The Ohio below the Rapids at Louisville—Ascent of the Mississippi from the mouth of the Ohio to St. Louis.[043]

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Our small boat descended over the rapids without injury; and having taken on board some wood near New Albany, we proceeded on our voyage, with a pressure of steam equalling one hundred pounds to the square inch, upon all parts of the engine exposed to its immediate operation. This enabled us to descend, at the rate of ten miles per hour. A small island in the Ohio, about twenty-three miles below the rapids, is called Flint Island, from the great numbers of fragments of flints, broken arrow points, and various instruments of stone, heretofore used by the Indians, which are found there on turning up the soil. This island has probably been the favourite residence of some tribe, particularly expert in the manufacture of those rude implements, with which the wants of the aboriginal Americans were supplied. The stone employed in these manufactures appears to have been, in most instances, that compact flint, which occurs in nodular masses, in the secondary limestones. In one instance we met with a triangular prism, of a very hard and compact aggregate of felspar, and hornblende, unlike any rock we have seen in the valley of the Mississippi. This prism was about five inches long, with faces of about {30} an inch in width, and was perforated, from end to end, forming a complete tube, with an orifice about half an inch in diameter, and[pg078] smoothly polished, both within and without. We were never able to discover to what use this implement could have been applied; nor do we recollect to have met with accounts of any thing analogous to it, except, perhaps, those "tubes of a very hard stone" mentioned by the Jesuit Venegas, as used by the natives of California, in their treatment of the sick.[044] That it may have passed, by means of the intercourse of various tribes of Indians, from the primitive mountains of California to the rapids of the Ohio, is not, perhaps, improbable. Indirect methods of communication may have conveyed the productions of one part of the continent to another very remote from it. The savages of the Missouri receive an intoxicating bean from their neighbours on the south and west; these again must probably procure it from other tribes inhabiting, or occasionally visiting, the tropical regions.

In the Philadelphia museum are many Indian pipes of that red indurated clay, found only (as far as hitherto known) on the Pipe Stone branch of the Little Sioux river of the Missouri; one of these, however, was found on the banks of the Rio de la Plata, in South America: several were found in the territory now called New England, and in the north-eastern part of the continent.

On the 26th we passed the mouth of the Wabash, and[pg079] arrived at Shawaneetown,[045] ten miles below. Near the mouth of the Wabash, an accident happened to the engine, which rendered it necessary for us to drift down, until we should arrive at some place where repairs might be made. Some of the gentlemen of the party determined to go on shore, and walk to Shawaneetown. In swimming across a creek, {31} three miles above that place, Lieutenant Graham dropped his rifle in the water, and having spent some time in attempts to recover it, did not arrive at Shawaneetown until after the boat had reached that place.

On the 27th, several of the party went out to hunt in the forests and swamps, north-west of Shawaneetown. At about four miles' distance from the Ohio, they arrived at the banks of a small pond, three miles long, and only three or four hundred yards wide. Here they killed a turkey; and some small birds. On the bank of the pond, was found a specimen of the Lake Erie tortoise,[046] depositing its eggs in the sand, at about twenty yards' distance from the water. It had made, with its feet, a hole in the sand, two inches in diameter and four inches in depth, enlarging towards the bottom to three inches. This species occurs frequently in the pools and stagnant waters along the Ohio. We first met with it near the rapids at Louisville. Among other birds, we noticed about Shawaneetown, the pileated woodpecker, the minute tern, numerous flocks of the psittacus caroliniensis, two broods of young wood duck, some gulls, and semipalmated sandpipers. The terns appear to be attracted hither by great[pg080] numbers of a species of phryganea, with which we found the stomachs of some of them filled. The semipalmated sandpipers were in large flocks, and did not appear stationary.

We left Shawaneetown at twelve o'clock on the 28th, and stopped three miles below, to take in wood; then proceeding forward, at four P. M. we ran aground on a sand bar, seven miles above the "Cave Inn," or "House of Nature."[047] After much exertion, by means of anchors and poles, with the aid of the engine, and all the men, who were under the necessity of jumping into the river, we at length {32} succeeded in getting her off, and ran down to the cave, where we lay by for the night.

