Mountain Name: Kelja Mountains
Peak height: 7167 meters above sea level
Whether it is not ascended: No
First, the basic situation introduced
The majestic Kunlun Mountains, located between the Qiangtang plateau in the north of Tibet and the Taklimakan Desert in the southern part of China, are the Chinese Longji. The Kunlun Mountains, full of myths, have a prominence in the history of Chinese culture. The Kunlun Mountains has dozens of peaks of more than 6,000 meters, and there are also many peaks around 7,000 meters. In addition to the high mountains such as Muztagag, Mount Kelja, the deep-rooted “Ujinbeilong (in Tibetan Buddhism, it refers to a place that is hidden in the present world but hidden)†has a magical charm. It is very high, 7167 meters above sea level, the mountain is relatively gentle (the average slope of the southern slope is only 30 degrees), the climate is dry, less precipitation, evaporation, the snow line height is 5800 meters - 5900 meters, from the satellite map Look, the glaciers developed on the southern slope of the Kelja Mountains form a huge pattern of aloe leaves and leaves. They are embedded in the vast northern land of Tibet and extend southward from the main peak to a ridge like a squid back to an elevation of 6,000 meters. According to the GOOGLEEARTHMAP analysis, the difficulty of climbing should be relatively small in a 7000-meter mountain. According to China Baiyue website information, in 1986, the Japanese climbing team first boarded, the specific information is unknown.
Second, historical information
This mountain has a long route into the mountains. It takes more than 20 days for either the Minfeng or the end to cross the Kezile Ateda or the Yutian to cross the sulfur mine.
In the late Qing dynasty official revision of the "Yushu County Local Records", it was recorded that "Keliya River originates from the Kelja Mountains and is hidden after passing through the road." The "later possession" is the Ali area in Tibet. The "Yushu County Local Records" also describes in detail that from the (Yuyu) County to the southwest of the county, it is the junction of Xinjiang and Houzang.
This ancient road is called the "Kelja Pass Road," and it runs from Yuxian County in Xinjiang along the Keliyan River in Henan Province, passing through Mu Shi Mountain (more than 6,600 meters above sea level) and Qiongmu Tong Tag Mountain (6920 meters above sea level). The Kelja Pass enters Tibet. So far, in the north of Plu Village, there is still the Allah Chui Yigu Station, and at the Kray Pass at the junction of Xinjiang and Tibet, the Hantampa Pasha Castle in the Tang Dynasty is preserved.
In 1717, the rebel forces in Xinjiang clashed with Abulbant to enter Tibet from the mouth of Kelja Pass. In 1723, the ambitious Qinghai prince Rob Tibet Tanzin also fled from here to Tibet; in 1878, the Qing soldiers hunted down. * When Qinghai Baiyanhu was destroyed, the road was destroyed. The Englishman Sterner claimed that there was an old road from this mountain to India. Later, some people came to Kakrakui to meet the rapids, but they did not advance to the ground. They did not go to the snow-capped mountains and returned to the mountains due to lack of oxygen.
Before the spring of 1929, Wu Lay rate people along the source of the poor polar river in the mountain valley. He had to abandon the horses and donkeys in the most important area in the middle of the valley. A few followers and a bag of apples...the lakes under the icebergs converge in a mountain basin that slopes from south to north. Ten snow-melted streams flow into the lake. They find outlets in the northeast corner of the lake. The lake is clear and cold. You can see the clear texture of the granite stone in the lake. Wu Layin dropped an apple toward the lake mouth. After half a month, the exhausted Wualay returned to Yutian County, where people drank a pot of apples from the mountains. When handed him, Urawa believed that the mountain lake was the source of the Keliya River. After the death of Wu Layin, he was buried in the Kunlun Mountains. The mountain lakes he discovered were called Wulaikule.
In 1950, an independent cavalry division of the Rescue Division of the Red Army departed from Yutian County, Xinjiang, and proceeded to advance toward the Kazan-Kunlun Mountains, drawing a road from the Kunlun Mountains. In fact, they follow the route contained in the "Yushu County Local Records". In 1951, General Wang Zhen led the Ministry of Foreign Affairs to begin construction of the New Tibet Highway in the upper valley of the Upper Creya River. However, at the time of blasting, he encountered the outbreak of the youngest volcano in China, the Karatush Mountain, and abandoned the construction of the New Tibet Highway. The construction of a 1465 km-long new Tibet Highway from Yecheng, Xinjiang to 1956, was started in 1956.) After the construction of the New Tibet Highway, very few people again took the Kelja Pass into Tibet. This ancient road through the Kunlun Mountains gradually Abandoned.
The only data that can be found in recent years is the following: In 1992, the Kyoya source expedition in Japan reached the Xinjiang side of the Kelajada for the first time; the Urumqi Adventure Association and the Northern Goat Club arrived twice in February and June of 2005 respectively. The Kechi Volcano area.
