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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| 0513 |
On Ancient Central-Asian Tracks : vol.1 |
| 中央アジア踏査記 : vol.1 |
キャプション
| [Photo] 132. |
バルタン川の峡谷,サウナブの上手,地震によって塞がれた状態。手前に見えるのは新たに形成された山湖と岩の破片に埋まった以前の川底。GORGE OF BARTANG RIVER, ABOVE SAUNAB, BLOCKED BY EARTHQUAKE. Newly formed tarn in foreground; former river bed buried under rock debris.
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| [Photo] 133. |
サレズの地震によって地滑りが起こり,せきとめられてできたシェダウ湖。。SHEDAU LAKE FORMED BY BARRAGE, THROWN DOWN BY SAREZ EARTHQUAKE.
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引用情報
OCR読み取り結果
rghab, or Bartang as the river is kno
ghis, had cut its way. The passage
a proved exceptionally difficult owi
great earthquake of February 191. T
breathing it had in many places c
e river passage and destroyed what tr
or above it. The big river, once fro
h-i-Panja and at one time claimed to
Oxus, had ceased altogether to flow.
e tarns, with colours of exquisite bea
replaced the river and contributed
Fig. 130). In some places debris w
he slopes like mud and offered no fot
ual march we clambered up to a m
or north by a high ridge of shattered r
s had bodily carried across from the
lley. On descending I sighted the narr
g. 133) which had been formed in vi
e mouth of the Shedau valley by the st
nd blocked the Bartang river. Scramb
e over rock debris heaped up in sile
ade our way past the northern end of the
ng the floor of that enormous barra
e spur was gained which divides what
y from what had been the Sarez Fir
m spur to the south-east the full exten
ours revealed itself (Fig. 135). The M
ntains from the range on the north had c
Bassie, once a favourite grazing-grou
a fine alpine lake which, according
s already in 1913 over seventeen mi
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57
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68
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79
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134
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168
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178
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189
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200
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212
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352
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364
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377
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391
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406
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418
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431
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442
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453
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466
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477
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491
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502
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511
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525
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537
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550
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561
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571
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578
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