Shigeru Kodama

QONG MUZTAG – RECONNAISSANCE & FIRST ASCENTSouth of Taklamakan, West Kunlun
How enchanting and fascinating does it sound? “Kunlun” has long tempted the travelers
to have all sense of adventure and ambition and even these days there still remained anuntrodden and hardly accessible mountain in the remotest eastern end of West Kunlun,
Xinjiang Province, China. That is Qong Muztag in the source of Keriya River. The
Waseda University Alpine Club of Tokyo unveiled the mountain for the first time asforeigners since an approach by H.H.P. Deasy of Survey of India in 1898 and succeededin the first ascent of Qong Muztag (6962m) on August 15, 2000.
The West Kunlun Mountains lie in the northwest of Tibetan Changtang Plateau. The
total length from east to west is some 350km, and Yulungkax River in the western partseparates the mountains to two latitudinal ranges – the North and the South ranges.
The former is relatively dry and the latter is of unstable weather. Most of high peaks arecovered with massive ice and snow fed to glaciers although there exists the only one
peak to exceed 7000m. In the central part Keriya River flows down from south to north
between the two ranges. Qong Muztagh, the second highest in the West Kunlun, soars
in the eastern end of South range being encircled by the headwaters of Keriya River.
Peaks of the North range have an easy access from villages along Silk Road. Peaks inthe western half of the South range may have also an access to take advantages of amilitary road to link Kashgar and Southwest Tibet via Karghalik. The highest peak
(7176m) rises in this part and has no difficulty to approach. The conditions surrounding
Qong Muztag are quite different as it locates far away from oasis villages at thenorthern foot of the range. In addition there is no road around the mountain.
Climbings in West Kunlun commenced in 1985 when a door was opened for foreigners toenter into the region. The highest peak was scaled by Tokyo University of Agriculture in1986 and several minor peaks were climbed by Japanese parties. Qong Muztag far in
the eastern end did not allow the foreign expeditions to challenge for a long time untill
the attwmpts by the Academic Alpine Club of Kyoto University (AACK) in 1985, 87 and88. However, AACK could not have even a glimpse of the mountain profile and gave up
further challenges.
The Waseda University Alpine Club of Tokyo launched intensively the pioneer

1expeditions to Qong Muztag as a venture in commemoration of the 80th anniversary ofthe foundation. The club got a permit for climbing the mountain from the Xinjiang
Mountaineering Association in March 1999. They took immediate steps to reconnoiterthe least known mountain in May and September 1999 successively, and the climbing
party was sent in the summer of 2000.

Fig.1 Approach to Qong Muztag (by Shigeru Kodama)Reconnaissance I - May 1999
Two members of Hiroaki Kino and Hideki Inaba were dispatched. They chose an oldtrade path that connected East Turkestan and Ladak. Polu (2560m) was a starting
point of their caravan. They left there and ascended a rough trail up the valley to thesouth as far as a high pass of 5114m that is drawn as Atoto Dawan in Deasy’s map.
From the pass they went down to large Achik Kul (4520m) basin named after one of thename of salty lake there at about 4500m. They marched forward through a barren andwaterless desert, ascended again to two more passes and then descended down tograveled riverbed of the upper Keriya River. Having overcome such hardship and2

difficulty as worse and cold weather and problems to handle donkeys, they reached apoint 25km far from the mountain. However, they retreated from there since no further
advance of the old trade path was felt possible.

Fig.2 "Map of Mountain Peaks on the Qinghai-Xizang Plateau"Compiled by the Chinese Resarch Institute of Surveying andMapping, China Mountaineering Association
Published and distributed by China Cartographic Publishing House

Reconnaissance II - September 1999
Shigeru Kodama departed alone to search an alternative approach to the mountain. Hefollowed a footstep that Captain Deasy had traced one hundred years ago, where asatellite image map of the West Kunlun indicates that a fault trough (graben) – a part of
Altintagh Fault – is extending westward indefinitely.
On the 4th September he left Khotan accompanied by an Uigur interpreter and a cookby 4WD vehicle. The road from Niya to Karasai crossed a graveled desert. It took morethan nine hours. Karasai is the last inhabited village situated at the foothill of theeastern corner of the West Kunlun. He employed a experienced muleteers, and gathered
as much information as possible on an access route that he was going to quest.
On the 7th they started caravan from Karasai with 12 donkeys, 6 for baggage and 6 forriding. They marched a graveled dry valley southward and crossed a pass named Ulesh
Dawan. An outstanding fault formation appeared here and continued further 300km
southwestward. From the pass they went down to an arid valley to the west. Many Hill
Pigeons and Yellow Billed Choughs were settling on the high sheered cliff. On the next3

