de la riviere des Amazones, pa. 95, says "Divers Indiens ont rapports qu'ils avoient vu sur les bords de la riviere de Coari dans le haut des terres, un pays decouvert, des mouches et quantite de betes a cornes, objets nouveaux pour eux, et qui prouvent que les sources deccs rivieres arrosent des pays voisins des colonies Espagnoles du haut Perou."
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