Early the next morning, we went to visit the cave, of the entrance to which two views were sketched by Mr. Seymour. It is a perpendicular fissure, extending about one hundred and sixty feet into the horizontal limestone cliffs, which here form the north bank of the river. At times of high water, the Ohio flows in, and fills the cave nearly to its roof. In this cave, it is said, great numbers of large bones were some time ago found, but we saw no remains of any thing of this kind. Impressions and casts of the shells of submarine animals are seen in the rocks, forming the sides of the cave, as in all the strata of compact limestone, in this region. The organic remains here, do not appear to be so numerous as those of the rocks at the falls, and at Cincinnati; and are much less distinct, and visible in the fracture; indeed the fracture generally exhibits to the eye no vestige of organic remains. It is upon the surface only, and more especially in such parts[pg081] of it as are in a certain stage of decomposition, that they are at all to be distinguished.

As far as we could discover, they consist chiefly of the caryophyllÆ, similar to the radiated species, so common at the falls of Ohio; of the encrinus, but of this our specimens were not so perfect as to enable us to determine the analogy. Numerous other remains were exhibited, but not sufficiently characterized to be referred to their proper places in the system. The top of the cliff, into which this fissure opens, is said to be the favourite haunt of great numbers of birds of prey. This is not improbable, as many hawks and birds of prey always choose high and inaccessible cliffs to build their nests in. We saw about the tops of these rocks, only one pair of hawks, which we took to be of the red-shouldered species, (falco lineatus,) but a heavy rain, which commenced soon after we had ascended, prevented {33} us from procuring a specimen. About the cave, we found some fragments of pottery, arrow points, and other articles of Indian manufacture.

Near Shawaneetown are extensive salt manufactories, at a place heretofore called United States' Saline, affording employment and a source of trade to a part of the inhabitants of that village. Common salt, with the nitrates of lime, potash, &c. occur in great plenty, in connexion with the horizontal limestones and sandstones on the Ohio. Of these we subjoin some account, from the mineralogical report of Mr. Jessup. [048]

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On the 29th of May we passed the mouths of the Cumberland and Tennessee, the two largest rivers, tributary to the Ohio. At the mouth of the Cumberland is a little village called Smithland; where, for a considerable part of the year, such goods are deposited as are designed for Nashville and other places on the Cumberland.

The Cumberland and Tennessee rivers are, for many miles, nearly parallel in direction, and at no great distance apart. Between them are some low sandstone hills; but, we believe, no lofty range of mountains, as has been[pg083] sometimes represented. About these hills, also, in the low ridges north of the Ohio, we found the sandstone, which appears to be the basis rock, often overlaid with extensive beds of a pudding-stone, wherein pebbles of white, yellow, and variously coloured quartz, are united in a cement highly tinged by oxide of iron; extensive fields of compact limestone also occur in the same connexion.

About half way between the mouth of the Cumberland and Tennessee, near the old deserted settlement originally called Smithland,[049] are several large catalpa trees. They[pg084] do not, however, appear to be native; nor have we here, or elsewhere, been able to discover any confirmation of the opinion, that this tree is indigenous to any part of the United States.

It is here called petalfra, which, as well as catalpa, {34} the received appellation, may be a corruption from Catawba, the name of the tribe by whom, according to the suggestion of Mr. Nuttall, the tree may have been introduced. Following the directions of the Pittsburgh navigator,[050] we kept near the left shore, below the Cave Inn; by which means we again ran our boat aground, on a sand-bar, where we spent a considerable part of the night in the most laborious exertions. These were at length crowned with success; and having the boat once more afloat, we proceeded with greater caution.

On the 30th, we arrived at a point a little above the mouth of Cash river, where a town has been laid out, called America.[051] It is on the north bank of the Ohio, about eleven miles from the Mississippi, and occupies the first heights on the former, secure from the inundation of both these rivers (if we except a small area three and a half miles below, where there are three Indian mounds, situated on a tract containing about half an acre above high-water mark). The land on both sides of the Ohio,[pg085] below this place, is subject to be overflowed to various depths, from six to fourteen feet in time of floods; and on the south side, the flat lands extend four or five miles above, separated from the high country by lakes and marshes. The aspect of the country, in and about the town, is rolling or moderately hilly, being the commencement of the high lands between the two rivers above mentioned; below it, however, the land is flat, having the character of the low bottoms of the Ohio. The growth is principally cotton-wood, sycamore, walnut, hickory, maple, oak, &c. The soil is first-rate, and well suited to the cultivation of all products common to a climate of 37 deg. N. lat. From the extensive flat, or bottom, in its neighbourhood, and the heavy growth of timber which here generally prevails, it is probable that the place will be unhealthy, till extensive clearings are made in its vicinity.

