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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| 0140 |
Southern Tibet : vol.3 |
| 南チベット : vol.3 |
引用情報
OCR読み取り結果
the great range in transverse valleys. In this case, therefore, the Transhimalaya is
shown as one very strong range, a new forerunner to the range of Hodgson and
Saunders. It has only small ramifications, most of them on the northern side. The
region between the Gang-dis-ri and the upper Tsangpo is represented as an elevated,
comparatively flat plateau-land with a steep slope to the river at its southern edge.
Only Buksiri is a small isolated range, N.N.E. of Shigatse. Along the southern
bank of the Tsangpo there is sometimes a double mountain system situated.
The Tsangpo is correctly shown as coming from Damtschuk Kabab (Tamchok-
kabab, though this mountain has assumed a rather unusual form. The source branches
have not at all been improved from d'Anville. The source of the Indus is com-
paratively well placed, and the source of the Satlej is perfectly correct; even the
Tage-tsangpo may be suspected on Grimm's map.
It seems indeed curious that a map of Tibet from 1832 can be quite filled
up with detail. There are scarcely any white patches at all, everything seems to be
known, even the names of mountains, rivers and lakes. And still there is nothing
that depends upon European researches, except a few names from Georgi's book.
All the rest is Chinese, and at a few places the interpreters' names are put within
brackets (d'Anv., Klapr.). D'Anville has here played the same part as Ptolemy for-
merly did, but on a smaller scale both as regards time and space.
Comparing Grimm's map of 1832 (Pl. XII) with Klaproth's map of 1836
(Pl. III) we find that the hydrography is about the same in both cases, but that the
mountain ranges, except Himalaya and Kara-korum, are very different. Instead of
Grimm's and Ritter's range of Dzang which stretches from west to east as one very
regular wall, Klaproth's ›third chain‹, between the Kailas and the ›Niantsin tangla
gangri‹ is very irregular, and, in its eastern part, broken up into several ranges and
ramifications. From this point of view, and especially regarding the Nien-chen-
tang-la part of the Transhimalaya, Klaproth's map is by far superior to Grimm's.
Pl. XIII is a reproduction of Tibet as shown on H. BERGHAUS' map of Asia,
published in 1843.¹ It should be compared with Grimm's and Klaproth's maps. It
is easy to find out the resemblances and differences. I will only point out that Berg-
haus has rejected the Hor or Khor Range completely. The hydrography is the
ordinary Chinese one. The orography of the Transhimalayan system is exactly the
same as on Klaproth's map, though the method of drawing is somewhat different.
He has one mighty head-range with many ramifications to the north and south. As
he has followed Klaproth's orography, his map is much better than Grimm's.² Berg-
haus also follows Klaproth's example in not giving the Transhimalayan mountains
one common name. He has the same names for different parts of the system like
Klaproth, only changing the spelling from French into German.
1
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17
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28
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38
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49
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60
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74
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86
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98
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108
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120
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133
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137
139
140
141
142
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147
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158
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168
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178
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189
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200
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210
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221
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231
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242
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253
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265
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277
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287
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298
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309
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321
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337
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349
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362
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375
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393
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410
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427
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443
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455
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473
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487
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500
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513
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527
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539
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550
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563
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575
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587
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599
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610
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