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1923%20Memoir%20on%20Maps%20of%20Chinese%20Turkistan%20by%20Stein%20s

1923%20Memoir%20on%20Maps%20of%20Chinese%20Turkistan%20by%20Stein%20s

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8 HISTORY OF SL'RVEYS [Chap. I<br />

Irkall ill tile west to tile 11igl1 ice-peaks towering above tllc Yur~ung-kilrl~ headwaters in the<br />

~out11-east. Amoug tl~esr points I included also certain 1)ealts in the much-eroded ooter bills<br />

towards Khotsn by which the longitude of the towu itself might be acc~~rately determined<br />

thereafter when a cl~auce of escept.ionally clear wcatlrer offered.<br />

Two days later a secoud hill station was a~ce~~detl on a 11igl1 ridgc abovc the Kunat<br />

pss (10,820 ft.), and the eqnally distant views there obtained renilered it. possible to secure<br />

triangles to a11110st all those points beforr the veil of dust carried 1111 by a rising \\rind iinally<br />

hid a11 but the nearest grouud from our horizon. Sobsequent experience has uliown how<br />

serions is tlle obstnrle presented to survey operations by the fog-Iikc haze of t.his region. All<br />

along the southern edge of the Tgrini basin and tlre adjoining n~o~urtainl; it. ral.c,ly lifts except<br />

for short. periods of the late natomn :u~l winter.<br />

After a short halt at. KI~otau necessitated by manifold preparations fol. our winter<br />

canlpaigu 1 tliapatclled Rin~ Sing11 on November 23rd for sulq)lement-<br />

Trinncnlntion townrcla<br />

linr,,,,ghu-tiXh, ary triangulation work in tlre mountains and for a surrey of thc high<br />

range stretching east of '31uz-t~gh '. l'l~is \\~oolil fill the gap bet,weeu<br />

our preriot~s wrrey aud the tt.:tet explored by Captain Densy about PGlur aud along the<br />

K'LIII-lun furtlrer east. In accordance wit11 ~IJ' instroctions HGm Sing11 retnrneil to oar<br />

foru1t.r route to\vards Karaugl~o-tiigl~ and established t,ri;~u~ulatioo stations first orr ;I promineut<br />

peak (14,900 ft.) above the UlCtgb-dawin over1ool;ing the Uuya valley, 'J and<br />

subsequently on tile edge of the high plateau above the Pisha valley (T3pe statiou, 13,Y-19 ft,.)<br />

closc to the point \yl~ere tlre trncl; to Karanghu-tigh falls steeply into tile deep-cut gorge of<br />

tlle Yurung-ktish %.<br />

Ile tlreu made his waj by the Igin-danltiu, at the head of the Pislla valley, across the<br />

range runuiug due north from 'Rluz-t;'\g11'. Beyond, t,liis c~tlminates in<br />

Snrvr). of rnnpe S. of<br />

Kbo,un.Kel.l).a, the couspicuous sno\vy massif of the Tikelili-tQgh (Pk.3/60~) and iinally<br />

loses itself on the broad piedn~ont gravel south-east of the<br />

Khotan oasis. Further east he proceeded across the open plateau-like valleys in whic11<br />

rise the heacl-waters of the rivers irrigating the oases bet\seeu Iil~ota~~ and Beriya. Keeping . -<br />

there on high grouud, uotwitl~stnntlil~g the bitter colcl of the season, 11e accurately n~npped<br />

the northern slopes of the outer maill K'UII-11111 range as far east as the vallcy above l'iirt-lniri~n<br />

(IniAmlar). " Fro111 stations eetabl~shed on broad elevntrcl spurs between the glacier-fed<br />

sonrces of the Yulung and Num rivers Ire triangulated a number of pealts on this part of the<br />

range rising to heights above 3 1,000 feet.<br />

\\'hen the increasing winter cold stopped further \vorl; at Ligli altitudes, Hiuui Sing11<br />

descended to the uarrow bell of oases 1v11ich strctclles east. of Cl~ira. Tl~ey lie along the line<br />

where the subsoil water absorbed 011 the gravel slopes to the south conles to light again in<br />

springs and reuclers cultivatiou possible here and there, before being finally lost in the drifting<br />

sands of the TalclamaliBn. From Keriya, the largest of the oases, Ile turnccl nortl~wards<br />

and, following the Keriya river don~n a previously ~unsurveyed portion of its coursr, rejoined<br />

me on December 23rd at the desert site of 13andhn-oilik. 26<br />

Since our separation I had myself been first occupied mitlliu the central portion of the<br />

Khotau oasis by surveys needecl for clearing up inanifold questions<br />

Trnrerses to<br />

Dl,dnol,lk concerning its historical topography. 97 Subsequently I set out by<br />

December 7th into the desert north-eastwards for my main task, the<br />

exploration of sand-buried ancient sites. The plane-table traverse carried out by me along my<br />

route to the ruins of DaodBu-oilik, the first of these, a distance of about 120 miles, had lain<br />

almost wholly through desert and for the last six marches over bare dunes, altogether very<br />

deceptive ground. Rim Singh's survey from Khotau to the same place had been brought<br />

*J See Sheet No. 14. A. 4, where the triangnlation<br />

station ryrnbol end tlre route 1i11c leading to thc po,ition<br />

of rh~n l~ill station linuc been omitted.by an<br />

" See Sheet No. 14. C. 4.<br />

ZG Cf. Btlins of Xhvfns. pp. 282 sq.; Sheet No.<br />

14. C. 1.<br />

overfigl~t.<br />

'= See 8l1eet Xo. 9. n. 4, and for portio~ls of a<br />

photogmph~c panornma 11sre taken in 19U6, Dererl<br />

CoUuy. i. F1g8. 66. 67. , .<br />

9' Bee Sl~eet No. 14. A. 3, 4.<br />

?' See insct mnp (Portions of hhofnn oasis, scale<br />

4 miles to 1 inch) in map ~ .f Aticie111 Ghoton; for tile<br />

location 01 l~ifitorically known points, etc., cf. Ancia~~f<br />

Xhoto~b, i. Chap. TII~, seo. i-iii.

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