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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| 0357 |
The Pulse of Asia : vol.1 |
| アジアの鼓動 : vol.1 |
引用情報
OCR読み取り結果
were abandoned, including Rawak, the major part, if not
all, of Dandan-Uilik, Karadong, the Niya River town,
Tuholo, Lulan, and possibly others whose dates are as yet
unknown. At the same time, the great trade route through
Lulan was given up in favor of a longer one. At a later
date, roughly between the ninth and the sixteenth centu-
ries, there appears to have been an epoch of somewhat
more favorable climatic conditions. Choka was built on the
Karatash River; Kenan and Lachinata, as well as Chira
and Gulakhma, flourished lower down on the main stream;
a road existed across the desert north of the present end
of the Keriya River; Bilel Konghan grew up to succeed
Tuholo; and Ying-pen, which appears to have been aban-
doned by its Buddhist builders, was reoccupied by Moham-
medans. During the last few centuries, as the vegetation
shows, there has been again a tendency toward aridity.
If the climatic pulsations outlined above have actually
taken place, the level of Lop-Nor ought to have fluctuated
in harmony with them. Apparently it has done so. The
problem of its fluctuations is complicated, however, by the
fact that the location of the lake has varied in response to
changes in the course of the Tarim River. Hedin, by means
of a careful survey with a transit, has proved that the western
part of the old bed of Lop-Nor contains two slight depres-
sions. One of these, the more southerly, is occupied by the
present lake, which the natives call Kara Koshun. The other
lies just south of Lulan. During the early centuries of the
Christian era, the Tarim River, which then watered Lulan,
discharged into this northern depression. It doubtless filled
it and formed a large lake, which included the other depres-
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