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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0433 Southern Tibet : vol.3
南チベット : vol.3
Southern Tibet : vol.3 / 433 ページ(カラー画像)

New!引用情報

doi: 10.20676/00000263
引用形式選択: Chicago | APA | Harvard | IEEE

OCR読み取り結果

Läng-chu is a broad valley flowing to
Shäldäng, only ENE. as its lower part
or SW. side only very and Läng-chu
comparatively high rocky peak. The
small valley full of ice. Flowing from
the hills and coming from west to east
Läng-chörille, two of her tributaries
ngma, the upper and lower Shä-la-ma
so that is reached by my man's way
n, all of them containing water are a
ent of the affluents to Läng-tsang-chu
considerable.

shores of the main river the ground is
ground is sandy and there are pebbles
ing the river is sharply incised and
l and sand, is nearly barren. The valley
plain of Kyangläm becomes gradually
nd valley of Targe-tsänge. Here begins
ley for 1½ km, and its bottom is 10 to
summer the river is said to be very
of the valley. At Läng-to the river
place the bottom of the valley a not a
branches from the river. At Läng-to
s. The valley is here directed to the S
black and steep, but the like I see
for timber owing to its long di
waste. The road therefore does not go

ches the following observations on the
to the S 40° W. a snowy yak. There
Tsangmak, also called Mäkdorche-yak
of the Targe-tsänge, and our first
S.W. is Galdäng and to the west Kang
To the ENE. is the ridge of the Gäl
ands very that undulating slope of the

sign of living rock.
Chumards is seen, to the S 50° E we
s 45° W. again, Mäkdorche-yak to
Shängchok, and S 5° W. Sänge-
Shängchok the Bumnak-chu flowing
and reaches the main river, it is here

VOL. III.