day the caravan crossed Kuyak River and entered into Selektuz valley, meaning of
which was Yellow Straight valley that was representing an existence of the tectonic line.
Massive volume of alluvial sediments having been cut apart by a narrow stream piledon the bottom of the valley. They entered into a deep gorge guarded with 100m highwalls in the both sides. After ascending the steep cliff a wide view of blue sky and anexpanse of pasture with many kinds of grasses came into sight. There were manyburrows of marmots too.
The series of terraces continue up to 4000m, streams disappeared, and massive talus
deposits and fluvio glacial deposits covered almost all the riverbed. The landscapechanged to that of a cold desert. Sign of a living thing seemed very scarce. Perhaps only
a few plants less than ten species grow there. Small shrubs belonging to family
Chenopodiaceae, Ceratoides compacta – indigenous name is Yapkak is a principal plantin this area. A typical scene of the birds living in a habitat in desert of high altitude wasobserved. A flock of Snow Finches flew around sand dunes and solitary Redstarts rested
on whitish gravel. They ascended a wide dry valley where glacial moraine formed alongitudinal parallel line. As they went up, the valley became a narrow basin between
rolling hills where a “8” shaped lake accumulated ground water coming from theglaciers that covered the mountains in the vicinity. 200 to 300 Ruddy Sheldacks werefeeding themselves on the lakeside. They had flown from Siberia, stopped over here andthen would headed to India. The local name of the lake is Gangutluk Kul that means
the lake of many Ruddy Shelducks.
On the sixth day after departure they reached a desolate pass of 5141m that was thehighest point throughout the route they traced. Shortly after having crossed the pass,appeared in front a large basin of 80km wide from east to west and 20km wide form
north to south. They could have a view of a chain of brilliant white peaks in the righthand side. There was a salty lake in the center of the basin, named Shor Kul at 4500m.
Fresh water sprang out from the north bank and formed a small stream flowing into thesalty lake. Some kind of cushion plants and countless footmarks of ungulates, birds anda sort of Feridae (cat) dotted the field near the stream. They went ahead 25km on thesandy and graveled plain from Shor Kul, turned to the south, ascended toward the gap
and crossed a corridor like a pass that the local people called Chap (4600m). The
topography surrounding Chap area had undergone deformation. Flat-topped ridges are
ranging to every direction.
From Chap area they descended to the Keriya River basin. For a short while they went
along the easternmost tributary of Keriya River filled with gravel. A small stream again
appeared near the confluence, Yatokogan (4335m) where three tributaries converged

4together. Huge volumes of deposit made up a wide riverbed and formed the riverterraces, which extended to the upper confluence. When they were moving to the leftbank terrace, they saw a big Wild Yak running away on the opposite bank.
The landscape changed here from an arid one to a place influenced by glaciation andperiglacial weatherig. Till several hundred years ago the mass of ice had remained here.
An average temperature got lower. When they took water from small streams in a wide
tributary joining from the southwest, they noticed the water contained some fine soil
and some flowering grasses that grew between the streams. It is assumed that apermafrost layer under the ground was the primary source of water supply, since there
were only bare rocks around this valley nor glacier ice was developing in theneighboring mountains. In the upper part of the valley that was curved like an arch,gramineous grasses came out which fed ungulates and hare. Here was Selukluk Boyan(4790m) – yellowish nape – so called by a muleteer being named after color of thegrasses. The watershed between east and southeast tributaries of Keriya River iswidely open and flat as a plain. A small salty lake was there and a herd of Kulan (wildass) were grazing around the lake.
At last a magnificent panorama of Qong Muztag came into view before them to the left
direction. It was a really breathtaking moment after 8 days caravan from Karasai.