This position may be considered as the head of constant {35} navigation for the Mississippi. The Mississippi, from New Orleans to the Ohio, is navigable for boats of the largest size; and America may be considered as the head of constant as well as heavy navigation. Ice is seldom to be found in the Mississippi as low down as the mouth of the Ohio, and never in so large quantities as to oppose any serious obstruction to the navigation.

The navigation of the Ohio has a serious impediment about four and a half miles above the town, occasioned by a limestone bar extending across the river, called the Grand Chain. This bar is impassable in the lowest stage of the water, and will not admit boats of any considerable burden, except in the higher stages.

The Mississippi has, in like manner, two bars, called the Big and Little Chain, which appear to be a continuation[pg086] of the same range of rocks as that in the Ohio, extending across the point of land situated between the two rivers. These bars are situated a little above the Tyawapatia Bottom, about thirty miles above the mouth of the Ohio, and in low water have but a moderate depth of water across them; which, added to the rapidity of the current, occasions a serious obstacle to the navigation.

Boats suited to the navigation of both rivers above the bars here specified, should be of inferior size; those for the Mississippi not exceeding one hundred tons burden, and those for the Ohio from fifty to seventy-five tons.

Any position on the Mississippi in the neighbourhood of the Ohio would be objectionable, for the following reasons:—First, The rapidity of the current, which renders it difficult to find a safe and commodious landing, there being no rocky-bound shore within thirty miles above and a far greater distance below the point. The Iron Banks,[052] seventeen miles below the mouth of the Ohio, have been thought by some an eligible position for the extensive business, {36} which, it is admitted by all, must centre in this neighbourhood. But at this place there is no safe landing; and besides, the banks are composed of layers of sand and clay alternating with each other, of an acclivity nearly perpendicular, and annually wearing away by the current of the river, which sets strongly against them. These banks are elevated about one hundred and thirty feet above the common level of the river, and are insurmountable, except by a circuitous route, leading from the river a considerable distance above and below them. [pg087]

Second, There are no positions on the Mississippi, except the Iron and Chalk Banks, for a great distance below the Ohio, secure from inundation. The bottom directly opposite the mouth of the Ohio, on the west side of the Mississippi is elevated a little above high water; but as it is an alluvial shore, having no permanent foundation, and the banks often falling in, it affords no conveniences or security as a place of business.

Third, No places of anchorage for boats of heavy burden are to be found, except in the main channel of the river, where they would be exposed to drift-wood, great quantities of which are brought down in times of freshet; and when borne along with the rapid current of the river, occasion serious danger to boats lying in its way.

The town of America is almost entirely exempt from any of these objections;—although it has not a rocky foundation, (which may be said of most of the towns on the Ohio,) the current of the river is so gentle, that no such guard against the undermining and wasting away of the banks is required. In case of an excessive flood, or an unusual quantity of floating ice (which may possibly be apprehended in remarkably cold seasons), the mouth of Cash river, five miles below the town, is a harbour in which boats may lie in perfect security.[053]

We would not encourage the idea, that the site {37} now fixed upon as a town is exclusively the point where business[pg088] is to be done; but that the town will eventually extend along on that side of the river about four miles, to the Big Chain above described.

In view of the great extent of inland navigation centring at this place, and the incalculable amount of products to be realized, at no distant period, from the cultivation of the rich vallies and fertile plains of the west, a great proportion of which must find a market here, no doubt can be entertained that it will eventually become a place of as great wealth and importance as almost any in the United States.

In the afternoon of the 30th we arrived at the mouth of the Ohio.

This beautiful river has a course of one thousand and thirty-three miles, through a country surpassed in fertility of soil by none in the United States. Except in high floods, its water is transparent, its current gentle, and nearly uniform. For more than half of its course its banks are high, and its bed gravelly. With the exception of about two miles at the rapids, at Louisville, it has sufficient depth of water, for a part of the year, to float vessels of 300 tons burthen to Cincinnati. The country which it washes may, with propriety, be considered under two divisions. The first, extending from its head at Pittsburgh to the little town of Rockport,[054] about 150 miles below the falls or rapids at Louisville, is hilly. This district forms a portion of one of the sides of that great formation of secondary rocks, which occupies the basin of the Mississippi and its tributaries. This formation, like others of the same period, is rough, with small elevations, which are most[pg089] considerable on its borders, and diminish in proportion as we approach nearer its central parts.

