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Between the Ohio and the Great Lakes, directly north of the Appalachian confederacies, and separated from them by the unpeopled wilderness now forming the States of Tennessee and Kentucky, dwelt another set of Indian tribes.

Let us now turn to another highland only the northern part of which was glaciated. The Appalachian highland, the second great division of North America, consists of three parallel bands which extend southwestward from Newfoundland and the St. Lawrence River to Georgia and Alabama.

Again, as during the Triassic, a warping of the crust formed a long trough parallel to the coast and to the Appalachian ridges, but cut off from the sea; and here the continental deposits of the early Cretaceous were laid.

Even as regards the seaports, the currents of trade were too thin and divergent to permit of large urban concentration, for the Appalachian water-shed shut off the Atlantic ports from the commerce of the central basin; and even the ambitious construction of railroads to the northwest, fostered by the seaboard cities, merely enabled the Piedmont planters to get their provisions overland, and barely affected the volume of the seaboard trade.

From Gaspe, the southeastern promontory at the entrance of the Gulf, the younger rocks of the Appalachian range, constituting the breast-bone of the continent, and culminating at the north in the White Mountains, describe a great curve southwesterly to the valley of the Hudson; and it is between the ridge-like elevations of this range and the older Laurentian Hills that we find the valley of the St.

THE MISSISSIPPIAN SERIES. In the interior the Mississippian is composed chiefly of limestones, with some shales, which tell of a clear, warm, epicontinental sea swarming with crinoids, corals, and shells, and occasionally clouded with silt from the land. In the eastern region, New York had been added by uplift to the Appalachian land which now was united to the northern area.

To escape from the persecutions of the aristocracy, many of the Regulators and their friends crossed the Appalachian Mountains and built their cabins in the Watauga region. Here, in 1772, there was established by these "rebels" the first republic in America, based upon a written constitution "the first ever adopted by a community of American-born freemen."

Fifth, another division has been organized for the study of the areal, structural, and historical geology of the Appalachian region, extending from the Atlantic, westward, to the zone which separates the mountain region from the great valley of the Mississippi. Mr. G.K. Gilbert has charge of this work, and has a large corps of assistants.

To the northward were Cade's Cove and the vale of Tuckaleechee, with Chilhowee in the near distance, and the Appalachian Valley stretching beyond our ramparts to where the far Cumberlands marked an ever-blue horizon. What matter that the plenteous roughs about us were branded with rude or opprobrious names?

These wars were really slave raids to make the Indians give up the Negro and half-breed slaves domiciled among them. The wars cost the United States ten million dollars and two thousand lives. The great Appalachian range, with its abutting mountains, was the safest path northward.