John T. Bealby and Peter A. Kropotkin

Summary

John T. Bealby and Peter A. Kropotkin 1911 Encyclopædia Britannica (1911)

Beyond these schists rises a broken wall of limestone, cleft to the base by gorges, through which flow the mountain torrents, and capped by pale precipitous battlements, which face the central chain at a height of 11,000 to 12,000 ft. Beyond, again, lies a broad furrow, or ‘longitudinal fold,’ as geologists call it, parallel to the ridges, and then rises the last elevation, a belt of low calcareous hills, on which, here and there among the waves of beech forest, purple or blue with distance, a white cliff retains its local colour and shines like a patch of fresh snow.
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John T. Bealby and Peter A. Kropotkin 1911 Encyclopædia Britannica (1911)

The distinctive animal of the Pamir plateau is the magnificent Ovis poli (conjectured to be the ancestor of the common sheep) . In the alpine tracts of the Tian-shan, on the borders of the Pamir, their horns and skulls are frequently met with, but there the place of the species is now taken by Ovis karelini. The wild horse, which occurred in Poland a few centuries ago, was discovered by Prezhevalsky in the highlands of Dzungaria. The wild camel inhabits the lonely plateaus south of the Ala-shan. The other mammals of Turkestan are mostly those which are met with elsewhere in north Asia.
Source: Wikisource

John T. Bealby and Peter A. Kropotkin 1911 Encyclopædia Britannica (1911)

Since the theory of geological cataclysms was abandoned, and that of slow modifications of the crust of the earth accepted, new data have been obtained in the Aral-Caspian region to show that the rate of modification after the close of the Glacial period, although still very slow, was faster than had been supposed from the evidence of similar changes now going on in Europe and America. The effects produced by desiccating agencies are beyond all comparison more powerful than those which result from the earthquakes that are so frequent in Turkestan.
Source: Wikisource

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