Compact limestone, and sandstone of several varieties, are the rocks which invariably occur along that portion of the Ohio we are now considering. Sandstone of a light gray or ashen colour, of a compact {38} texture, an argillaceous cement, and a slaty or lamellated structure, is the most abundant, and occupies the lowest points which we have hitherto been able to examine. This rock frequently contains alternating beds of coal, bituminous shale, and its accompanying minerals. The beds of compact limestone, which occur in this region, usually rest upon the sandstone just mentioned. Considered as a stratum, its distribution is the reverse of that of the sandstone. It occupies the central and least elevated portions of the formation; and on the borders where the sandstone is most abundant, the limestone is of less extent and of more uncommon occurrence. These remarks are applicable to the hilly district on the upper portion of the Ohio river. From Pittsburgh to Cincinnati, the prospect from the river is that of hills of moderate elevation, sometimes rocky and abrupt, but often sufficiently gradual in their ascent to admit of cultivation to their summits. Their character, as to extent, direction, &c. seems to be determined by the number, direction, and magnitude of the streams which traverse them. They are the remains of what was formerly a continuous and nearly horizontal stratum, with a large deposit of superincumbent soil, which the flowing of water, during the lapse of ages, has channelled and excavated to its present form. These hills diminish in altitude as you approach the falls from above; there they again rise to a height nearly equal to what they attain at the head[pg090] of the river, and from thence gradually diminish, until they disappear, a little above the confluence of the Ohio and Green[055] rivers. Here commences the low country, which extends west to the Mississippi. It is characterized by the great extent of the river alluvion, the increased width and diminished velocity of the stream. The river banks are low, but thickly wooded with sycamore, cotton-wood, river maple, the planera aquatica, cypress, &c. The river hills, which terminate the alluvial district, {39} are distant and low; and it often happens that the surface descends on both sides, from the immediate banks of the river to these hills. Hence, when the waters of the river are sufficiently swollen to flow over its banks, they inundate extensive tracts; from which they cannot return to the channel of the river, and are left stagnant during the summer months, poisoning the atmosphere with noxious exhalations. Many of these inundated tracts have a soil of uncommon fertility, which it is probable will hereafter be recovered from the dominion of the river by dikes or levees.

The beach or sloping part of the immediate bank of the Ohio, throughout its whole extent, is of rather gradual ascent, and covered with timber a considerable distance below high-water mark. The average rapidity of the current of the Ohio is about two and a half miles per hour, and the descent of its surface nine inches per mile, as estimated by Dr. Drake of Cincinnati. The annual inundations happen in the spring. The range between extreme high and low water, in the upper part of the river, is more than 60 feet; but below, where it is not confined by high banks, it is much less. [pg091]

About the falls of Ohio, the cane, (myegia macrosperma of Persoon,) begins to be seen, and increases in quantity thence westward to the Mississippi. The "Cave Inn Rock," or "House of Nature," which we have before mentioned, is an immense cavern penetrating horizontally into a stratum of compact limestone, which forms the river bank for some distance above Golconda in Illinois. Its entrance is a large and regular arch, placed immediately on the brink of the river, and a similar form is preserved in some degree through its whole extent. The Battery Rock is a high mural precipice of the same stratum, running in a straight line, and forming the northern bank of the river which washes its base. The face of this precipice is smooth and naked, and it is surmounted {40} by a heavy growth of timber. This limestone is compact, entirely horizontal in its position, and filled with organic remains. It is traversed by veins containing sulphuret of lead; and at several places near Golconda, this is accompanied by fluat of lime, in beautiful yellow and violet-coloured crystals. Fluat of lime is also found disseminated in small and irregular masses throughout the rock. At Golconda, six miles below the cave, a coarse gray flinty sandstone is found, extending some distance to the west. This rock forms broad hills on the Kentucky side, between the Cumberland and Tennessee rivers; where it abounds in iron ore of several kinds. Perhaps these hills ought to be considered as a spur from the Cumberland hills. At the mouth of the Tennessee river, is a locality of the columnar argillaceous oxide of iron, which rises from the surface in pyramidal and columnar masses, somewhat resembling the cypress knees.