Pic.1

The highest peak of Qong

Muztag (6962 m).
From "First Ascent of Qong Muztag(6962)" Waseda University
Alpine Club, 2000

Captain Deasy had been here, but he could not see such panorama nor take photes due
to bad weather. His mention in his book is; “Then we climbed the long ascent toKumboyan, where, close to the head of the pass, we found antelope, abundance of grassand, by digging, a sufficiency of water. Descending the slope on the other side, wecrossed a tiny tributary of the Keriya River system. A mere brook, quite shallow andless than ten feet broad. In crossing this stretch of country we had to contend withheavy rain and sleet, but now, at Yepal Ungur,” (In Tibet and Chinese Turkestan, Page
176-77)
They descended to Keriya River and pitched tents on the windswept place – Sarkuchi.
They could see the great Keriya River depression and alluring white mountains. The5

following two days were spent for reconnaissance into the untouched area.
The meaning of Qong Muztag is “ice covered great mountains” in Turkish/Uigurish. Themain peak of the mountains is the highest 6962m peak – a rock peak with ice and snow.
To the west the main peak links to the twin peaks of 6740m and to the east the main
peak links to 6845m beyond a big gap and further stretching to the second highest peakof 6942m. A viable climbing route to the main peak would presumably be the northridge with heavy snow. The north face and the north glacier must be avoided because of
the danger of crevasses and avalanches. Qong Muztag is surrounded by huge volumes ofglacial moraine that heaps up old and new deposits. The foothill of the mountains is aheavenly place for wild animals, in particular, for ungulates such as Chirus, Wild Yak,Picas and carnivores. The base camp can be set up among the moraines.

First Ascent – July to August 2000
The climbing expedition led by Shin Yamada (55) was sent in the summer of 2000. The
party was composed of 13 members including 5 university students and 2 TV crews. The
approach and climbing record are summarized as under:July 18: The main party left Japan. (The advance party departed on July 11.)
“ 21: Move from Hotan to Niya.
“ 22: Move from Niya to Kyantokai. The rising of water as a result of heavy rainfall
having continued for a week had them take a time to ford rivers and streams.
“ 23: They started the 220km approach march from Kyantokai (just before Karasai)
to the Base Camp (4850m). The caravan consisted of 90 donkeys, 61 forbaggage and 29 for riding, 17 muleteers and the party members. 12 days wereneeded to reach Base Camp from Kyantokai having crossed the desert of highaltitude. Rainy weather affected adversely the progress of the caravan. Therushing torrents of rivers retarded them and let them wait for 2 days on theriver bank.
Aug. 3: Base Camp was set up at the northern foot of Qong Muztag.
“ 5: Advance Base Camp was set up at 5200m. Donkeys carried the baggage to thiscamp.
“ 9: C1 was pitched at 5900m on the north ridge.
“ 12: C2 was pitched at 6400m on the north ridge. The north ridge was broad andcovered with deep snow.
“ 15: The first ascent of Qong Muztag was accomplished. Yamada wrote:The first assaulting party of Eiho Otani (53), Hiroaki Kino (37) and Yasushi Tanahashi

6(37) left C2 for the summit. They fixed ropes for several pitches on the steep Snow Dome(6650m) to avoid the danger of avalanches. Unstable weather often made them stop
going forward. Snowstorm shut the visibility. They reached the lowest col in rock ridge
at 12:00 when it began to snow fiercely. They stayed there for 2 hours waiting for clear
view. They resumed climbing at 14:00. They tackled the most difficult part to climb.
They took a route along the contact line of rock ridge with cornices and steep snow slope
where they fixed 50m rope. The final leg to the summit was steep snow slope too. At
15:30 they stood on the top. However the weather was not improved. At 19:00 Otani
decided to bivouac beside the large rock on the saddle between the summit and thejunction peak extending to the west peak of 6740m. They returned to C2 at 10:30 on thefollowing day.
Aug. 18: Yamada and Inaba moved from Base Camp to C2 for the second ascent and 4
members including 2 students came to C1 for targeting the west peak. Badweather continued.
“ 20: The both parties retreated from the Snow Dome as the weather was getting
worse and visibility deteriorated. They decided to terminate the climbing.
“ 23: The caravan left Base Camp for return way. “ 29: They came back to Karasai.

Pic.2 A panoramic view of Qong Muztag (6962 m) massif from the upper Keriya basin.
From "First Ascent of Qong Muztag (6962)" Waseda University Alpine Club, 2000■■7