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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| 0242 |
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
creased in size, and new springs appeared lower down in
its bed, as has already been stated. Apparently, in this re-
gion, as in all Central Asia, there was an increase in rainfall
from about 1893 to 1900, between times of lessened precip-
itation. The extraordinary abundance of water at Karakir
was due probably in part to the increased rainfall, but much
more to what may be called an accident. The newly opened
watercourse, so it seems, happened to be located in such
a position that for ten or twelve years, and perhaps to the
time of my visit, the stream continued to deepen its chan-
nel. It maintained its volume by continually penetrating
to and drawing upon new layers of soil lying well below the
level of ground-water, and therefore completely saturated.
The temporary increase in rainfall, culminating in 1900,
seems to be part of one of the periodic variations of climate
which Brückner has shown to take place once in about
thirty-six years in all parts of the world. Such changes
appear competent to explain the minor changes in the vil-
lages and vegetation of the Chira region, for instance the
abandonment of Dumuka at the end of a temporary dry
period in 1841. They cannot explain the broader facts of
the progressive abandonment of cultivated areas and the
death of vegetation from north to south. If the climate of
to-day is like that of the time when the old town north of
Karakir flourished, there is no reason why the vegetation
around the ruins should have been dead for centuries.
To-day, if all the water of Karakir were free to flow as far
as it could, it would not reach the ruins.
On leaving the ruins, we spent a day and a half in traversing
an almost absolutely barren area of reddish or yellowish
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