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0161 Southern Tibet : vol.1
南チベット : vol.1
Southern Tibet : vol.1 / 161 ページ(白黒高解像度画像)

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doi: 10.20676/00000263
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KUBI-GANGRI, TAMCHOK-KABAB AND CHEMA-YUN'DUNG.   I05

tsangpo somewhere about half-way between the source and the confluence. Then it crosses the Chema-yundung somewhere below its source, and finally it goes up to the southern shore of Gunchu-tso. It has never crossed the joint Tsangpo west of Chaksam-ferry. But it crosses the Kubi and the Chema near their sources. The Chinese traveller has probably not even seen the Maryum-chu. He has believed that the Chema joined the Kubi immediately below the point where he crossed the Kubi. Therefore the Ta-ch'ing text says that the Tamchok-kamba comes partly from Kubi-gangri and partly from Chema-yundung-pu and Tamchok-kabab. And it knows only two principal rivers instead of three. The traveller of the northern itinerary had, however, found that a river, which he calls Tchar tchou, came from the wes-and joined Maryum-chu. Therefore when the results of the two surveys should be comt bined on one and the same map, it has been supposed that the Tchar tchou and the river from lake Djima Young rong were two different rivers, although in reality they were one and the same. We arrive at the same result when discussing d'Anville's map. But d'Anville has, from causes unknown to me, placed Tamchokkabab at the source of the river which is identical with the Kubi-tsangpo, and only this view must, of course, be the correct one.

As the Tamchok-kabab has been wrongly placed on the Ta-ch'ing map, the name »Tsan po (Tam tchouk kamba), has also been misplaced, for it follows the Chema-yundung instead of the Kubi-tsangpo. Otherwise the river which comes from Kubi-gangri is fairly correctly laid in on the map.

It is said in the Ta-ch'ing text that the Kouben gang tsian is covered with an enormous glacier and that it belongs to the same mountain range as Goumang and Tam tchouk khabab. Both statements are perfectly correct. On the other hand the statement that the mountains of Maryong should join the Tamchok-kabab with the Changou yarak ri, which is a part of the Transhimalaya, is wrong, even if Tamchok-kabab is placed as the Ta-ch'ing map has it. It is true that Ryder on his map has, just south of Gunchu-tso, a meridional range forming a very sharply marked watershed between the Tsangpo-Brahmaputra system and the ManasarovarSatlej system. But there can hardly be said to exist any continuous range at this place. Straight south of the eastern end of Gunchu-tso there is a spur, which I crossed in Marnyak-la (5,302 m.). Then I passed up the tributaries of Chema-yundung to Tamlung-la and down the Tage-tsangpo to the Manasarovar. The Tamlung-la is a threshold pass in a longitudinal valley and by no means situated in a mountain ridge or range. And the difference in absolute altitude between the Tamlung-la and the surface of the Manasarovar is only 696 meters.

The Chinese text could have added that the range, of which Kubi-gangri is a part, continues the whole way to Langchen-kabab, for this is correctly pointed out on the map. Whether this range, which I have called Kubi-gangri and Ganglunggangri, from names given me by Tibetans, continues also to Gurla Mandata, I cannot tell. Ryder has here two parallel ranges, the southern joining the Gurla

14-131387 I.