Third, the specific route
This route is located on a plateau 5000 meters above sea level. Along the way, it preserves ancient ruins with thousands of years of history. It also boasts the most spectacular volcanic clusters in the country, the highest lake in the world, and many snow-capped mountains not known to have been climbed. The dangers and difficulties of the road mainly come from the uncertain climate, high altitude adaptation, no supply along the way and no fresh water in some areas. However, with full preparation, safety is still guaranteed.
Starting from the Plu village, it climbs along the Keliya River, over 5114 meters of sulphur plates, and enters the Uruk Plateau basin with an average elevation of 5,000 meters. It is also known as the No People’s Area of ​​the Tibetan Plateau, where rich aquatic plants live. Many wild asses and antelopes are wild animal paradises. There are two large mountain lakes and 14 volcanoes in this deserted area. Among them, the volcano Aqikukul, known as the Asian Volcano No. 1 was once in 1951. The eruption became the youngest active volcano in China. About 130km from Pulu to the crater, the march takes 7 days.
From then on, it took about 15 days to go south again. Through the Aksu River Valley and the Atmusu Valley, they crossed over two more than 5,000 meters of Daxu and more than 5,500 meters of Kiliya Pass, reaching Bangda and Guozao. The plateau (about 5,100 meters) between the plateaus and about 30 kilometers to the northwest reached the base of Kelja Foothills at an altitude of 5,200 meters. Started a climbing adventure. Depending on the time, budget, and physical condition of the people, after the end of the mountaineering expedition, we chose to walk 200 kilometers westwards on foot or by car and arrive at the New Tibet Highway at Dashanshan to get back to Xinjiang. The entire trekking trip is about 400-500 kilometers.
In the process of crossing the Kikya Pass to reach the hinterland of the Kunlun Mountains in the middle, you can experience the gorges, snow peaks, volcanoes, and lakes hidden in the high mountains and the history from the Paleolithic period to the early 1950s. Sites, as well as the vast and northern wasteland of northern Tibet.
Fourth, the landscape along the way
Landscapes passing through the mountains:
Lashtak
6596 meters above sea level, also known as Kutai Kelik Hill. The famous Hetian jade is produced here. The height of the basalt mountain is more than 6,000 meters, forming a mountain range that is lined with clouds and is called Lashtak Mountain. If you have the opportunity to go to southern Xinjiang and you're lucky enough to catch a good rain in Minfeng and Yutian, you may see Kunlun Mountain, the highest snow mountain in Lushitak Mountains. She completely blocked the south. The incoming moisture also blocked dust from the Taklamakan Desert. â€
Volcano 1
Located 2.5km southeast of Ashkol, it was reported that the volcano had erupted on May 27, 1951. The volcanic morphology was well preserved and may be the youngest volcano in the area. The symmetry of the truncated conical shape, the relative height of about 150m, slope angle of about 35 degrees, the crater is a diameter of 120m cylindrical deep pot bottom shape, internal depth of 56m, 40 ° internal angle, the bottom has collapsed and stacked Lava fragments.
Volcano 2
Located on the northern margin of the basin, it is 9km away from No. 1 volcano, with a large cone size and a relative height of 264m. From a morphological point of view, the crater with a composite pyramid structure may reflect the history of resurrection after the volcano died.
Volcano 3
A fully-conserved volcanic cone 1.3km northeast of Urukekler is Volcan 3 with a relative height of only 70--80m. Radial gullies have developed around the cone. The top of the cone is an invagination of the negative terrain but the bottom is relatively flat, and the north is high and the south is low and open to the south and there are traces of water.
In addition, there are seven volcanoes around Urukkole and at least three other volcanoes in the rest of the Ashkule Basin.
The Big Four Faults (Guo Zhao, Bunda Fault, Woolba Fault and Longmu Cuo)
Tibet is the province with the largest number of lakes in China. The dotted lake is one of the natural landscapes here. The northern Tibet Plateau is the highest lake area in the world. Some data show that Wolba is the highest lake with an elevation of 5177 meters, an area of ​​89 square kilometers, and a lagoon. Bangda wrong, lake 4902 meters above sea level, an area of ​​106 square kilometers, salt water lake, Bangda wrong through the drinking water river - spring river to accept Woolba wrong diarrhea. Bangda wrong, once known as Yarr's fault, the lake is 4,902 meters above sea level, with an area of ​​106 square kilometers, and a saltwater lake. Bangda is an ellipse. In August 1987, the measured water depth was 3.8 meters and the transparency was 1.3 meters. The phenomenon of lake shore retreat was extremely obvious. There were 15 lake banks and sand banks. Guo Zhazao, the highest lake in China with an area of ​​over 1,000 square kilometers, is shaped like a broad bean, lying in the south of Kunlun.
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