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
|
|
カラー画像サムネイル -
目次 -
ページ番号 -
書誌情報(メタデータ) -
キャプション -
カラー画像 -
白黒高解像度画像 -
見開きページ -
グラフィック -
| 0475 |
Southern Tibet : vol.3 |
| 南チベット : vol.3 |
引用情報
OCR読み取り結果
293
Near the little valley Page-lungpa there is a living rock of quartz-porphyrite,
— elsewhere living rock is very rare. The ground is soft material, fine gravel and
dust, here and there covered with moss. In the beds of water-courses the ground
is treacherous, sinking under the feet of the animals. Tanglang-chu joins the valley
of Serchen and several other tributaries, and goes down to Tsargam. At one of
the tributaries Camp 154, Sabuk, has a height of 4 947 m. The snowy mountains
to the west from which the Serchen comes, are called Rong-serchen-kang.
The valleys of Sabuk and Tsechung join the Tsargam-tsangpo; both are full
of ice at this season. The road follows the hills between them and crosses the
pass Bäng-la, 5 237 m high. The rock in the neighbourhood is quartz-porphyry.
Although Bäng-la is secondary and without any importance, it affords a magnificent
view to the north, especially over the mighty Targo-gangri, its glaciers and snowy
summits; to the right of it is seen the deep, broad valley of the Targo-tsangpo;
the Dangra-yum-tso is hidden, but the mountains on its eastern shore appear in
rose colour descending to the lake; Shuru-tso is hidden by hills; to the N.N.W
a snow-covered mountain is called Gablung-pu. In the mountains to the west are
the deep valleys of Tanglang and Changchung. Southwards the ground rises to the
heights of Angden-la.
South of the Bäng-la we enter a round arena-valley, surrounded by relatively
low, partly snow-covered ridges, sending several brooks down to the Sabuk. Camp
155, Angjum, is at a height of 5 186 m. From here the slope becomes steeper;
the hills are pierced by many deep ravines; from the west comes the valley Lung-
chang, with high snowy mountains in the background. The ground is very soft and
swampy, with grass and moss, everything hard frozen; gravel is rare; in protected
places the snow lies two feet deep. The last bit is a stiff climb in the bed of the
brook which comes from the pass.
Angden-la has a height of 5 643 m, and is marked by a mani cairn with flags.
The living rock on the northern side of this flat pass is quartz-porphyrite, quartz-
conglomerate, and some greatly weathered schistous rock. The pass is situated on
the continental water-parting, and in the same range as Sha-la, Chang-la-Pod-la and
Sela-la; to the west this range seems to be connected with the Kanchung-gangri;
northwards the water runs to Shuru-tso, southwards to the Raga-tsangpo.
The view from Angden-la is fascinating, though much is hidden by the sporadic
snow-mountains, rising especially in the west and east, above this hopeless confusion
of ridges, ranges and ramifications. To the south the northern range of the Hima-
laya is clearly seen with its innumerable flat, snow-covered peaks, all apparently of
about one and the same height, and north of the gigantic range is the great valley
of the Tsangpo. To the north the whole Shuru-tso is visible, whereas the Dangra is
hidden behind the Targo-gangri which dominates the whole northern horizon. To
the N. 61° E. we recognise the peak Do-tsänkang.
A second threshold close by is only some 10 m lower than the principal one.
1
.
.
.
.
|
.
.
.
.
17
.
.
.
.
|
.
.
.
.
28
.
.
.
.
|
.
.
.
.
38
.
.
.
.
|
.
.
.
.
49
.
.
.
.
|
.
.
.
.
60
.
.
.
.
|
.
.
.
.
74
.
.
.
.
|
.
.
.
.
86
.
.
.
.
|
.
.
.
.
98
.
.
.
.
|
.
.
.
.
108
.
.
.
.
|
.
.
.
.
120
.
.
.
.
|
.
.
.
.
133
.
.
.
.
|
.
.
.
.
147
.
.
.
.
|
.
.
.
.
158
.
.
.
.
|
.
.
.
.
168
.
.
.
.
|
.
.
.
.
178
.
.
.
.
|
.
.
.
.
189
.
.
.
.
|
.
.
.
.
200
.
.
.
.
|
.
.
.
.
210
.
.
.
.
|
.
.
.
.
221
.
.
.
.
|
.
.
.
.
231
.
.
.
.
|
.
.
.
.
242
.
.
.
.
|
.
.
.
.
253
.
.
.
.
|
.
.
.
.
265
.
.
.
.
|
.
.
.
.
277
.
.
.
.
|
.
.
.
.
287
.
.
.
.
|
.
.
.
.
298
.
.
.
.
|
.
.
.
.
309
.
.
.
.
|
.
.
.
.
321
.
.
.
.
|
.
.
.
.
337
.
.
.
.
|
.
.
.
.
349
.
.
.
.
|
.
.
.
.
362
.
.
.
.
|
.
.
.
.
375
.
.
.
.
|
.
.
.
.
393
.
.
.
.
|
.
.
.
.
410
.
.
.
.
|
.
.
.
.
427
.
.
.
.
|
.
.
.
.
443
.
.
.
.
|
.
.
.
.
455
.
.
.
.
|
.
.
.
472
473
475
476
477
.
|
.
.
.
.
487
.
.
.
.
|
.
.
.
.
500
.
.
.
.
|
.
.
.
.
513
.
.
.
.
|
.
.
.
.
527
.
.
.
.
|
.
.
.
.
539
.
.
.
.
|
.
.
.
.
550
.
.
.
.
|
.
.
.
.
563
.
.
.
.
|
.
.
.
.
575
.
.
.
.
|
.
.
.
.
587
.
.
.
.
|
.
.
.
.
599
.
.
.
.
610
Copyright (C) 2003-2026
National Institute of Informatics(国立情報学研究所)
and
The Toyo Bunko(東洋文庫). All Rights Reserved.
本ウェブサイトに掲載するデジタル文化資源の無断転載は固くお断りいたします。