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0066 Southern Tibet : vol.3
南チベット : vol.3
Southern Tibet : vol.3 / 66 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

Klaproth call the upper part of the river R. Danak boutchou? On the Ta-ch'ing
map it is called Daghri phou tchou. It is obviously the same name in both cases.
Both the Ta-ch'ing map and Klaproth have mixed two rivers or rather made one
river of two. This may be seen already from my preliminary account which runs
as follows:¹ ›Tanak-puchu is a great valley coming down from the north, and its
river irrigates the fields in Tanak. I could not obtain a clear description of this
valley: all I heard was that it came from a pass to the north; so I do not know
whether it comes from the Transhimalaya, like the Mü-chu and Shang-chu valleys.
If such is the case, however, then the eastern watershed of the Mü-chu is a hydro-
graphic boundary between it and the Tanak-puchu, not the Shang-chu. The question
can only be solved by future investigations on the spot.‹

Of course Klaproth's Danak boutchou and the Ta-ch'ing map's Daghri phou
tchou are the same as my Tanak-puchu. The name should be written Tanak-pu-chu,
which means ›the river of the upper part of the valley of the black horse‹. For
pu is the upper part of a valley. The name may also be written Ta-nakpo-chu.² My
Rung-chu, by which I came down to the Tsangpo in 1907, is obviously the Rong-
tchou of the Ta-ch'ing map, where the confluence is correctly situated above the
confluence of the Sab-tchou (Shap-chu) and the Tsangpo. On Klaproth's map the
Rung-chu is somewhat changed and drawn out considerably longer than on the
Chinese map, but it has no name. The situation of the Delden (Terten) and Temple
Delden shows, however, that it is the same river in both cases. As the situation
of Delden corresponds to Ye-shung it may be either Ganden-gompa or Tugden-
gompa. I cannot make out the Kiet-tchou of Klaproth, Kié tchou of the Chinese map.
Probably it is some small valley. But the fact that both maps have added
the upper part of the Tanak-valley to the Shang-valley or assumed that the Shang
river was called Tanak in its upper part, seems to permit us to draw two conclu-
sions, viz. that my above quoted suggestion was correct, namely, that the Tanak-
pu-chu comes from a pass in the water-parting range of the Transhimalaya, and
secondly that the surveyors of the Ta-ch'ing map have not been up the whole way
to Khalamba-la, for if that had been the case, they would have observed that the
river came from N.E. and not from N.N.W. And if the Chinese surveyors had really
followed the Tanak-valley from its head and down to the Tsangpo, they would have
observed that the river joined the Tsangpo and not the Shang river.

The region in which the source of the Tanak river is situated still remains
absolutely unknown, for, from a European point of view, the two maps I am
discussing cannot be accepted as real or even approximate knowledge. Not even
Nain Sing, from his northern route, has been able to see anything in this direction.
The map is still left blank. Only my first crossing, over the Sela-la, gave an