IIIFカラー高解像度
国立情報学研究所 - ディジタル・シルクロード・プロジェクト
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| IIIFカラー高解像度 |
| Scientific Results of a Journey in Central Asia, 1899-1902 : vol.1 | |
| 1899-1902年の中央アジア旅行における科学的成果 : vol.1 |
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| 湖を埋め立てている沖積物Fluvial sediment filling up a lake | |
| 現在のソゴトとカサン・シンディのボルジェマル。THE BOLDSCHEMALS OF SOGOT AND KASAN-SINDI AT THE PRESENT TIME. | |
| カサン・シンディ湖が独立して切り離された時のタリム川の水路。COURSE OF TARIM WHEN KASAN-SINDI ALONE WAS ABANDONED. |
引用情報
FROM AJAGH-ARGHAN TO JURT-TSCHAPGHAN. 205
flows the water of the Kontsche-darja. The formative significance of this relation I shall discuss at a later stage, though it seemed not inexpedient to direct attention here to the existence of this hydrographie homology, as well as to the function which these lakes discharge as receptacles for the fluvial sediment. The water, when it enters them at (a), is muddy; but when it leaves them at (b), it is clear. The sediment settles on the lake-bottom; though when the lake gets filled, the water at (b) is likewise muddy.
~a
b
Fig. 17o.
CHAPTER XV.
FROM AJAGH—ARGHAN TO JURT—TSCHAPGHAN.
On 5th June we continued our drift down the Tschong-tarim, with a flood of 55 cub.m. in the second. Shortly after starting we passed two abandoned loops, Sogot on the left and Kasan-sindi on the right. Both still contained water, although the natives told me these boldschemals were abandoned some ten or twelve years ago. At the present time the river flows pretty evenly between them both. As
Fig. 171. THE BOLDSCHEMALS OF SOGOT Fig. 172. COURSE OF TARIM WHEN
AND KASAN-SINDI AT THE PRESENT TIME. KASAN-SINDI ALONE WAS ABANDONED.
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