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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| 0078 |
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
fan-delta deposited by this stream where it enters the narrow
main valley had encroached upon the Jhelum and raised
its level, just as has happened at many other places lower
down — for instance, at Uri, where the front of the fan
was in later times cut off by the river. The process of cut-
ting off the front of the Yaksadara fan, though begun arti-
ficially under the direction of Suyya, probably continued
naturally during later centuries; for the level of the Wular
Lake appears to have fallen steadily, as though the river were
slowly deepening its channel by cutting away the fans and
other material in the bottom of its valley, thus forming a
terrace. In proof of this fall of the lake-level, Stein cites
certain villages which Kalhana, 1148 A. D., seems to indi-
cate as having been actually reclaimed from the lake, and
which Jonajara, circa 1450 A. D., still places on its very
edge, although now they are three miles from its border.
Similarly, Srivara, circa 1480 A. D., speaking of the neigh-
boring villages stretching from Sudarkoth (Sadykoot) to
Andarkoth (Andykoot), places them along the shore of the
lake, although they are now from four to six miles away.
Stein attributes the change in the relation of the villages
to the lake to the building up of the delta of the Jhelum,
where it enters Lake Wular. This cause, however, though
doubtless operative, is inadequate to produce results so
great, especially when it is considered that some of the
marshy regions to the south of the lake away from the delta
have also become drier. The chief cause is probably the
lowering of the level of the lake by the deepening of the
outlet channel — a process which appears to be still in
operation, as may be inferred from the "winding but well-
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