Among The Tibetans By Isabella L. Bird























































 -   We took
five hours for the ascent of the Digar Pass, our loads and some of us
on yaks, some - Page 20
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We Took Five Hours For The Ascent Of The Digar Pass, Our Loads And Some Of Us On Yaks, Some Walking, And Those Who Suffered Most From The 'pass- Poison' And Could Not Sit On Yaks Were Carried.

A number of Tibetans went up with us.

It was a new thing for a European lady to travel in Nubra, and they took a friendly interest in my getting through all right. The dreary stretches of the ascent, though at first white with edelweiss, of which the people make their tinder, are surmounted for the most part by steep, short zigzags of broken stone. The heavens were dark with snow-showers, the wind was high and the cold severe, and gasping horses, and men prostrate on their faces unable to move, suggested a considerable amount of suffering; but all safely reached the summit, 17,930 feet, where in a snowstorm the guides huzzaed, praised their gods, and tucked rag streamers into a cairn.

The loads were replaced on the horses, and over wastes of ice, across snowfields margined by broad splashes of rose-red primulas, down desert valleys and along irrigated hillsides, we descended 3,700 feet to the village of Digar in Nubra, where under a cloudless sky the mercury stood at 90 degrees!

Upper and Lower Nubra consist of the valleys of the Nubra and Shayok rivers. These are deep, fierce, variable streams, which have buried the lower levels under great stretches of shingle, patched with jungles of hippophae and tamarisk, affording cover for innumerable wolves. Great lateral torrents descend to these rivers, and on alluvial ridges formed at the junctions are the villages with their pleasant surroundings of barley, lucerne, wheat, with poplar and fruit trees, and their picturesque gonpos crowning spurs of rock above them. The first view of Nubra is not beautiful. Yellow, absolutely barren mountains, cleft by yellow gorges, and apparently formed of yellow gravel, the huge rifts in their sides alone showing their substructure of rock, look as if they had never been finished, or had been finished so long that they had returned to chaos. These hem in a valley of grey sand and shingle, threaded by a greyish stream. From the second view point mountains are seen descending on a pleasanter part of the Shayok valley in grey, yellow, or vermilion masses of naked rock, 7,000 and 8,000 feet in height, above which rise snow capped peaks sending out fantastic spurs and buttresses, while the colossal walls of rock are cleft by rifts as colossal. The central ridge between the Nubra and Upper Shayok valleys is 20,000 feet in altitude, and on this are superimposed five peaks of rock, ascertained by survey to be from 24,000 to 25,000 feet in height, while at one point the eye takes in a nearly vertical height of 14,000 feet from the level of the Shayok River! The Shayok and Nubra valleys are only five and four miles in width respectively at their widest parts.

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