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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| 0094 |
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
rienced in bringing water to the places where it is wanted
is enormous. At Hardus, for instance, on the Dras River
near the mouth of the Suru, we saw that a mountain stream
had been diverted into a little canal and carried along the
precipitous side of the valley for three or four miles at a
height of over a thousand feet above the river. Far below,
in some characteristically rocky fields, irrigated from an-
other canal, women with baskets slung on their backs were
laboriously gathering the stones which had worked up dur-
ing the winter.
The glacial features of the upper part of the valley and
the terraces of the middle both appear to owe their origin
to the great series of climatic changes of which we have al-
ready found evidence in Kashmir. It is difficult to assign
any date to the later changes on the basis of local evidence.
The general freedom of the fronts of the glaciers among the
lofty mountains from large amounts of detritus and the
withdrawal of some of them from their moraines show that
the glaciers are on the whole diminishing in size; this sug-
gests that the climate is becoming warmer or drier. Work-
man, however, mentions the case of one glacier which has
recently advanced, though the advance may be only tem-
porary. He also mentions finding large trees lying dead at
a height greater than that where even stunted trees now
grow. Probably the trees are relics of the dry epoch dur-
ing the first half of the Christian era, but this has not been
proved. West of the pass of Fotu La, I later saw, at an ele-
vation of 12,400 feet, the ruins of a village which was said to
have been abandoned a few years ago because its springs
dried up — another suggestion of change of climate. The
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