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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| 0083 |
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
thousand years the climate of those regions has passed
through four successive phases. Up to the first or second
century of our era, it appears to have been distinctly colder
and moister than at present. Then, for several hundred
years, it grew rapidly warmer and drier, until in the fifth
or sixth centuries the desert regions were even more arid
than to-day. During the succeeding mediæval epoch, the
climate again became slightly cooler and moister; while
during modern times, there is a general, though slight
tendency toward aridity. The earliest legend demands a
large lake. Physiographic evidence shows that such a
lake was probably formed during the dry interfluvial epoch
preceding or possibly synchronous with the occupation of
Kashmir by man.
Evidence as to the succeeding epoch is more definite and
more completely harmonious. The legend points to a cold
period, during which Kashmir was not habitable in winter,
and during which the lake that occupied the plain was
drained by the cutting of a deeper channel. Physiography,
as we have seen in the discussion of the paradoxical origin
of lakes, seems to show that if there were a lake larger than
that of to-day, it must have been drained during one of the
moist epochs of which the terraces furnish independent
evidence. In Transcaspia, Persia, and Turkestan, other
lines of research indicate that two thousand or more years
ago the water supply was decidedly larger than now, the
country was colder, and the desert regions were more habit-
able. Putting together all these conclusions, there seems
to be reason for believing that a fluvial epoch, culminating
somewhere in remote antiquity, had not yet wholly passed
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