Читать книгу Flagg's The Far West, 1836-1837, part 1 - Flagg Edmund - Страница 9

There are few objects upon the Mississippi in which the geologist and natural philosopher may claim a deeper interest than that singular series of limestone cliffs already alluded to, which, above its junction with the Ohio, present themselves to the traveller all along the Missouri shore. The principal ridge commences a few miles above Ste. Genevieve; and at sunrise one morning we found ourselves beneath a huge battlement of crags, rising precipitously from the river to the height of several hundred feet. Seldom have I gazed upon a scene more eminently imposing than that of these hoary old cliffs, when the midsummer-sun, rushing upward from the eastern horizon, bathed their splintered pinnacles and spires and the rifted tree-tops in a flood of golden effulgence. The scene was not unworthy Walter Scott's graphic description of the view from the Trosachs of Loch Katrine, in the "Lady of the Lake:"

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All of these precipices, not less than those on the Ohio, betray palpable indication of having once been swept by the stream; and the fantastic excavations and cavernous fissures which their bold escarpments expose would indicate a current far more furious and headstrong than that, resistless though it be, which now rolls at their base. The idea receives confirmation from the circumstance that opposite extends the broad American Bottom, whose alluvial character is undisputed. This tract once constituted our western border, whence the name.

The bluffs of Selma and Herculaneum are distinguished for their beauty and grandeur, not less than for the practical utility to which they have been made subservient. Both places are great depositories of lead from the mines of the interior, and all along their cliffs, for miles, upon every eligible point, are erected tall towers for the manufacture of shot. Their appearance in distant view is singularly picturesque, perched lightly upon the pinnacles of towering cliffs, beetling over the flood, which rushes along two hundred feet below. Some of these shot manufactories have been in operation for nearly thirty years.68 Herculaneum has long been celebrated for those in her vicinity. The situation of the town is the mouth of Joachim Creek; and the singular gap at this point has been aptly compared to an enormous door, thrown open in the cliffs for the passage of its waters. A few miles west of this village is said to exist a great natural curiosity, in shape of a huge rock of limestone, some hundred feet in length, and about fifty feet high. This rock is completely honeycombed with perforations, and has the appearance of having been pierced by the mytilus or some other marine insect.

A few miles above Herculaneum comes in the Platine Creek;69 and here commence the "Cornice Rocks," a magnificent escarpment of castellated cliffs some two or three hundred feet in perpendicular altitude from the bed of the stream, and extending along the western bank a distance of eight or ten miles. Through the façade of these bluffs pours in the tribute of the Merrimac, a bright, sparkling, beautiful stream.70 This river is so clear and limpid that it was long supposed to glide over sands of silver; but the idea has been abandoned, and given place to the certainty of an abundant store of lead, and iron, and salt upon its banks, while its source is shaded by extensive forests of the white pine, a material in this section of country almost, if not quite, as valuable.71 Ancient works of various forms are also found upon the banks of the Merrimac. There is an immense cemetery near the village of Fenton, containing thousands of graves of a pigmy size, the largest not exceeding four feet in length. This cemetery is now enclosed and cultivated, so that the graves are no longer visible; but, previous to this, it is said that headstones were to be seen bearing unintelligible hieroglyphical inscriptions.72 Human remains, ancient pottery, arrow-heads, and stone axes are daily thrown up by the ploughshare, while the numerous mounds in the vicinity are literally composed of the same materials. Mammoth bones, such as those discovered on the Ohio and in the state of New-York, are said also to have been found at a salt-lick near this stream.

