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Scientific Results of a Journey in Central Asia, 1899-1902 : vol.4 |
274 WESTWARDS TO LADAK.
also other beach-lines or rather terraces; but they belong to an older period, when the lakes were larger in consequence of a more abundant inflow of water. At one place only did we observe a few blades of grass growing close in beside the shore; though very near to them were some smaller sand-hills, held together by short, hard
Fig. 171. LOOKING WEST FROM CAMP CXXXIX.
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Fig. 172. LOOKING NORTH FROM CAMP CXXXIX.
grass. This section of the river was also perfectly free from ice, and emptied into a third independent lake-basin, which on the contrary was almost entirely frozen over, except for a few open strips of water in the middle, probably due to the current from above.
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