[81] What explanation the advocates for the doctrine of the recent emersion of our continent will give of the highly and exclusively primitive character of the Rocky Mountains, we are at a loss to conjecture. The organized remains hitherto observed in the secondary aggregates along the base of those mountains, are mostly of animals supposed to have inhabited the depths of the ocean. But if the granite of the Rocky Mountains has been forced up at a recent period, where are the traces of all those older secondary, and fletz rocks, which should have intervened between it and the horizontal sandstones? If these mountains had formed the shores of that ocean, in which the greater part of our continent was so long immersed, after the elevation of the old world, we should have expected to find along their base, the remains of littoral animals, and not of those which inhabited the depths of the ocean. It would be proper, however, before we refer to the character of the Rocky Mountains, as invalidating or confirming any system of opinions, to ascertain that their eastern and western sides are in all respects similar.—James.
[82] Personal Narrative, vol. i. p. 87. American edition.—James.
[83] Pinkerton.—James.
[84] The valley of Red river abounds in limestone, often presenting the shells of oysters and other molluscous animals in a state of petrifaction, scattered in profusion over the surface of the ground, and retaining their original form entire, while on the Arkansa, the rocks are generally sandstone, no limestone being found, except of the Illinois, Grand, and Canadian rivers. Major Long's MS. Journal. Several organic relics from the country about the confluence of the Kiamesha, have been obligingly communicated by Mr. Nuttall: among these is a shell which approaches nearest to the variety of the gryphœa dilatata of Sowerby, 149. fig. 2, but the lobe is far less distinct, and the shell is more narrowed towards the hinge, and is somewhat less dilated, and much more like an ostrea. It may be thus described: G. corrugata, Say.—Small valve, flat, and very much wrinkled, and like the other, narrowed near the hinge. The beak is short, and curved upwards, and laterally, and the sulcus is very distinct. Length, and greatest breadth of the small valve nearly equal; from 1½ to 2 inches. It is in a very perfect state of preservation. Mr. Nuttall brought also from Red river, a species of ostrea, which to the eye appears hardly changed. The anterior portion of the specimens are wanting, but the greatest breadth of the remaining portion of the largest one is nearly three inches. The hinge fosse in this species is proportionably much more contracted, and smaller in every respect, than any other species of the genus we have seen; that of the specimen above mentioned is less than one-half of an inch. The specimens were evidently those of old shells, being much thickened. Another species of ostrea, a hinge fragment of an old and thickened individual, which appears to have been long, and narrow; the hinge fosse itself is long and wide. Length of the hinge more than three inches, greatest width more than one inch.—James.
[85] "A very extensive bed of native argil occurs on the right bank of the Mississippi, commencing near the head of Tiawapeti Bottom, at the Little Chain, about forty miles above the junction of the Ohio and Mississippi, and extending with very little interruption near six miles above the Grand Tower, a distance of thirty-four miles. Beyond these limits I have not observed it. Its colour is snow-white; structure fine, pulverulent; fracture dull earthy. It is amorphous, and adheres to the tongue. It does not effervesce with acids, even in the slightest degree. The bed of argil reposes on horizontal strata of siliceous sandstone, and is overlaid by shell limestone. In the vein of argil, nodules and veins of flint are arranged so as to make with the horizon an angle of about fifty degrees. The argil has been taken to New Orleans, Pittsburgh, St. Louis, &c. in considerable quantities, supposing it to be chalk, for which substance it has been used." Mr. Jessup's MS. Report.
"Flint.—This occurs in nodules and veins in a bed of native argil, above Tiawapeti Bottom. Its colours are bluish-gray and greenish-black. It gives fire with steel; fracture is conchoidal, and the edges are translucent. The veins of flint dip to the south-east." Ibid.
Imbedded in the chalk of Cape Girardeau, are occasionally found nodules of flint, which are enveloped by a hard crust of calcareous carbonate, arranged in concentric layers. Its colour is grayish-black, breaks with a perfectly conchoidal fracture, is translucent on the edges, and readily gives fire with the steel. Schoolcraft's View of the Lead Mines, p. 180.—James.
[86] Jameson in the Edinburgh Encyclopedia, Art. Mineralogy.—James.
[87] Humboldt's Personal Narrative, vol. iv. p. 171. 195. vol. v. p. 553.—James.
[88] Stoddart's Louisiana, p. 391.—James.