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 |
| Southern Tibet : vol.2 | |
| 南チベット : vol.2 |
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引用情報
1
^,I
RÉSUMÉ OF THE HISTORY OF EFFLUENCE.
183
In the year 1909 abundant rains occurred in Western Tibet, and water began to flow through the channel from the Manasarovar to the Rakas-tai.
The rains were still stronger in 1910, and a >'rushing stream» flowed down through the channel.
In June and July 1911 there was no water in the channel, but in the autumn of the same year water was running from Manasasovar to Rakas-tai. In 1912 and 1913 the channel remained dry. From 1909 to 1911 there was no water flowing out of the Rakas-tai.
In the following table 1 have brought together the above-mentioned material; -I- signifies outflow; — no outflow:
| Year. 1590 | From the Manasarovar. + | From the Rakas-tai. + |
| ? 1625 | + | + |
| 171I | + | + |
| 1715 | + | + |
1717 + +
?1762 + +
1760-65 + +
1770 +
:360628077-8 -4-
.'
79 + ?
179 +
1804 +
181
181
1817-18 + ?
1819 + ?
184 -
1846 +
1848 +
1849 + -
1865
1868
1900 -
1904
1905
1907
1908
1909 +
1910 +
191I +
1912
1913
A glance at this list is sufficient to show how meagre the material is. All the information before 1812 dates from natives, except in 1765, and only from the last
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