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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| 0454 |
Ruins of Desert Cathay : vol.2 |
| 中国砂漠地帯の遺跡 : vol.2 |
引用情報
OCR読み取り結果
a small amphitheatre, and an ascent of 1000 feet over steep
Alpine meadows brought us to a grassy plateau known
as Pan-t'o-pa. On its edge rose a watch-tower, built of
stamped clay with a wooden framework and similar in size
and construction to the watch-towers familiar to me from
the desert Limes. But what a change in the surround-
ings! Clay and woodwork both looked much decayed;
but with climatic conditions so different from those of the
plains no estimate of date could be hazarded.
Only one thing seemed clear. This tower and an
exactly similar one on the pass itself, together with the
little fort of which I found traces on the Chio-po-chia Pass
beyond, plainly proved that inroads had been feared from
these mountains. Who were the people who once threatened
the low lands from the now uninhabited valleys of the Nan-
shan? I thought of the 'Little Yüeh-chih,' remnants of an
ancient nomad race, who are mentioned in these mountains
by later Chinese records down to the tenth century A.D.
They are said to have been left behind here when their
kindred, the 'Great Yüeh-chih,' who under the name of
Indo-Scythians were destined to become the rulers of the
Oxus region and the Indian North-West, were forced by
Hun aggression in the second century B.C. to start on
their great migration westwards. If only the snowy peaks
which have ever looked down on these valleys and plains
could tell us the story!
The distance across the plateau to the Hou-tzŭ Pass
southward was only three-quarters of a mile; yet, small as
it was, it brought a surprise. A stream which came down
from a snow-capped peak on the right disappeared before
my eyes in a boulder-filled basin enclosed by grassy slopes
on all sides. Its water, no doubt, finds an underground
passage into the Chin-fo-ssŭ valley below. As soon as I
had reached the pass itself, about 11,350 feet high by the
aneroid, the same curious topographical feature presented
itself on a larger scale. Below a beautiful semicircle of
snowy peaks rising in the centre to close on 9000 feet
there extended a large level basin to the south foot of the
pass (Fig. 232).
At first glance it might have been taken for a lake;
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32
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43
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53
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142
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155
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166
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188
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199
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210
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231
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245
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279
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293
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308
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319
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332
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359
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382
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395
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407
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419
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431
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442
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452
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454
455
457
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465
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478
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491
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505
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518
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529
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540
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553
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567
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581
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594
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605
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617
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629
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642
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657
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670
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683
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696
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709
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723
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736
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749
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760
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771
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783
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793
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803
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813
814
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