An extensive tract of land between the Tennessee and[pg092] Mississippi rivers, included in the recent purchase from the Cherokees,[056] is rocky and broken, abounding in ores of iron and lead, and probably some other minerals. We have seen a specimen of sulphuret of antimony, in possession of an inhabitant, who being a sort of alchymist, greatly delighting in mystery, thought it imprudent to reveal the secret of its particular locality. It is to be hoped, future and more minute examinations than we had the opportunity of making, may hereafter detect valuable mineral depositions in this tract.

The confluence of the Ohio and Mississippi, is in latitude 37° 22' 9 north, according to the observations of Mr. Ellicott, and in longitude 88° 50' 42 west, from Greenwich.[057] The lands about the junction of these two great rivers are low, consisting of recent alluvion, and covered with dense forests. At the time of our journey, the spring floods having subsided in the Ohio, this quiet and gentle river {41} seemed to be at once swallowed up, and lost in the rapid and turbulent current of the Mississippi. Floods of the Mississippi, happening when the Ohio is low, occasion a reflux of the waters of the latter, perceptible at Fort Massac, more than thirty miles above. It is also asserted, that the floods in the Ohio occasion a retardation in the current of the Mississippi, as far up as the Little Chain, ten miles below Cape Girardeau.[058] The navigation of the Mississippi above the mouth of the Ohio, also that of the Ohio, is usually obstructed for a part of the winter by large masses of floating ice. The boatmen[pg093] observe that soon after the ice from the Ohio enters the Mississippi, it becomes so much heavier by arresting the sands, always mixed with the waters of that river, that it soon sinks to the bottom. After ascending the Mississippi about two miles, we came to an anchor, and went on shore on the eastern side. The forests here are deep and gloomy, swarming with innumerable mosquitoes, and the ground overgrown with enormous nettles. There is no point near the confluence of the Ohio and Mississippi, from which a distant prospect can be had. Standing in view of the junction of these magnificent rivers, meeting almost from opposite extremities of the continent, and each impressed with the peculiar character of the regions from which it descends, we seem to imagine ourselves capable of comprehending at one view all that vast region between the summits of the Alleghanies and of the Rocky Mountains, and feel a degree of impatience at finding all our prospects limited by an inconsiderable extent of low muddy bottom lands, and the unrelieved, unvaried, gloom of the forest.

Finding it necessary to renew the packing of the piston in the steam-engine, which operation would require some time, most of the gentlemen of the {42} party were dispersed on shore in pursuit of their respective objects, or engaged in hunting. Deer, turkeys, and beaver are still found in plenty in the low grounds, along both sides of the Mississippi; but the annoyance of the mosquitoes and nettles preventing the necessary caution and silence in approaching the haunts of these animals, our hunting was without success.

We were gratified to observe many interesting plants, and among them several of the beautiful family of the[pg094] orchidÆ,[059] particularly the orchis spectabile, so common in the mountainous parts of New England.

The progress of our boat against the heavy current of the Mississippi, was of necessity somewhat slow. Steam-boats in ascending are kept as near the shore as the depth of water will admit; and ours often approached so closely as to give such of the party as wished, an opportunity to jump on shore. On the first of June, several gentlemen of the party went on shore, six miles below the settlement of Tyawapatia bottom, and walked up to that place through the woods. They passed several Indian encampments, which appeared to have been recently tenanted. Under one of the wigwams they saw pieces of honey-comb, and several sharpened sticks, that had been used to roast meat upon: on a small tree near by was suspended the lower jaw-bone of a bear. Soon after leaving these they came to another similar camp, where they found a Shawanee Indian and his squaw, with four children, the youngest lashed to a piece of board, and leaned against a tree.

The Indian had recently killed a deer, which they purchased of him for one dollar and fifty cents—one-third more than is usually paid to white hunters. They afterwards met with another encampment, where were several families. These Indians have very little acquaintance with the English language, and appeared reluctant to use the few words they {43} knew. The squaws wore great numbers[pg095] of trinkets, such as silver arm-bands and large earrings. Some of the boys had pieces of lead tied in various parts of the hair. They were encamped near the Mississippi, for the purpose of hunting on the islands. Their village is on Apple Creek, ten miles from Cape Girardeau.

