Western Himalaya and Tibet - BestLightNovel.com
You’re reading novel Western Himalaya and Tibet Part 32 online at BestLightNovel.com. Please use the follow button to get notification about the latest chapter next time when you visit BestLightNovel.com. Use F11 button to read novel in full-screen(PC only). Drop by anytime you want to read free – fast – latest novel. It’s great if you could leave a comment, share your opinion about the new chapters, new novel with others on the internet. We’ll do our best to bring you the finest, latest novel everyday. Enjoy
p. 12). Chinese geographers, according to him, describe all parts of Tibet as more or less mountainous; the eastern portion of West Tibet (Gnari) as least so. Captain H. Strachey, in his account of his visit to lake Manasarawar, says expressly that "the surface of Gnari is for the most part extremely mountainous." In the lower Tibetan course of the Sutlej, the recent discoveries of Captain Strachey show that an alluvial table-land of considerable extent exists, intersected by deep ravines.
[36] See some observations of the thermometer recorded by Mr. Vigne, at Iskardo, Khapalu, etc.
[37] Asie Centrale, vol. iii. p. 22.
[38] In the Map No. 65 of the Survey of the Western Himalaya, by Captains Hodgson and Herbert, the glacier of Gangutri is marked "Great snow-bed _or glacier_;" but whether this indication of a knowledge of the true nature of the ma.s.s is due to the surveyors or to the maker of the map in England, I have no means at present of ascertaining.
[39] On the Snow-level in the Himalaya, in the Journal of the Asiatic Society of Calcutta.
[40] The thermometric results obtained by these two travellers do not agree with one another. M. Hugel's thermometer indicated 6300 feet for the elevation of Kashmir, a result which is known from the barometric observations of Jacquemont to be 1000 feet in excess. Mr. Vigne's thermometer, when tested by Moorcroft's barometric results at Le, errs considerably in the opposite direction. In neither case do I know the mode of calculation employed, the results only being given.
INDEX.
Abadan, 209.
Adenocaulon Himalaic.u.m, 47.
Agricultural processes at Iskardo, 259.
" " Le, 443.
Alibransa pa.s.s, 463.
Alluvial deposits of Chango, 112.
" " Chorbat, 206.
" " Dankar, 125.
" " Dras valley, 448.
" " Indus below Le, 391.
" " Karakoram, 433, 438.
" " Kardong, 398.
" " Kyuri, 117.
" " Landar valley, 309.
" " Lio, 107.
" " Molbil, 446.
" " Nubra, 196.
" " Phatu pa.s.s, 445.
" " Phutaksha, 382.
" " Piti valley, 122.
" " Rondu, 254.
" " Shayuk valley, 190.
" " s.h.i.+gar valley, 262.
" " Sungnam, 97.
" " Tibet, 491.
" " Tolti, 232.
" " Zanskar, 369.
Alsine, tufted, 426.
Asdhari, 347.
Avalanches in Dras, 265.
" " Kashmir, 271.
" " Rondu, 253.
Badarwar, 329.
Balanophora, 47.
Ballota, 306.
Baltal, 269, 452.
Banahal pa.s.s, 297.
" valley, 299.
Bardar pa.s.s, 355.
Basehir, 51.
Baspa river, 75.
