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WATER' SYSTEM LAKES UBSA AND KOSO. 95<br />

THE EKTAG ALTAI AND TANNU-OLA RANGES.<br />

Owing to the greater elevation of the Mongolian plains, the southern slopes of<br />

the Altai have a lower relative elevation than those facing northwards. Here, also,<br />

the snow-line is higher, rising to about 8,700 or 9,000 feet, altitudes reached by<br />

few of the northern crests, except in the west on the Kobdo plateau. In this region<br />

of Central Asia the most humid atmospheric currents are those which come from the<br />

nearest marine basin ; that is, from the Polar Sea. Hence the rain-bearing and<br />

fertilising winds blow from the north-east. But these winds discharge their<br />

moisture on the northern slopes of the Altai, so that those facing Mongolia are<br />

mostly destitute of vegetation. In several places the contrast is complete between<br />

the two sides dense forests on the north, mere scrub and brushwood on the south.<br />

The two chief ranges branching from the Altai into Mongolian territory are<br />

the Ektag Altai and the Tannu-ola. The former, sometimes also called the " Great<br />

Altai," runs north-west and south-east parallel with the course of the Black Irtish<br />

and Uluugur. Some of its crests rise above the snow-line, whence the term Ektag,<br />

a dialectic form of the Turki Ak-tagh, or " White Mountains." But the range<br />

is pierced by deep depressions, through which the Russian caravans easily reach<br />

the Kobdo plateau from the Irtish valley. The range itself, as shown by the<br />

recent explorations of Potanin, is continued south-eastwards far beyond the<br />

meridian of Kobdo, after which it trends eastwards under the name of the Altai-<br />

nuru. In this recently discovered section some of the peaks attain an altitude of<br />

10,000 feet, and the Olb'n-daba Pass, crossed by the Kobdo-Barkul route, is no less<br />

than 9,400 feet high.<br />

Farther east other ranges run parallel with the Ektag and Tannu-ola that is,<br />

north-west and south-east ;<br />

but these are everywhere cut up into irregular masses<br />

by erosion. Here is apparently the culminating point of the Altai' system, crossed<br />

by Ney Elias at the Bayan-ingir Pass (over 9,000 feet) on the route from Kobdo<br />

to Biisk. A snowy peak rising immediately north of the pass seemed to this traveller<br />

to have an elevation of 12,000 feet, or 830 more than the Bielukha, highest summit<br />

of the Russian Altai'.<br />

The Tannu-ola, or eastern chain of the Kobdo plateau, stretches far east of the<br />

Altai to the head-streams of the Selenga. Although some of its peaks pass the<br />

snow-line, the Tannu-ola is in many places but slightly elevated above the<br />

surrounding plains. From its base the plateau stretches for 120 miles southwards<br />

to the Khangiii range, above whose wooded slopes several snowy crests are said to<br />

have an elevation of 10,000 feet. Between the Kinghai and the Altai'-uuru the<br />

>t>'ppe has a mean altitude of from 5,000 to 6,000 feet.<br />

WATER SYSTEM LAKES UBSA AND Koso.<br />

All the depressions of ihe plateau comprised in the vast quadrilateral of the<br />

Mongolian Altai' arc occupied by lacustrine basins. One of these is the saline<br />

Ubsa-nor, one of the largest lakes in the Chinese Empire, with an area of at least

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