|
Gansu Corridor
The Hexi Corridor (, Xiao'erjing: حْسِ ظِوْلاْ, IPA: ), also known as the Gansu Corridor, is an important historical region located in the modern western Gansu province of China. It refers to a narrow stretch of traversable and relatively arable plain west of the Yellow River's Ordos Loop, flanked between the much more elevated and inhospitable terrains of the Mongolian and Tibetan Plateaus. The name ''Hexi'', refers to "west of the river". As part of the Northern Silk Road, running northwest from the western section of the Ordos Loop between Yinchuan and Lanzhou, the Hexi Corridor was the most important trade route in Northwest China. It linked China ''proper'' to the historic Western Regions for traders and military incursions into Central Asia. It is a string of oases along the northern edges of the Qilian Mountains and Altyn-Tagh, with the high and desolate Tibetan Plateau further to the south. To the north are the Longshou, Heli and Mazong Mountains separatin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hexi Corridor
The Hexi Corridor (, Xiao'erjing: حْسِ ظِوْلاْ, IPA: ), also known as the Gansu Corridor, is an important historical region located in the modern western Gansu province of China. It refers to a narrow stretch of traversable and relatively arable plain west of the Yellow River's Ordos Loop, flanked between the much more elevated and inhospitable terrains of the Mongolian and Tibetan Plateaus. The name ''Hexi'', refers to "west of the river". As part of the Northern Silk Road, running northwest from the western section of the Ordos Loop between Yinchuan and Lanzhou, the Hexi Corridor was the most important trade route in Northwest China. It linked China ''proper'' to the historic Western Regions for traders and military incursions into Central Asia. It is a string of oases along the northern edges of the Qilian Mountains and Altyn-Tagh, with the high and desolate Tibetan Plateau further to the south. To the north are the Longshou, Heli and Mazong Mountains separatin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
China Proper
China proper, Inner China, or the Eighteen Provinces is a term used by some Western writers in reference to the "core" regions of the Manchu-led Qing dynasty of China. This term is used to express a distinction between the "core" regions populated by the dominant Han population and the "frontier" regions of China, sometimes known as "Outer China". There is no fixed extent for China proper, as many administrative, cultural, and linguistic shifts have occurred in Chinese history. One definition refers to the original area of Chinese civilization, the Central Plain (in the North China Plain); another to the Eighteen Provinces of the Qing dynasty. There is no direct translation for "China proper" in the Chinese language due to differences in terminology used by the Qing to refer to the regions. The expression is controversial among scholars, particularly in China, due to issues pertaining to territorial integrity. Outer China usually includes the geographical regions of Dzungar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Liupan
Mount Liupan ( zh, c=六盘山, p=Lìupán Shān) is a mountain range in northwestern China, located mostly in southern Ningxia Hui Autonomous Region. It marks the southwestern boundary of the Ordos Basin. Its southern section is known as Mount Long ( zh, c=陇山, p=Lǒng Shān), which strides southeast through eastern Gansu and western Shaanxi province before joining into the Qinling Mountains The Qinling () or Qin Mountains, formerly known as the Nanshan ("Southern Mountains"), are a major east–west mountain range in southern Shaanxi Province, China. The mountains mark the divide between the drainage basins of the Yangtze and Yellow ..., giving rise to regional names like "Longxi Commandery, Longxi" (陇西, lit. "west of Mount Long"), "Longdong" (陇东, "east of Mount Long", referring to the Jing River valley, valley basin region around eastern Pingliang, southern Qingyang and northern Xianyang) and "Longnan" (陇南, "south of Mount Long"). It is the western boundary ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Longxi Commandery