It was a bright morning, on the fifth day of an exceedingly long passage, that we found ourselves approaching St. Louis. At about noon we were gliding beneath the broad ensign floating from the flagstaff of Jefferson Barracks.73 The sun was gloriously bright; the soft summer wind was rippling the waters, and the clear cerulean of the heavens was imaged in their depths. The site of the quadrangle of the barracks enclosing the parade is the broad summit of a noble bluff, swelling up from the water, while the outbuildings are scattered picturesquely along the interval beneath; the view from the steamer cannot but strike the traveller as one of much scenic beauty. Passing the venerable village of Carondelet, with its whitewashed cottages crumbling with years, and old Cahokia buried in the forests on the opposite bank, the gray walls of the Arsenal next stood out before us in the rear of its beautiful esplanade.74 A fine quay is erected upon the river in front, and the extensive grounds are enclosed by a wall of stone. Sweeping onward, the lofty spire and dusky walls of St. Louis Cathedral, on rounding a river bend, opened upon the eye, the gilded crucifix gleaming in the sunlight from its lofty summit; and then the glittering cupolas and church domes, and the fresh aspect of private residences, mingling with the bright foliage of forest-trees interspersed, all swelling gently from the water's edge, recalled vividly the beautiful "Mistress of the North," as my eye has often lingered upon her from her magnificent bay. A few more spires, and the illusion would be perfect. For beauty of outline in distant view, St. Louis is deservedly famed. The extended range of limestone warehouses circling the shore give to the city a grandeur of aspect, as approached from the water, not often beheld; while the dense-rolling forest-tops stretching away in the rear, the sharp outline of the towers and roofs against the western sky, and the funereal grove of steamboat-pipes lining the quay, altogether make up a combination of features novel and picturesque. As we approached the landing all the uproar and confusion of a steamboat port was before us, and our own arrival added to the bustle.

And now, perchance, having escaped the manifold perils of sawyer and snag, planter, wreck-heap, and sand-bar, it may not be unbecoming in me, like an hundred other tourists, to gather up a votive offering, and – if classic allusion be permissible on the waters of the wilderness West – hang it up before the shrine of the "Father of Floods."

It is surely no misnomer that this giant stream has been styled the "eternal river," the "terrible Mississippi;"75 for we may find none other imbodying so many elements of the fearful and the sublime. In the wild rice-lakes of the far frozen north, amid a solitude broken only by the shrill clang of the myriad water-fowls, is its home. Gushing out from its fountains clear as the air-bell, it sparkles over the white pebbly sand-beds, and, breaking over the beautiful falls of the "Laughing Water,"76 it takes up its majestic march to the distant deep. Rolling onward through the shades of magnificent forests, and hoary, castellated cliffs, and beautiful meadows, its volume is swollen as it advances, until it receives to its bosom a tributary, a rival, a conqueror, which has roamed three thousand miles for the meeting, and its original features are lost for ever. Its beauty is merged in sublimity! Pouring along in its deep bed the heaped-up waters of streams which drain the broadest valley on the globe; sweeping onward in a boiling mass, furious, turbid, always dangerous; tearing away, from time to time, its deep banks, with their giant colonnades of living verdure, and then, with the stern despotism of a conqueror, flinging them aside again; governed by no principle but its own lawless will, the dark majesty of its features summons up an emotion of the sublime which defies contrast or parallel. And then, when we think of its far, lonely course, journeying onward in proud, dread, solitary grandeur, through forests dusk with the lapse of centuries, pouring out the ice and snows of arctic lands through every temperature of clime, till at last it heaves free its mighty bosom beneath the Line, we are forced to yield up ourselves in uncontrolled admiration of its gloomy magnificence. And its dark, mysterious history, too; those fearful scenes of which it has alone been the witness; the venerable tombs of a race departed which shadow its waters; the savage tribes that yet roam its forests; the germes of civilization expanding upon its borders; and the deep solitudes, untrodden by man, through which it rolls, all conspire to throng the fancy. Ages on ages and cycles upon cycles have rolled away; wave after wave has swept the broad fields of the Old World; an hundred generations have arisen from the cradle and flourished in their freshness, and, like autumn leaflets, have withered in the tomb; and the Pharaohs and the Ptolemies, the Cæsars and the Caliphs, have thundered over the nations and passed away; and here, amid these terrible solitudes, in the stern majesty of loneliness, and power, and pride, have rolled onward these deep waters to their destiny!

There is, perhaps, no stream which presents a greater variety of feature than the Mississippi, or phenomena of deeper interest, whether we regard the soil, productions, and climate of its valley, its individual character and that of its tributaries, or the outline of its scenery and course. The confluents of this vast stream are numerous, and each one brings a tribute of the soil through which it has roamed. The Missouri pours out its waters heavily charged with the marl of the Rocky Mountains, the saffron sands of the Yellow Stone, and the chalk of the White River; the Ohio holds in its floods the vegetable mould of the Alleghanies, and the Arkansas and Red Rivers bring in the deep-died alluvion of their banks. Each tributary mingles the spoils of its native hills with the general flood. And yet, after the contributions of so many streams, the remarkable fact is observed that its breadth and volume seem rather diminished than increased.77 Above the embouchure of the Missouri, fifteen hundred miles from the Mexican gulf, it is broader than at New-Orleans, with scarce one tenth of its waters; and at the foot of St. Anthony's Falls its breadth is but one third less. This forms a striking characteristic of the Western rivers, and owes, perhaps, its origin partially to the turbid character of their waters: as they approach their outlet they augment in volume, and depth, and impetuosity of current, but contract their expanse. None, however, exhibit these features so strikingly as the grand central stream; and while, for its body of water, it is the narrowest stream known, it is charged with heavier solutions and has broader alluvions than any other. The depth of the stream is constantly varying. At New-Orleans it exceeds one hundred feet. Its width is from half of one mile to two miles; the breadth of its valley from six miles to sixty; the rapidity of its current from two miles to four; its mean descent six inches in a mile, and its annual floods vary from twelve feet to sixty, commencing in March and ending in May. Thus much for Statistics.

