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
『東洋文庫所蔵』貴重書デジタルアーカイブ
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| 0204 |
Southern Tibet : vol.2 |
| 南チベット : vol.2 |
引用情報
OCR読み取り結果
The fact that water had begun to stream, in 1910, from the Manasarovar
to the Rakas-tal, proves that one link in the chain had been joined again, and that
only one interruption existed, namely, between the Rakas-tal and the Tirtapuri Satlej.
In the late autumn of 1913 I received a new letter from Gulam Rasul, in which
he informed me that he had sent a reliable man to have a look at the two lakes
and the brook. This man returned to Leh about the middle of October and on
the 20th of October, 1913, Gulam Rasul wrote a letter to me, containing the follow-
ing information:
I. In 1911 there was a lot of rain in Chang-thang, by cause of which the water of
Mawang-Thhso ran into the Langag-Thhso through the way of Gang-gi Grogpo.
II. There was no rain in Chang-thang in 1912. By that reason the two lakes not
joined together as in 1911. And there was no good grass produced in the surroundings.
III. In 1913 there was only a little rain in the beginning of summer, and there was a
good deal of rain in the end of summer, but Mawang has not got any chance in this year to
go and meet with Langag, and Gang-gi Grogpo was dried and empty.
IV. The western lake, Langag-Thhso, does never flow into the Tretapuri-Satlaj.
According to this latest information the links in the chain are again isolated
from each other. Even the considerable rains in the late summer of 1913 were
not sufficient to give rise to an effluence from the Manasarovar.
I have not been able to trace the hydrographical pulsations of 1914 and 1915,
as the war has interrupted my correspondence with Gulam Rasul.
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51
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73
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83
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95
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109
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121
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132
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144
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155
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167
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177
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269
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279
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289
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305
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323
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334
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345
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356
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367
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381
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393
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403
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428
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445
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461
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473
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487
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503
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517
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532
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