Longxi Commandery (Chinese: trad. , simp. , ''Lǒngxījùn'') was a commandery of imperial China in present-day Gansu, named due to its location west of Mount Long (the southern portion of Mount Liupan). Qin dynasty Established by Shi Huangdi, it originally covered the entire territory of the Qin Empire west of Mount Long with its seat at Didao (present-day Taoyang in Lintao County). This area included most of the upper Wei valley. Its principal route of communication was the Long Road (named for the mountain), which probably passed along the course of the modern railroad west from Xi’an although much of the area nearest the river was then marshland. The territory was used as a staging ground for campaigns up the Tao and the upper Yellow River.De Crespigny, Rafe.The Government and Geography of the Northern Frontier of Late Han!--sic-->". Australian National University, 2004. A revised version of "Northern Frontier: the Policies and Strategy of the Later ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarim Basin
The Tarim Basin is an endorheic basin in Northwest China occupying an area of about and one of the largest basins in Northwest China.Chen, Yaning, et al. "Regional climate change and its effects on river runoff in the Tarim Basin, China." Hydrological Processes 20.10 (2006): 2207–2216.online 426 KB) Located in China's Xinjiang region, it is sometimes used synonymously to refer to the southern half of the province, or Southern Xinjiang, Nanjiang (), 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 (Uyghur language, Traditional spelling: 六城 or ), which means 'six cities' in Uyghur language, Uyghur. Geography and relation to Xinjiang Xinjiang consists of two main geographically, historically, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tianshan Mountains
The Tian Shan,, , otk, 𐰴𐰣 𐱅𐰭𐰼𐰃, , tr, Tanrı Dağı, mn, Тэнгэр уул, , ug, تەڭرىتاغ, , , kk, Тәңіртауы / Алатау, , , ky, Теңир-Тоо / Ала-Тоо, , , uz, Tyan-Shan / Tangritog‘, , also known as the Tengri Tagh or Tengir-Too, meaning the ''Mountains of Heaven'' or the ''Heavenly Mountain'', is a large system of mountain ranges located in Central Asia. The highest peak in the Tian Shan is Jengish Chokusu, at high. Its lowest point is the Turpan Depression, which is below sea level. One of the earliest historical references to these mountains may be related to the Xiongnu word ''Qilian'' ( zh, s=祁连, t=祁連, first=t, p=Qílián) – according to Tang commentator Yan Shigu, ''Qilian'' is the Xiongnu word for sky or heaven. Sima Qian in the ''Records of the Grand Historian'' mentioned ''Qilian'' in relation to the homeland of the Yuezhi and the term is believed to refer to the Tian Shan rather than the Qilia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steppe
In physical geography, a steppe () is an ecoregion characterized by grassland plains without trees apart from those near rivers and lakes. Steppe biomes may include: * the montane grasslands and shrublands biome * the temperate grasslands, savannas and shrublands biome A steppe may be semi-arid or covered with grass or with shrubs or with both, depending on the season and latitude. The term " steppe climate" denotes the climate encountered in regions too dry to support a forest but not dry enough to be a desert. Steppe soils are typically of the chernozem type. Steppes are usually characterized by a semi-arid or continental climate. Extremes can be recorded in the summer of up to and in winter, . Besides this major seasonal difference, fluctuations between day and night are also very great. In both the highlands of Mongolia and northern Nevada, can be reached during the day with sub-freezing readings at night. Mid-latitude steppes feature hot summers and cold wint ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gobi Desert
The Gobi Desert (Chinese: 戈壁 (沙漠), Mongolian: Говь (ᠭᠣᠪᠢ)) () is a large desert or brushland region in East Asia, and is the sixth largest desert in the world. Geography The Gobi measures from southwest to northeast and from north to south. The desert is widest in the west, along the line joining the Lake Bosten and the Lop Nor (87°–89° east). In 2007, it occupied an arc of land in area. In its broadest definition, the Gobi includes the long stretch of desert extending from the foot of the Pamirs (77° east) to the Greater Khingan Mountains, 116–118° east, on the border of Manchuria; and from the foothills of the Altay, Sayan, and Yablonoi mountain ranges on the north to the Kunlun, Altyn-Tagh, and Qilian mountain ranges, which form the northern edges of the Tibetan Plateau, on the south. A relatively large area on the east side of the Greater Khingan range, between the upper waters of the Songhua (Sungari) and the upper waters of the Liao-h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Badain Jaran Desert
