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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| 0152 |
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
steeply sloping piedmont region of coarse gravel, and
reaches the flatter region of fine sand and impervious
clay, it approaches the surface, or rather the surface ap-
proaches it, until finally, near the end of the last fine gravels,
the ground becomes permanently damp close to the sur-
face. The phenomenon is the same as the so-called spring-
line in northern Italy, where the water from the Alps, after
flowing underground through piedmont gravels, forms a
line of springs. In the Lop basin, where the surface of the
ground becomes damp, an abundant growth of vegetation,
chiefly reeds, tamarisks, and poplars, is able to flourish
without the help of rain. The zone of vegetation thus formed
varies in width from nearly twenty miles between Khotan
and Keriya, to a few hundred yards at the eastern end of
Lop-Nor, but its character is everywhere much the same.
It is unmistakable along the entire south side of the basin
for nearly a thousand miles, and is almost equally continu-
ous, I believe, on the north side, though there it is much
less noticeable because its location is almost coincident with
that of the similar zone of vegetation of the eccentrically
placed Tarim River. The only part of the basin where the
zone cannot be detected is the northeast corner, which is
exceptional in many other ways also. Most of the towns
of the Lop basin are located in the zone of vegetation;
the chief roads follow it, and from the point of view of
geography or the relation of the organic to the inorganic,
it is the most important feature of the country.
The areas of sand and lacustrine deposits comprised in
the central plain are notable as examples of the kinds of
regions not adapted to life of any form. They are more
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