Flagg's The Far West, 1836-1837, part 1. Flagg Edmund

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Flagg's The Far West, 1836-1837, part 1 - Flagg Edmund

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two years subsequent a town was laid off by authority of Congress, and the lots sold as other public lands. Since then it has been gradually becoming the commercial emporium of southern Illinois.

      The buildings, among which are a very conspicuous bank, courthouse, and a land-office for the southern district of Illinois, are scattered along upon a gently elevated bottom, swelling up from the river to the bluffs in the rear, but sometimes submerged. From this latter cause it has formerly been subject to disease; it is now considered healthy; is the chief commercial port in this section of the state, and is the principal point of debarkation for emigrants for the distant West. Twelve miles in its rear are situated the Gallatin Salines, from which the United States obtains some hundred thousands of bushels of salt annually.34 It is manufactured by the evaporation of salt water. This is said to abound over the whole extent of this region, yielding from one eighth to one twelfth of its weight in pure muriate of soda. In many places it bursts forth in perennial springs; but most frequently is obtained by penetrating with the augur a depth of from three to six hundred feet through the solid limestone substratum, when a copper tube is introduced, and the strongly-impregnated fluid gushes violently to the surface. In the vicinity of these salines huge fragments of earthenware, apparently of vessels used in obtaining salt, and bearing the impress of wickerwork, have been thrown up from a considerable depth below the surface. Appearances of the same character exist near Portsmouth, in the State of Ohio, and other places. Their origin is a mystery! the race which formed them is departed!35

      Ohio River.

      IV

      "Who can paint

      Like Nature? Can imagination boast,

      Amid its gay creations, hues like hers?

      Or can it mix them with that matchless skill,

      And lose them in each other, as appears

      In every bud that blooms?"

Thomson.

      "Precipitous, black, jagged rocks,

      For ever shattered, and the same forever."

Coleridge.

      It was near noon of the third day of our passage that we found ourselves in the vicinity of that singular series of massive rock formations, stretching along for miles upon the eastern bank of the stream. The whole vast plain, extending from the Northern Lakes to the mouth of the Ohio, and from the Alleghany slope to the boundless prairies of the far West, is said by geologists to be supported by a bed of horizontal limestone rock, whose deep strata have never been completely pierced, though penetrated many hundred feet by the augur. This limestone is hard, stratified, imbedding innumerable shells of the terebratulæ, encrinites, orthocerites, trilobites, productus, and other species. Throughout most of its whole extent it supports a stratum of bituminous coal, various metals, and saline impregnations: its constant decomposition has fertilized the soil, and its absorbent and cavernous nature has prevented swamps from accumulating upon the surface. Such, in general outline, is this vast limerock substratum of the Western Valley. It generally commences but a few feet below the vegetable deposite; at other places its range is deeper, while at intervals it rises from the surface, and frowns in castellated grandeur over objects beneath. These huge masses of limestone sometimes exhibit the most picturesque and remarkable forms along the banks of the western rivers, and are penetrated in many places by vast caverns. The region we were now approaching was a locality of these singular formations, and for miles before reaching it, as has been remarked, a change in scenery upon the eastern bank is observed. Instead of the rounded wooded summits of the "Ohio hills" sweeping beautifully away in the distance, huge, ponderous rocks, heaped up in ragged masses, "Pelion upon Ossa," are beheld rearing themselves abruptly from the stream, and expanding their Briarean arms in every direction. Some of these cliffs present a uniform, jointed surface, as if of masonry, resembling ancient edifices, and reminding the traveller of the giant ruins of man's creations in another hemisphere, while others appear just on the point of toppling into the river. Among this range of crags is said to hang an iron coffin, suspended, like Mohammed's, between heaven and earth. It contains the remains of a man of singular eccentricity, who, previous to his decease, gave orders that they should be deposited thus; and the gloomy object at the close of the year, when the trees are stripped of their foliage, may be perceived, it is said, high up among the rocks from the deck of the passing steamer. This story probably owes its origin to an event of actual occurrence somewhat similar, at a cliff called by the river-pilots "Hanging Rock."36 It is situated in the vicinity of "Blennerhasset's Island."37 The first of these singular cliffs, called "Battery Rock," stretches along the river-bank for half a mile, presenting a uniform and perpendicular façade upward of eighty feet in height. The appearance is striking, standing, as it does, distinct from anything of a kindred character for miles above and for some distance below. Passing several fine farms, which sweep down to the water's edge, a second range of cliffs are discovered, similar to those described in altitude and aspect; but near the base, through the dark cypresses skirting the water, is perceived the ragged entrance to a large cavernous fissure, penetrating the bluff, and designated by the name of "Rock-Inn-Cave."38 It is said to have received this significant appellation from emigrants, who were accustomed to tarry with their families for weeks at the place when detained by stress of weather, stage of the river, or any other circumstance unfavourable to their progress.

