Taklamakan Desert in the context of "Plateaus"

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⭐ Core Definition: Taklamakan Desert

The Taklamakan Desert (/ˌtækləməˈkæn/ TAK-lə-mə-KAN) is a desert in northwest China. Located inside the Tarim Basin in Southern Xinjiang, it is bounded by the Kunlun Mountains to the south, the Pamir Mountains to the west, the Tian Shan range to the north, and the Gobi Desert to the east.

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In this Dossier

Taklamakan Desert in the context of Tarim Basin

The Tarim Basin is an endorheic basin in Xinjiang, Northwestern China occupying an area of about 888,000 km (343,000 sq mi) and one of the largest basins in Northwest China. Located in China's Xinjiang region, it is sometimes used synonymously to refer to the southern half of the province, that is, Southern Xinjiang or Nanjiang (Chinese: 南疆; pinyin: Nánjiāng), as opposed to the northern half of the province known as Dzungaria or Beijiang. Its northern boundary is the Tian Shan mountain range and its southern boundary is the Kunlun Mountains on the edge of the Tibetan Plateau. The Taklamakan Desert dominates much of the basin. The historical Uyghur name for the Tarim Basin is Altishahr (Traditional Uyghur: آلتی شهر, Chinese: 六城), which means 'six cities' in Uyghur. The region was also called Little Bukhara or Little Bukharia. The basin is a major area for renewable energy development, particularly solar and wind power, with a focus on utilizing the vast Taklamakan Desert. A high-voltage power loop has been constructed around the basin, collecting energy from various sources and transmitting it to other regions.

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Taklamakan Desert in the context of Plateau

In geology and physical geography, a plateau (/pləˈt, plæˈt, ˈplæt/; French: [plato]; pl.: plateaus or plateaux), also called a high plain or a tableland, is an area of highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones.

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Taklamakan Desert in the context of Uyghurs

The Uyghurs, alternatively spelled Uighurs, Uygurs or Uigurs, are a Turkic ethnic group originating from and culturally affiliated with the general region of Central Asia and East Asia. The Uyghurs are recognized as the titular nationality of the Xinjiang Uyghur Autonomous Region in Northwest China. They are one of China's 55 officially recognized ethnic minorities.

The Uyghurs have traditionally inhabited a series of oases scattered across the Taklamakan Desert within the Tarim Basin. These oases historically functioned as independent states or came under the control of various civilizations, including Chinese, Mongol, Tibetan, and Turkic powers. The Uyghurs gradually started to become Islamized in the 10th century, and most Uyghurs identified as Muslims by the 16th century. Islam has since played an important role in Uyghur culture and identity.

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Taklamakan Desert in the context of Fault (geology)

In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep.

A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geological maps to represent a fault.

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Taklamakan Desert in the context of Hotan Prefecture

Hotan Prefecture (see also § Etymology) is located in the Tarim Basin region of southwestern Xinjiang, China, bordering the Tibet Autonomous Region to the south and Union Territory of Ladakh and Gilgit-Baltistan to the west. The vast majority of the Aksai Chin region which is disputed between China and India is administered as part of Hotan Prefecture. The seat of Hotan Prefecture is Hotan and its largest county by population is Karakax County. The vast majority of the residents of the prefecture are Muslim Uyghurs and live around oases situated between the desolate Taklamakan Desert and Kunlun Mountains.

The region was the center of the ancient Iranian Saka Buddhist Kingdom of Khotan. Later, the region was part of the Kara-Khanid Khanate, followed by the Qara Khitai, Chagatai Khanate, Moghulistan and the Dzungar Khanate, which was conquered by the Qing dynasty of China. Hotan became part of Xinjiang under Qing rule. In the 1930s, the Khotan Emirate declared independence from China. The People's Liberation Army entered Hotan in 1949.

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Taklamakan Desert in the context of Hotan

Hotan (Uyghur: خوتەن, romanizedXoten; Chinese: 和田; pinyin: Hétián) is a major oasis town in southwestern Xinjiang, an autonomous region in Northwestern China. The city proper of Hotan broke off from the larger Hotan County to become an administrative area in its own right in August 1984. It is the seat of Hotan Prefecture.

With a population of 408,900 (2018 census), Hotan is situated in the Tarim Basin some 1,500 kilometres (930 mi) southwest of the regional capital, Ürümqi. It lies just north of the Kunlun Mountains, which are crossed by the Sanju, Hindutash and Ilchi passes. The town, located southeast of Yarkant County and populated almost exclusively by Uyghurs, is a minor agricultural center. An important station on the southern branch of the historic Silk Road, Hotan has always depended on two strong rivers, the Karakash River and the White Jade River, to provide the water needed to survive on the southwestern edge of the vast Taklamakan Desert. The White Jade River still provides water and irrigation for the town and oasis.

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Taklamakan Desert in the context of Turpan water system

The Turpan water system, also called the Turfan kārēz system, is used for water supply via a vertical tunnel in the Turpan Depression of Xinjiang, China. "Karez" (lit.'well') is a word in the local Uyghur language that is derived from the word in the Persian language for the system from which it is derived: kārīz. Turpan has the Turpan Karez Paradise (a Protected Area of the People's Republic of China), which is dedicated to demonstrating its karez water system, as well as exhibiting other historical artifacts.

Turpan's karez well system was crucial in Turpan's development as an important oasis stopover on the Silk Road, which skirted the barren and hostile Taklamakan Desert.

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Taklamakan Desert in the context of Yarkant County

Yarkant County, also known as Yakan County or Shache County, is a county in the Xinjiang, China, located on the southern rim of the Taklamakan Desert in the Tarim Basin. It is one of 11 counties administered under Kashgar Prefecture. The county, usually referred to as Yarkand in English, was the seat of an ancient Buddhist kingdom on the southern branch of the Silk Road and the Yarkand Khanate. The county sits at an altitude of 1,189 metres (3,901 ft) and as of 2003 had a population of 373,492.

The fertile oasis is fed by the Yarkand River, which flows north down from the Karakorum mountains and passes through the Kunlun Mountains, known historically as the Congling mountains (lit. 'Onion Mountains' - from the abundance of wild onions found there). The oasis now covers 3,210 square kilometres (1,240 sq mi), but was likely far more extensive before a period of desiccation affected the region from the 3rd century CE onwards.

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