The Badain Jaran Desert () is a desert in China which spans the provinces of Gansu, Ningxia and Inner Mongolia. It covers an area of . By size it is the third largest desert in China. This desert is home to some of the tallest stationary dunes on Earth, with some reaching a height of more than , although most average at around . Its tallest dune is also measured, from base to peak, as the world's third tallest dune and highest stationary dune in the world. The desert also features over 100 spring-fed lakes that lie between the dunes, some of which are fresh water while others are extremely saline. These lakes give the desert its name which is Mongolian for "mysterious lakes". These lakes are not completely studied and high pH lakes harbor extremely interesting animal communities. It is also crossed by one river, the Ruo Shui ("weak water"), which has formed an alluvial plain in the desert. Geography Measuring over , the Badain Jaran Desert covers a significant part of the south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mazong Mountain
The Mǎzōng Shān () is a minor mountain range of Subei Mongol Autonomous County, Jiuquan, northern Gansu, China, between the Altay range to the north and the Qilian range to the south. The Mǎzōng Shān peak rises to 2584 m. Climate Mount Mazong has a cold desert climate (Köppen climate classification ''BWk''). Gallery File:Txu-pclmaps-oclc-8607404-mongolia-west.jpg, Map including Mazong Mountain (labeled as MATSZUN SHAN) and surrounding areas (1935) File:Gongpoquansaurus mazongshanensis.jpg, Hadrosauroid Dinosaur skeleton found on (and named for) Mazongshan: '' Gongpoquansaurus mazongshanensis''. References See also * Equijubus * Xinminbao Group The Xīnmínbǎo Group () is a group of geological formations in north central China. They occur across a large depression (geology), depression between the Altai mountains of Mongolia to the north and the Qilian Shan, Qilian mountains of the Qing ... Mountain ranges of China Landforms of Gansu {{Gansu-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Altyn-Tagh
Altyn-Tagh (also Altun Mountains, Altun Shan; , Pinyin: ''A'erjin Shan'', Wade–Giles: ''A-erh-chin Shan;'' Uyghur'':ئالتۇن تاغ'') is a mountain range in Northwestern China that separates the Eastern Tarim Basin from the Tibetan Plateau. The western third is in Xinjiang while the eastern part forms the border between Qinghai to the south and Xinjiang and Gansu to the north. Altun Shan is also the name of a mountain near the eastern end of the range, the highest point in Gansu. Etymology Altyn Tag means ''Gold Mountain'' in Turkic, and Jin Shan () is Chinese for '' Gold Mountain''. Geography A series of mountain ranges run along the northern edge of the Tibetan Plateau. In the west are the Kunlun Mountains. About halfway across the south side of the Tarim Basin, the Altyn-Tagh Range diverges northeast while the Kunluns continue directly east, forming a relatively narrow "V". Inside the "V" are a number of endorheic basins. The eastern end of the Altyn-Shan is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qilian Mountains
The Qilian Mountains (, also romanized as Tsilien; Mongghul: Chileb), together with the Altyn-Tagh (Altun Shan) also known as Nan Shan (, literally "Southern Mountains"), as it is to the south of Hexi Corridor, is a northern outlier of the Kunlun Mountains, forming the border between Qinghai and the Gansu provinces of northern China. Geography The range stretches from the south of Dunhuang some 800 km to the southeast, forming the northeastern escarpment of the Tibetan Plateau and the southwestern border of the Hexi Corridor. The eponymous Qilian Shan peak, situated some 60 km south of Jiuquan, at , rises to 5,547 m. It is the highest peak of the main range, but there are two higher peaks further south, Kangze'gyai at wit5,808 mand Qaidam Shan peak at wit5,759 m Other major peaks include Gangshiqia Peak in the east. The Nan-Shan range continues to the west as Yema Shan (5,250 m) and Altun Shan (Altyn Tagh) (5,798 m). To the east, it passes north of Qinghai Lake, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
