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Ch. 6 Sources of Ivory

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236 IVORY AND THE ELEPHANT
decorating masks, beluga hats, finger rattles, etc.; in other cases the material is worked up into ladles, spoons, skin scrapers, and the like.*
The group known as the Liakov Islands, the principal ones being Liakov's Island, Moloi, and Kotelnoi, was named by order of Empress Catherine II of Russia, for the dis­coverer, a fur hunter, who landed on one of these islands in 1770. Examination of the soil revealed the presence of enormous deposits of fossil ivory. Subsequent exploration resulted in the discovery of the other islands of this group, all presenting similar conditions. Indeed, to some of these early explorers it almost appeared as though the islands were built up out of these fossil remains. When the ice-covered sand cliffs were thawed by the summer sun, the surface would slip down, bearing along great quantities of mammoth tusks and bones. In 1806 Sirovatskoi discovered the island later known as New Siberia and several others in its vicin­ity. New Siberia proved to be the richest of all these islands of the Arctic Sea in fossil remains, and we learn that, in 1809, 10,000 pounds of fossil ivory was taken thence, while in 1821 the production rose to 20,000 pounds; the supply seemed to be inexhaustible, f It has been noted that the ivory taken in New Siberia is whiter than that from the mainland of Siberia.
Various theories have been advanced to explain the pres­ence of the mammoth remains in such extraordinary abun­dance. It is supposed that geological changes, the sinking of the land, gradually forced these mammals to the higher ground, and finally to the tops of the hills, which had be­come isolated from the mainland as islands. There being little means of subsistence left for the animals, they per-
*Communication of G. T. Emmons, of Princeton, N. J.
fRev. D. Gath Whitley, "The Ivory Islands of the Arctic Ocean," in the Journal of the Transactions of the Victoria Institute, Vol. XLII, pp. 85-57, London, 1910.
*
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