National Institute of Informatics - Digital Silk Road Project
Digital Archive of Toyo Bunko Rare Books

> > > >
Color New!IIIF Color HighRes Gray HighRes PDF   Japanese English
0044 Memoir on Maps of Chinese Turkistan and Kansu : vol.1
Memoir on Maps of Chinese Turkistan and Kansu : vol.1 / Page 44 (Color Image)

New!Citation Information

doi: 10.20676/00000215
Citation Format: Chicago | APA | Harvard | IEEE

OCR Text

High plateaus S. of
main K'un-lun range.

descending from the great main range of the K'un-lun which overlooks
the Yurung-kāsh headwaters from the south. A series of lake basins
extends along the foot of those spurs at elevations of 15,000 to 16,000
feet; but the streams draining the wide valleys to the north rarely reach them, and are lost in
vast detritus fans. 74 Crossing the debouchures of these valleys we made our way still westwards
over the easy divides, separating the lake basins; but progress was made very trying by the
inclement weather and by the utter barrenness of the ground which together with the great ele-
vations told heavily on our ponies and donkeys. With the transport nearing exhaustion and the
fodder supply running out it was impossible to spare time either for triangulation or visits to the
heads of the valleys descending from that portion of the southern K'un-lun range which
stretches from the triangulated peak 8/52M (23,309) south-eastwards as far as circ. long. 80° 30'.
After six long marches from where we had left the Pōlur-Lanak-lā route (C. 468),

Johnson's route
retraced.

we reached the east end of a large salt lake, now mostly dry, which a
party of the G. T. Survey of Ladāk appears to have sighted some forty-
five years before. 75 Marching thence to the north-west for three more
days over very dismal ground, we passed dry salt-encrusted lagoons and struck by September
17th traces of the forgotten route by which Hāji Habibullah had tried to open direct
communication with Ladāk and over which Johnson had been taken to Khotan in 1865. 76
As we followed the track still clearly marked by cairns and other relics, and crossed two easy
passes to the north-west, the main range came again into full view and allowed our position
accurately to be fixed with the help of two triangulated peaks (4/52M or E 57 ; 6/52M or E 58)
of the G.T. Survey. At last we emerged on September 18th in the valley of an eastern feeder
of the Kara-kāsh where some abandoned stone-huts still showed Johnson's camp 'Kārakāsh'. 77

Ascent to glacier col in
search of Yangi-dawān.

It only remained to trace Johnson's route to his 'Yangi-diwān Pass' by which he
crossed the main K'un-lun range towards Karanghu-tāgh. A line of
cairns showed the side valley where the pass would have to be looked
for; but towards its head all trace of the old route had become obliterat-
ed by advancing masses of ice and snow. Information gathered from some Kirghiz who
had joined us lower down in the Kara-kāsh valley, induced me on September 22nd to make
a reconnaissance with the surveyor due north up a steep glacier which appeared to offer the
nearest approach to the watershed. When after a very trying ascent over much-crevassed ice
and névé it was gained on a snowy col for which hypsometer and aneroid readings indicated
a height of about 19,900 feet, the extensive view opening northward supplied the hoped-for
links with our former surveys of 1900 and 1906 from the Khotan side of the main range. 78
But instead of the 'Yangi-dawān' which was to give access eastwards to a tributary of the
Yurung-kāsh (Chomsha-jilga?), we had reached the crest-line of the main range where it
overlooks the glacier-fed headwaters of the Panāz river which flows into the Kara-kāsh.

Junction of K'un-lun
ranges.

The triangulated snowy peak, 3/52 M, 23,071 feet, rising to the east of our position,
effectively blocked all view towards the unexplored portion of the range
flanking the Yurung-kāsh headwaters. But as a compensation this
highest of our survey stations furnished definite proof of the interesting
orographic fact that the high peak in question represents not merely the point of junction of
the two K'un-lun ranges between which the Yurung-kāsh rises, but that it is also the head of
the great northward spur dividing the drainage areas of the Yurung-kāsh and Kara-kāsh rivers.

Frostbite accident.

Unfortunately this important gain to our survey work was attended by a very serious
accident to myself. The delay at that icy height necessitated by
mapping and photographic work, together with incidents arising from
a late and hurried descent to escape the risk of being altogether