June 2d. As it was only ten miles to Cape Girardeau, and the progress of the boat extremely tedious, several of the party, taking a small supply of provisions, went on shore, intending to walk to that place.

Above the settlement of Tyawapatia, and near Cape À la Bruche,[060] is a ledge of rocks, stretching across the Mississippi, in a direct line, and in low water forming a serious obstacle to the navigation. These rocks are of limestone, and mark the commencement of the hilly country on the Mississippi. Here the landscape begins to have something of the charm of distant perspective. We seem released from the imprisonment of the deep monotonous forest, and can occasionally overlook the broad hills of Apple Creek, and the Au Vaise,[061] or Muddy river of Illinois, diversified with a few scattered plantations, and some small natural meadows. [pg096]

About five miles above Cape Girardeau we found the steam-boat Jefferson, destined for the Missouri. She had been detained some time waiting for castings which were on board the Western Engineer. Several other steam-boats, with stores for the troops about to ascend the Missouri, had entered that river, and were waiting to be overtaken by the Jefferson and the Calhoun, which last we had left at the rapids of the Ohio. On the 3d of June we passed that insular rock in the middle of the Mississippi, called the Grand Tower.[062] It is about one hundred and fifty feet high, and two hundred and fifty in diameter. Between it and the right shore is a {44} channel of about one hundred and fifty yards in width, with a deep and rapid current.

In the summer of 1673, Father Marquette and M. Joliet descended the Mississippi, probably as far as the mouth of the Arkansa. Their narrative contains sufficient evidence that they passed the mouth of the Missouri, the Grand Tower, the mouth of the Ohio, &c. As their work may not be easily accessible to many of our readers, we subjoin, in a note, an interesting passage, in which these objects are mentioned. [063]

[pg097]

The strata of sandstone containing the extensive beds of coal which have been explored, about the Muddy river of Illinois, are here divided transversely by the bed of the Mississippi. The Grand Tower, the precipice opposite the mouth of the Obrazo,[064] containing the singular cavity called the Devil's Oven, the Cornice Rock, and other remarkable cliffs, are monuments indicating the great extent to which the Mississippi has channelled its bed in these strata of horizontal sandstone.

The Grand Tower, from its form and situation, strongly suggests the idea of a work of art. It is not impossible[pg098] that a bridge may be constructed here, for which this rock shall serve as a pier. The shores, on both sides, are of substantial and permanent rocks, which undoubtedly extend across, forming the bed of the river. It is probable, however, that the ledge of rocks called the Two Chains, extending down to Cape À la Bruche, presents greater facilities for the construction of a bridge than this point, as the high lands there approach nearer the river, and are less broken than in the neighbourhood of the Grand Tower. The Ohio would also admit of a bridge at the chains, which appear to be a continuation of the range of rocks here mentioned, crossing that river fifteen miles above its confluence with the Mississippi. We look forward to the time when these great works will be completed.

{45} Compact and sparry limestones are frequent in this region; but all the rocks seem to be acted upon with great rapidity by currents of water. The country on the east side of the Mississippi, back of Fort Chartres, and about the river St. Mary, is much broken by sink holes, having the form of a funnel, and occasioned, probably, by the action of subterraneous streams of water finding their way through the friable sandstones, which underlay the deep and fertile soils in those places. We passed in succession the mouths of the river St. Mary, opposite to which is the fine settlement of the Bois Broule bottoms; the Ocoa, or Kaskaskia river; the St. Lora, a handsome stream, from the west; and the Gabaree Creek, on which stands the old French town of St. Genevieve.[065] The navigation of the[pg099] Mississippi, above the mouth of the Ohio, is at all times difficult. The current is considerably accelerated by the descent of the river over the rocky traverses which cross its bed. At times of low water, innumerable sand-bars occur in various parts of the channel, rendering the navigation extremely precarious.

