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Ch. 6 Sources of Ivory

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QUALITIES OF IVORY              235
This is due to the non-conducting properties of the material, and also to its preservation frozen in ice for many thousand years. In fact, one mammoth was found with skin and flesh so well preserved that it was traced by following the dogs who had eaten of it for years. The first notice of these remains was given by natives in 1799, when the body was probably still nearly or quite intact, but when Adams secured it, in 1806, much of it had been eaten, and the tusks had been removed by a native. In all some dozen remains in this condition have been found in Siberia, the earliest being dis­covered in 1787 in the Alasega River.*
However, only about 15 per cent, of this ivory is of very good quality; some 17 per cent, is fairly good, but the remainder is worthless·! Fossil ivory when scraped emits a fetid odour, due to decomposition and the presence of sulphurated hydrogen gas. Holtzapffel notes the finding in these Siberian fields of a tusk weighing 186 pounds, which was cut up for piano keys.| An interesting circumstance connected with the finding of these fossil remains is that, in 1722, Peter the Great gave orders to the provincial governors of the region to make diligent search to secure a complete skeleton of the extinct mammal.
Mammoth ivory is found along the banks of the streams flowing into Kotzebue Sound, Alaska, more especially the Kowak, Buckland, and Selawik, in Eschscholtz Bay, etc. The deposits, which are uncovered by freshets and the re­cession of ice cliffs, include both teeth and tusks, some of them still in very fair condition, though many are black and hard. Decayed mammoth ivory of a bluish hue is some­times ground up by the Eskimo and used as a pigment for
*Lydekker, "The Royal Natural History." Vol. II, London, 1894, p. 544. fLydekker, op. cit.. Vol. II, p. 545.
{Charles Holtzapffel, "Turning and Mechanical Manipulation," Vol. I, London, 1843, p. 138, note.
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