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| 0566 |
Southern Tibet : vol.7 |
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the principal bulk of the mighty Kuen-lun.» This view is rather to fall back upon
HUMBOLDT'S and RITTER'S standpoint which had been abandoned some 40 years earlier.¹
Saser-la he says is 17,800 feet high. At its eastern foot he camped on the
Shayok at a place he calls Sirsil. From there he went up on the right bank of
the river. Eight times he had to cross it, but never had more water than to the
saddle, or so as to make the luggage wet. The guides went in front and measured
the depth with poles. Very little snow was seen on the mountains around — as is
usual in the middle of summer. But at some versts from Sirsil, on the right side
of the river, rises the magnificent snow-group Ak-tash, the height of which he estimates
to be 24,000 feet.
Then comes the most interesting passage in his narrative, regarding the Kum-
dan Glaciers:²
From it (Ak-tash) a long but narrow glacier is stretching down in the valley, pro-
viding with water a wild brook, which falls into the Shayok. Some 16 versts beyond it
one finds the colossal glacier Chum-Khumdan, the sources of which are to be found in the
mountains which are situated far to the west. All these glaciers proceed to the very
bottom of the valley, having their lowest edge at a height of 15,300 to 15,700 feet over
the sea. The front edge of Chum-Khumdan has a breadth of about one verst and is broken
off in vertical ice-walls, being 30 to 40 sashen in height. Near its end the glacier represents
an accumulation of colossal ice blocks, some of which have taken extraordinary original
and capricious forms. From under the glacier a brook is streaming, joining with the
river and at some places covered with ice; an ice-covering is also beginning already here
on the Shayok, which from here becomes much smaller.
He camped above the glaciers at a height of 15,800 feet. There is not a
word of any difficulties in passing between the front of the glaciers and the right
bank of the river, and only the next days he went over to the left bank. From
this description we may conclude that the glaciers in 1898 ended at about the same
point as in 1892 as described by GRENARD. It is curious that Novitskiy mentions
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681
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693
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704
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714
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726
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747
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758
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773
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788
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801
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813
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833
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848
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864
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876
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888
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