A little below the mouth of the Kaskaskia, is a creek called the Saline, entering on the west side. A grant of a tract of land, one league square, was here made by the Spanish government, in favour of a Frenchman named Pegreau, the founder of the deserted town called New Bourbon.[066] The tract included a valuable brine spring, near the mouth of the creek. The proprietor built a house near the bank of the Mississippi, where he resided for some time, and carried on a manufacture of salt; but having occasion to go to France, he rented his works to a man, who for want of funds, or for some other reason, failed to keep them in operation. After the transfer of Louisiana to the United States' Government, this grant, among others, became an object of speculation; and advantage being taken of Pegreau's absence, the worthless tenant was instigated {46} to prosecute his landlord for breach of contract, and by a legal process recovered damages to the amount of nine thousand dollars, for the disbursement of which the property was sold, and fell into the hands of the present proprietors.

At the mouth of the Kaskaskia river, on the east bank[pg100] of the Mississippi, a town has been recently commenced, called Portland. The high lands approach here to the brink of the river, affording an elevated and advantageous site. The landing is said to be good; and there is reason to expect that Portland will soon rival the old town of Kaskaskia, the present seat of a great portion of the mercantile business in this part of Illinois.[067]

On the 5th the wind blew from the south-east, and with the aid of sails, we were enabled to ascend the river with considerable rapidity. As we were proceeding briskly forward, our boat struck upon one of those concealed trunks of trees so frequent in the Mississippi, and soon afterwards we discovered that a leak had occurred, which made it necessary for us to lie by. By the constant use of the pumps during the remainder of the day, and the following night, we were able to prevent the water from gaining further upon us; and the next day, having discovered the leak, we raised the stern of the boat, by means of a pair of shears, and succeeded in repairing the injury.

On the beach, opposite the place where we lay by for these repairs, was a large flock of pelicans, which remained in sight for several hours. We had met with some wild geese; and a swan, which we saw was unable to fly, having at that time cast its feathers. The yellow-breasted chat, chuck-wills-widow, the falco haliatus, the kingfisher,[pg101] bank swallow, and numerous other birds, occurred.

At the mouth of the Kaskaskia river, on the east side of the Mississippi, commences the celebrated valley called the American Bottom, extending along {47} the eastern bank of the river last mentioned to the Piasa hills, four miles above the mouth of the Missouri. It is several miles in width, and has a soil of astonishing fertility, consisting of comparatively recent depositions from the river. It has all the disadvantages usually attending tracts of recent river alluvion, the most valuable parts of it being liable to be swept away by the current of the Mississippi, and its surface descending from the brink of the river to the stagnant pools and lagoons, at the outskirts of the valley. But the inexhaustible fertility of its soil makes amends for the insalubrity of the air, and the inconveniences of a flat and marshy situation; and this valley is undoubtedly destined to become one of the most populous parts of America. We were formerly shown here a field that had been cultivated, without manure, one hundred years in succession, and which, when we saw it (in August, 1819) was covered with a very luxuriant growth of corn.

The town of Kaskaskia, the villages of Prairie de Roches, Kahokia, Prairie du Pont, Harrisonville, and Fort Chartres, are situate in this tract. Some of them are in a flourishing condition. Fort Chartres, which was built by the French government, at the expense of one million and a half of dollars, stood near the bank of the river, about twenty miles from Kaskaskia. Not long after they were erected, a part of the works were undermined by the washing of the river; since which time the whole has[pg102] been suffered to remain in ruins, which are now one-fourth of a mile distant from the river.[068]

The country west of the Mississippi, opposite the American Bottom, is of a very different character. The high lands approach the river, presenting abrupt declivities, prominent points, and in many places perpendicular precipices from one to two hundred {48} feet high, frowning over the brink of the river. One of the most remarkable of these is known by the name of the Cornice Rock. It bounds a narrow arm of the river, which has generally sufficient water to admit the passage of boats. The rock extends nearly in a straight line, having a front of about four hundred yards, the brow of the precipice at some points impending over the channel through which boats pass. The rock rises above, to the height of fifty or sixty feet, smoothly rounded by the attrition of the water, which never rising to the upper part of the precipice, leaves that to project in the form of a cornice. Though the lands on the west side of the Mississippi are less fertile than those of the American Bottom, they are of great value, and have long been objects of scandalous speculation.

