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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| 0489 |
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
the wide marshy expanse at its foot, and the size of its
glaciers, made the view truly imposing. Behind this
great semicircle of snows, for which the Russian travellers
Roborowsky and Kozloff heard the Mongol name of
Shagolin-Namjil, lie the drainage of Lake Kokonor and
the confines of north-eastern Tibet. But I knew well
that my plans could not extend to those regions.
All day on August 13th we skirted the great basin in
which the Su-lo Ho gathers its main sources, having
mostly to keep close by the foot of low side spurs to avoid
its spreading marshes. But scattered over this boggy
expanse there showed, near and far, glittering ridges of
drift sand, in the shape of big semi-lunes so familiar to
me from the desert. It was strange to meet this combina-
tion of dunes and marshes on a scene set with ice-crowned
mountains. But was it not the most fitting birthplace for
the river which was to end its course amidst those dreary
wastes of sand, gravel, and salt marsh which I had
surveyed beyond the westernmost end of the Tun-huang
Limes? At one point I managed to approach the nearest
chain of dunes, and found there a succession of big semi-
lunes or Barkhans, to use the technical designation,
running roughly from south-east to north-west with
intervals of 400 to 600 yards between them (Fig. 242).
The one I examined closely measured fully 330 yards
between the extreme ends of its receding horns, and
showed forty feet as its maximum height in the centre,
which with its convex side was pointed to the north-west.
The ground within the concavity of these Barkhans was
generally quite clear of sand and in places occupied by
small spring-fed marshes.
From the point where we halted for the night of
August 13th, close on 13,500 feet above the sea, we had a
majestic view of the Shagolin-Namjil group (see Fig. 155).
But clouds were now gathering above it, and a distinct
change in the weather on the following day prevented
the determination of the highest peaks rising above the
large glaciers. The next march took us over easy de-
tritus slopes, boggy in many places, to the top of a long-
stretched flat ridge forming the lowest point of the
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43
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382
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407
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431
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442
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453
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465
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478
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486
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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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