      It was near noon of a beautiful day when the necessary orders for landing were issued to the pilot, and our boat rounded up to the low sand-beach just below this celebrated cavern. As we strolled along the shore beneath "the precipitous, black, jagged rocks" overhanging the winding and broken pathway towards the entrance, we could not but consider its situation wild and rugged enough to please the rifest fancy. The entrance, at first view, is exceedingly imposing; its broad massive forehead beetling over the visiter for some yards before he finds himself within. The mouth of the cavern looks out upon the stream rushing along at the base of the cliff, and is delightfully shaded by a cluster of cypresses, rearing aloft their huge shafts, almost concealed in the luxuriant ivy-leaves clinging to their bark. The entrance is formed into a semi-elliptical arch, springing boldly to the height of forty feet from a heavy bench of rock on either side, and eighty feet in width at the base, throwing over the whole a massive roof of uniform concavity, verging to a point near the centre of the cave. Here may be seen another opening of some size, through which trickles a limpid stream, and forming an entrance to a second chamber, said to be more extensive than that below. The extreme length of this cavern is given by Schoolcraft39 as one hundred and sixty feet, the floor, the roof, and the walls gradually tapering to a point. The rock is a secondary limestone, abounding with testacea and petrifactions, a fine specimen of which I struck from the ledge while the rest of our party were recording their names among the thousand dates and inscriptions with which the walls are defaced.

      Like all other curiosities of Nature, this cavern was, by the Indian tribes, deemed the residence of a Manito40 or spirit, evil or propitious, concerning whom many a wild legend yet lives among their simple-hearted posterity. They never pass this dwelling-place of the divinity without discharging their guns (an ordinary mark of respect), or making some other offering propitiatory of his favour. These tributary acknowledgments, however, are never of much value. The view of the stream from the left bench at the cave's mouth is most beautiful. Immediately in front extends a large and densely-wooded island, known by the name of the Cave, while the soft-gliding waters flow between, furnishing a scene of natural beauty worthy an Inman's pencil; and, if I mistake not, an engraving of the spot has been published, a ferocious-looking personage, pistol in hand, crouched at the entrance, eagerly watching an ascending boat. This design originated, doubtless, in the tradition yet extant, that in the latter part of the last century this cavern was the rendezvous of a notorious band of freebooters which then infested the region, headed by the celebrated Mason,

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<p>34</p>

For a brief statement on the salines, see James's Long's Expedition, in our volume xiv, p. 58, note 11. – Ed.

<p>35</p>

An excellent account of the Mound Builders is given by Lucien Carr in Smithsonian Institution Report, 1891 (Washington, 1893), pp. 503-599; see also Cyrus Thomas, "Report on Mound Explorations" in United States Bureau of Ethnology Report (1890-91). – Ed.

<p>36</p>

Hanging Rock is the name given to a high sandstone escarpment on the right bank of the river, three miles below Ironton, Ohio. – Ed.

<p>37</p>

Blennerhasset's Island is two miles below Parkersburg, West Virginia. For its history, see Cuming's Tour, in our volume iv, p. 129, note 89. – Ed.

<p>38</p>

A brief description of Rock Inn Cave (or Cave-in-Rock) may be found in Cuming's Tour, in our volume iv, p. 273, note 180. – Ed.

<p>39</p>

For Schoolcraft, see Gregg's Commerce of the Prairies, in our volume xx, p. 286, note 178. – Ed.

<p>40</p>

It is a remarkable circumstance, that this term is employed to signify the same thing by all the tribes from the Arkansas to the sources of the Mississippi; and, according to Mackenzie, throughout the Arctic Regions. – Flagg.