Below its confluence with its turbid tributary, the Mississippi, as has been observed, is no longer the clear, pure, limpid stream, gushing forth from the wreathy snows of the Northwest; but it whirls along against its ragged banks a resistless volume of heavy, sweeping floods, and its aspect of placid magnificence is beheld no more. The turbid torrent heaves onward, wavering from side to side like a living creature, as if to overleap its bounds; rolling along in a deep-cut race-path, through a vast expanse of lowland meadow, from whose exhaustless mould are reared aloft those enormous shafts shrouded in the fresh emerald of their tasselled parasites, for which its alluvial bottoms are so famous. And yet the valley of the "endless river" cannot be deemed heavily timbered when contrasted with the forested hills of the Ohio. The sycamore, the elm, the linden, the cotton-wood, the cypress, and other trees of deciduous foliage, may attain a greater diameter, but the huge trunks are more sparse and more isolated in recurrence.

But one of the most striking phenomena of the Mississippi, in common with all the Western rivers, and one which distinguishes them from those which disembogue their waters into the Atlantic, is the uniformity of its meanderings. The river, in its onward course, makes a semicircular sweep almost with the precision of a compass, and then is precipitated diagonally athwart its channel to a curve of equal regularity upon the opposite shore. The deepest channel and most rapid current is said to exist in the bend; and thus the stream generally infringes upon the bend-side, and throws up a sandbar on the shore opposite. So constantly do these sinuosities recur, that there are said to be but three reaches of any extent between the confluence of the Ohio and the Gulf, and so uniform that the boatmen and Indians have been accustomed to estimate their progress by the number of bends rather than by the number of miles. One of the sweeps of the Missouri is said to include a distance of forty miles in its curve, and a circuit of half that distance is not uncommon. Sometimes a "cut-off," in the parlance of the watermen, is produced at these bends, where the stream, in its headlong course, has burst through the narrow neck of the peninsula, around which it once circled. At a point called the "Grand Cut-off," steamers now pass through an isthmus of less than one mile, where formerly was required a circuit of twenty. The current, in its more furious stages, often tears up islands from the bed of the river, removes sandbars and points, and sweeps off whole acres of alluvion with their superincumbent forests. In the season of flood the settlers, in their log-cabins along the banks, are often startled from their sleep by the deep, sullen crash of a "land-slip," as such removals are called.

The scenery of the Mississippi, below its confluence with the Missouri, is, as has been remarked, too sublime for beauty; and yet there is not a little of the picturesque in the views which meet the eye along the banks. Towns and settlements of greater or less extent appear at frequent intervals; and then the lowly log-hut of the pioneer is not to be passed without notice, standing beneath the tall, branchless columns of the girdled forest-trees, with its luxuriant maize-fields sweeping away in the rear. One of these humble habitations of the wilderness we reached, I remember, one evening near twilight; and while our boat was delayed at the woodyard, I strolled up from the shore to the gateway, and entered easily into confabulation with a pretty, slatternly-looking female, with a brood of mushroom, flaxen-haired urchins at her apron-string, and an infant at the breast very quietly receiving his supper. On inquiry I learned that eighteen years had seen the good woman a denizen of the wilderness; that all the responsibilities appertained unto herself, and that her "man" was proprietor of some thousand acres of bottom in the vicinity. Subsequently I was informed that the worthy woodcutter could be valued at not less than one hundred thousand! yet, en verite, reader mine, I do asseverate that my latent sympathies were not slightly roused at the first introduction, because of the seeming poverty of the dirty cabin and its dirtier mistress!

St. Louis.