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Barkol Shan
The Barkol Tagh, also known as Barkol Shan (), forms together with the Qarlik Tagh the easternmost end of the Tian Shan mountain range. It is located along an active thrust fault in the Kumul prefecture in Xinjiang province. Barkol city and the hypersaline A hypersaline lake is a landlocked body of water that contains significant concentrations of sodium chloride, brines, and other salts, with saline levels surpassing those of ocean water (3.5%, i.e. ). Specific microbial species can thrive i ... Lake Balikun (116 km2) are located at the northern flank of the mountain range. There, mean annual temperature is 1.0°C and mean annual precipitation is 210 mm. Another branch of the Tian Shan, the Meiqinwula Mountains, is located north of the Lake Balikun basin. References Mountain ranges of China Mountain ranges of Xinjiang Mountain ranges of the Tian Shan Xinjiang {{China-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Xinjiang
Xinjiang,; , SASM/GNC romanization, SASM/GNC: Chinese postal romanization, previously romanized as Sinkiang, officially the Xinjiang Uygur Autonomous Region (XUAR), is an Autonomous regions of China, autonomous region of the China, People's Republic of China (PRC), located in the Northwest China, northwest of the country at the crossroads of Central Asia and East Asia. Being the List of Chinese administrative divisions by area, largest province-level division of China by area and the List of the largest country subdivisions by area, 8th-largest country subdivision in the world, Xinjiang spans over and has about 25 million inhabitants. Xinjiang Borders of China, borders the countries of Afghanistan, India, Kazakhstan, Kyrgyzstan, Mongolia, Pakistan, Russia, and Tajikistan. The rugged Karakoram, Kunlun Mountains, Kunlun and Tian Shan mountain ranges occupy much of Xinjiang's borders, as well as its western and southern regions. The Aksai Chin and Trans-Karakoram Tract regions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tian Shan
The Tian Shan, also known as the Tengri Tagh or Tengir-Too, meaning the "Mountains of God/Heaven", is a large system of mountain ranges in Central Asia. The highest peak is Jengish Chokusu at high and located in Kyrgyzstan. Its lowest point is at the Turpan Depression, which is below sea level. The Tian Shan is sacred in Tengrism. Its second-highest peak is known as Khan Tengri, which can be translated as "Lord of the Spirits". At the 2013 Conference on World Heritage, the eastern portion of Tian Shan in western China's Xinjiang Region was listed as a World Heritage Site. The western portion in Kyrgyzstan, Kazakhstan, and Uzbekistan was then listed in 2016. Geography Tian Shan with the ancient Silk Road The Tian Shan range is located north and west of the Taklamakan Desert and directly north of the Tarim Basin. It straddles the border regions of Kazakhstan, Kyrgyzstan, Uzbekistan and Xinjiang in Northwest China. To the south, it connects with the Pamir Mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qarliq Tagh
Qarliq Tagh (also Harlik Shan, Karlik Tagh, or Qarlik Shan) is the easternmost mountain range of the Tian Shan, China. It is located in Xinjiang, China, between 42º50'N–43º35'N and 93º41'O–95º07'O. In its western end it connects with the Barkol Shan. The highest peak is the Tomort ({{Höhe, 4886 above sea level). The mountain range is characterized by distinct ice caps and more than 122 glaciers with a total area of 126 km2, of which are 73 on the southern and 49 on the northern flanks. In the north, the mountains descend steeply into the Naomaohu basin, which connects to the Naomaohu Gobi (chin.) / Nomingyyn Gobi (mongol.). In the south, the mountain range descends into the Hami basin, with elevations as low as 50 m below sea level. References Cunningham, D., Owen, L., Snee, L., & Jiliang, L. (2003). Structural framework of a major intracontinental orogenic termination zone: the easternmost Tien Shan, China. Journal of the Geological Society, 160(4), 575-59 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrust Fault
A thrust fault is a break in the Earth's crust, across which older rocks are pushed above younger rocks. Thrust geometry and nomenclature Reverse faults A thrust fault is a type of reverse fault that has a dip of 45 degrees or less. If the angle of the fault plane is lower (often less than 15 degrees from the horizontal) and the displacement of the overlying block is large (often in the kilometer range) the fault is called an ''overthrust'' or ''overthrust fault''. Erosion can remove part of the overlying block, creating a ''fenster'' (or ''window'') – when the underlying block is exposed only in a relatively small area. When erosion removes most of the overlying block, leaving island-like remnants resting on the lower block, the remnants are called ''klippen'' (singular '' klippe''). Blind thrust faults If the fault plane terminates before it reaches the Earth's surface, it is called a ''blind thrust'' fault. Because of the lack of surface evidence, blind thrust fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hami
Hami ( zh, c=哈密) or Kumul () is a prefecture-level city in eastern Xinjiang, China. It is well known for sweet Hami melons. In early 2016, the former Hami county-level city merged with Hami Prefecture to form the Hami prefecture-level city with the county-level city becoming Yizhou District, Hami, Yizhou District. Since the Han dynasty, Hami has been known for its production of agricultural products and raw resources. History Origins and names Cumuḍa (sometimes ''Cimuda'' or ''Cunuda'') is the oldest known exonym and endonym, endonym of Hami, when it was founded by a people known in Han Chinese sources as the ''Yuezhi, Xiao Yuezhi'' ("Lesser Yuezhi"), during the 1st millennium BCE. The oldest attested Chinese name is "" ( zh, labels=no, p=Kūnmò). By the time of the Han dynasty, it was referred to in Chinese as "" ( zh, labels=no, p=Yīwú) or "" ( zh, labels=no, p=Yīwúlú). Under the Tang dynasty, it was also known as , . The name I-gou, I-gu, Igu, &c. sometimes en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barkol Kazakh Autonomous County
Barkol Kazakh Autonomous County (sometimes Barkul or Balikul in English) is a part of Hami Prefecture in Xinjiang and has an area of . It forms part of the China–Mongolia border (bordering the Mongolian provinces of Khovd and Govi-Altai) on the county's north, while bordering Yizhou District to the south, Yiwu County to the east and Changji's Mori Kazakh Autonomous County to the west. Barkol was made an autonomous county on October 1, 1954. It is noted for camel breeding and horse breeding with the Barkol horse well known throughout China. Due to the large number of camels, which is unparalleled in China, the county is nicknamed the "county of ten thousand camels". History Barkol was a territory of Pulei country in ancient times. During the continuous Han–Xiongnu War, in 72 BC, Emperor Xuan of Han sent Zhao Chongguo as general of Pulei, together with Wusun to attack the Huns. After the Northern Wei dynasty, Rouran and Gaoche competed for the Pule grassland for a long tim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hypersaline Lake
A hypersaline lake is a landlocked body of water that contains significant concentrations of sodium chloride, brines, and other salts, with saline levels surpassing those of ocean water (3.5%, i.e. ). Specific microbial species can thrive in high-salinity environments that are inhospitable to most lifeforms, including some that are thought to contribute to the color of pink lakes. Some of these species enter a dormant state when desiccated, and some species are thought to survive for over 250 million years. The water in hypersaline lakes has great buoyancy due to its high salt content. Hypersaline lakes are found on every continent, especially in arid or semi-arid regions. In the Arctic, the Canadian Devon Ice Cap contains two subglacial lakes that are hypersaline. In Antarctica, there are larger hypersaline water bodies, lakes in the McMurdo Dry Valleys such as Lake Vanda with salinity of over 35% (i.e. 10 times as salty as ocean water). The most saline water body ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of China
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Xinjiang
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mount ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of The Tian Shan
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