Among a variety of stratagems, practised in this part of the country to obtain titles to lands, was one which will be[pg103] best explained by the following anecdote, related to us by a respectable citizen of St. Genevieve. Preparatory to taking possession of Louisiana in 1805, the legislature passed a law, authorising a claim to one section of land, in favour of any person who should have actually made improvements, in any part of the same, previous to the year 1804. Commissioners were appointed to settle all claims of this description; more commonly known by the name of improvement rights. A person, somewhere in the county of Cape Girardeau, being desirous of establishing a claim of this kind to a tract of land, adopted the following method:—The time having expired for the establishment of a right, agreeably to the spirit of the law, he took with him two witnesses to the favourite spot, on which he wished to establish his claim, and in their presence marked two trees, standing on opposite sides of a spring; one with the figures 1803, the other 1804, and placed a stalk of growing corn in the spring. He then brought the witnesses before the commissioners, who upon their {49} declaration, that they had seen corn growing at the place specified, in the spring between 1803 and 1804, admitted the claim of the applicant, and gave him a title to the land. In the old district of Cape Girardeau, as in other parts of Louisiana, the difficulty of establishing indisputable titles to the lands, arising out of the great number of Spanish grants, pre-emption, and improvement claims, has greatly retarded the settlement of the country.[069] Establishments were made here more than one hundred and fifty years since; yet the features of the country are little changed, retaining[pg104] the rudeness and gloominess of the original forest.[070]

At five o'clock, on the afternoon of the sixth, we passed the Platteen rock, a perpendicular precipice, not unlike the Cornice rock, near the mouth of a creek of the same name. Along the base of this cliff, we found the water three and sometimes four fathoms deep. In the evening we arrived at Herculaneum, a small village on the west side of the Mississippi, depending principally upon the lead mines for its business.[071]

Here are three shot manufactories, all of them built at the summits of perpendicular precipices; by which means, the expense of erecting high towers has been avoided. Thirty or forty miles to the south-west of Herculaneum, commences the region of the lead mines, which, though not yet satisfactorily explored, is known to extend for many miles through the hilly country, at the sources of the Merameg, the St. Francis, and the other small rivers, rising in the angle between the Mississippi and Missouri, below the mouth of the latter river.

Soon after the cession of Louisiana to the United States, particular care was taken to have all claims to land investigated and registered. Some few {50} may have been omitted, which may be hereafter revived, but these cannot be numerous. In all the recent sales of public lands in the[pg105] western states and territories, liberal reservations have been made for the encouragement of learning. We subjoin some particulars, extracted from a communication of the commissioner of public lands. From this statement, it will be easy to form an idea of the liberal provision made by government, for the future support of schools and colleges. It is probable, similar grants will be made to the Eastern States. [072]

[pg106]

On the 7th, after taking in wood at Herculaneum, we moved up the river; but had scarcely passed the mouth of the Merameg,[073] when we found ourselves unable to stem the heavy current of the Mississippi, on account of the great quantities of mud that had accumulated in the boilers, and prevented our raising the requisite pressure of steam. While we were lying at anchor, to afford the steam engineer an opportunity to clean the boilers, some gentlemen of the party returned along shore to the Merameg, a beautiful river, whose limpid and transparent waters present a striking contrast to the yellow and turbid Mississippi. They were fortunate in meeting with many interesting objects, and, among others, an undescribed mus, which has received, from Mr. Ord, the name of floridanus.[074] [pg107]Upon the specimen, which was a male, was a dilated, glabrous, ventral line, 2¼ inches long. This species is well known in some districts, under the name of large hairy-tailed rat, and is by no means rare in Florida. It is as large as the ordinary stature of the Norway rat, and is equally troublesome. The contents of its stomach were entirely vegetable, consisting of the green bark of trees, and the young shoots of plants. Their nests are large, and are composed of a great quantity of brush. Dr. Baldwin had rarely been able to join in the excursions on shore. Plants were, however, collected and brought to him on board the boat, {51} where he spent much of his time in the examination of such as were interesting or new.[075]

A few rods above our anchoring ground, were two graves, supposed to be those of Indians. One of them was quite recent, and both were covered with heaps of loose stones, probably designed as monuments, and to protect the graves from the ravages of wolves or other animals. The eighth of June brought us to the small village[pg108] of Vide Poche,[076] and the following day to St. Louis, where our arrival was noticed by a salute from a six-pounder on the bank of the river, and the discharge of ordnance on board several of the steam-boats lying in front of the town.