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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| 0052 |
Southern Tibet : vol.3 |
| 南チベット : vol.3 |
引用情報
OCR読み取り結果
Klaproth shows, not improved the map.¹ Pl. I is a reproduction of this map, which
marks an epoch in European knowledge of Tibet. Here for the first time Eastern
and Southern Tibet have been well placed in relation to Central Asia, Szechuan
and India. The Indo-Chinese rivers come down from a world of Tibetan mountains,
and it can easily be guessed that the upper Tsangpo is situated between two
tremendous systems of mountain ranges. In the west we find the excellent repre-
sentation of the sources of the Tsangpo and the Satlej which has been dealt with
before,² with the only exception of the mistake about the origin of the Ganges.
Central and Northern Tibet, on the other hand, remain unknown, and the Chinese
material d'Anville has had at his disposition has not been sufficient to prevent him
from the supposition that ›Cobi ou Desert de Sable‹ continued without interruption
from Eastern Turkestan to the neighbourhood of Tengri-nor. Western Kwen-lun
and Eastern Kwen-lun are shown as two different mountain systems quite indepen-
dent of each other. Eastern Turkestan is not nearly so good as on RENAT's and
STRAHLENBERG's maps. Yarkand-darya is correctly shown as going the whole
way through the desert to old Lop Nor, but Aksu-darya comes to an end at the
town of the same name. South of Khotan is a Mount Kirian, which is probably
meant to be the Keriya-kotel on the old road between Khotan and Lhasa, to
which we shall have to return later on.
Of great interest is the legend at the end of Hotomni-Solon Mouren or
Khotan-darya: Cette Rivière se perd dans les Sables de ce Desert demême que
plusieurs autres. For if this legend were correct and if it were to be accepted
literally the climate of Eastern Turkestan would be more humid now than in the
days whence d'Anville has drawn his information. At the present epoch Khotan-
darya reaches, as we know, the Tarim during some weeks every summer. Curiously
enough not a single tributary, on d'Anville's map, reaches the main river, except
the Hajitou Mouren. But the latter is the river of Kara-shahr, Khaidu-gol, which
in reality passes the Bagrash-kul on its way. West of Harachar (Kara-shahr) we
recognise some other names, as Couroulac (Korla), Yantac (Yantak-chikke) and
Yanghisar (Yangi-sar). The whole situation of the Yarkand-darya and Khaidu-gol
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487
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527
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539
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550
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563
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575
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587
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599
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610
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