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the village of Abdalli, close to its mouth in Lob-nor,<br />

LOB-NOR. 63<br />

it is little more than 2 feet<br />

per second, and the discharge may here be estimated at about 2,700 cubic feet. At<br />

Abdalli the Tarim emerges from the reedy swamps of Lake Kara-buran, or " Black<br />

Storm," which belongs to the Lob-nor system. But here it is again divided into a<br />

number of natural and artificial canals, beyond which it disappears in a forest of<br />

reeds even more dense and taller than those of the Kara-burun, rising to a height<br />

of over 20 feet above the surface, and partly concealing from view the Chok-kul<br />

(Great Lake), or Kara-kurchin, which jointly with the Kara-buran forms the great<br />

reservoir commonly known as the Lob-nor. The eastern section covers an area of<br />

perhaps 800 square miles ; but it is little mostly more than a lagoon or flooded<br />

morass, with a mean depth of scarcely more than 7 feet along its southern or more<br />

elevated bank. Even in the centre a few fishing villages lie hidden amid the<br />

Fig.<br />

23. LAKE KAUASUAK.<br />

Scale 1 : 1,230,000.<br />

L of G. 8630 87" 30'<br />

, 30<br />

Miles.<br />

dense reeds overgrowing a strip of land which here rises above the surface. These<br />

villages are thus protected from the fierce gales from the east and north-east,<br />

which sweep the lake and open plains, especially in spring, and which cause the<br />

water to flood the flat shores of the Kara-buran for a space of 10 or 12 miles;<br />

hence its expressive name, the " Black Storm."<br />

Lake Lob is evidently a mere remnant of the ancient " Mediterranean " men-<br />

tioned in legend and historic records, and traces of which are clearly detected<br />

throughout the whole Tarim depression eastwards to the Mongolian plateaux. The<br />

researches of Richthofon enable us accurately to define the contours of what was<br />

once the Si-hai, or " Western Sen," and what is now the " Ilan-hai," or " Dried-up<br />

Sea," of the Chinese. This ancient sea, running parallel<br />

with the Tian-shan and<br />

Kuon-lun, is now known to have covered an area of over 800,000 square miles,<br />

with a depth of at least 3,000 feet in its lowest depression ; that is, where the

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