Peter Kropotkin and Charles Norton Edgcumbe Eliot

Summary

Peter Kropotkin and Charles Norton Edgcumbe Eliot 1911 Encyclopædia Britannica (1911)

The climate is so dry, and the rains are so scarce, that an absence of forests and Alpine meadows is characteristic of the ridge; but when heavy rain falls simultaneously with the melting of the snows in the mountains, the watercourses become filled with furious torrents, which create great havoc. The main glaciers (12) are on the north slope, but none creeps below 10,000 to 12,000 ft. The Peter the Great range, or Periokh-tau, in Karateghin, south of the valley of the Vakhsh, runs west-south-west to east-north-east for about 130 m., and is higher than the Hissar range.
Source: Wikisource

Peter Kropotkin and Charles Norton Edgcumbe Eliot 1911 Encyclopædia Britannica (1911)

Trade has been greatly promoted by the building of the Transcaspian railway across the country (from Charjui on the Oxus to Kati-kurgan) in 1886–1888. The exports to Russia consist of raw cotton and silk, lamb-skins, fruits and carpets, and the imports of manufactured goods and sugar. The imports from India are cottons, tea, shawls and indigo. There are very few roads; goods are transported on camels, or on horses and donkeys in the hilly tracts.
Bokhara has for ages been looked upon as the centre of Mussulman erudition in central Asia.
Source: Wikisource

Peter Kropotkin and Charles Norton Edgcumbe Eliot 1911 Encyclopædia Britannica (1911)

The climate of Bokhara is extreme. In the lowlands a very hot summer is followed by a short but cold winter, during which a frost of −20° Fahr. may set in, and the Oxus may freeze for a fortnight. In the highlands this hot and dry summer is followed by four months of winter; and, finally, in the regions above 8000 ft. there is a great development of snowfields and glaciers, the passes are buried under snow, and the short summer is rainy. The lowlands are sometimes visited by terrible sand-storms from the west, which exhaust men and kill the cotton trees.
Source: Wikisource

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