Chola Mountains
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Chola Mountains
The Chola Mountains, also romanized as the Trola Mountains, are a northern subrange of the Shaluli Mountains in western Sichuan Province, China. The mountains were once at the centre of the Kingdom of Derge and many remnant Tibetan Buddhist monasteries can be found in the mountain range's valleys. Etymology The Chinese transliteration of the Chola Mountains is ''Que Er Shan'' (). The Chola Mountains are named after the primary pass crossing the range, Cho La or Tro La. Cho La in Tibetan means ''Lake Pass''. However, others claim, Chola is just another name for snow mountain, given by local Tibetans. Due to the Chinese transliteration of the mountains into ''Què'ér'' and its common usage on official maps, the mountain range is sometimes mistakenly translated into "Sparrow Mountains" or "Bird Mountains". Geology Located in the eastern Tibetan Plateau, the Chola Mountains are a result of uplift caused during the Indian subcontinent's collision with the Eurasian Plate. The Ch ...
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Shaluli Mountains
The Shaluli Mountains (), known in Standard Tibetan, Tibetan as Powor Gang, are a large mountain range in western China between the Upper Yangtze (Jinsha) and Yalong River, Yalong Rivers. It is one of the core ranges of the Hengduan Mountains, Hengduan group of mountains. The Shaluli Mountains stretch over 500 km from Dege County, Sichuan in the north to Shangri-La County, Yunnan in the south. The highest peak of the range is Ge'nyen Massif at above sea level. Other subranges in the Shaluli Mountains include the Chola Mountains to the north, the Zhaga Mountains to the east, the Yading massif in the south, and Haba Snow Mountain at the southern edge of the range. The Shaluli Mountains were historically part of the Kham region of Tibet and are now mostly administered as part of Garze Prefecture in modern-day Sichuan Province. Litang County, Litang is the major population centre in this mountain region. The major peaks of the range outside of the Chola Mountains include: *G ...
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Xianshuihe Fault System
The Xianshuihe fault system is a major active sinistral (left-lateral) strike-slip fault zone in southwestern China, at the eastern edge of the Tibetan Plateau. It has been responsible for many major earthquakes, and is one of the most seismically active fault zones in this part of China. Tectonic setting The Xianshuihe fault system lies within the complex zone of continental collision between the Indian Plate and the Eurasian Plate. It forms one of a set of sinistral fault zones that help accommodate the eastward spreading of the Tibetan Plateau. The fault zone defines the northern and eastern edges of the Sichuan-Yunnan block, and the southeastern boundary of the Bayan Har block. Geometry The Xianshuihe fault system comprises several distinct segments, with an overall length of about 350 km. The main segments are the Ganzi (or Ganzi-Yushu), the Xianshuihe, the Anninghe-Zemuhe, and the Xiaojiang faults. Seismicity Movements on this fault system have been responsible for man ...
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Derge
Derge (; ) is a town in Dêgê County in Garzê Tibetan Autonomous Prefecture in Sichuan, China. It was once the center of the Kingdom of Derge in Kham. History Historically, Derge, which means "land of mercy", was an important centre of Tibetan culture, along with places such as Lhasa and Xiahe. Derge was formerly the seat of the kings of the kingdom of Derge, whose 1300-year lineage was broken with the death of the last male heir in the 1990s. The kingdom was an important industrial, religious and political center in Eastern Tibet. In the early 20th century, the kingdom fell into political struggle between the final heirs to the throne, Djembel Rinch'en and Doje Senkel. The latter, who had enjoyed the backing of the Chinese, yielded the kingdom to China in 1908 in exchange for the ousting of his rival. The palace of the Derge kings was torn down after 1950 and a school was later built on the site.McCue, 241. Culture The town of Derge is famous for its three-storey printing ...
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Tibet
Tibet (; ''Böd''; ) is a region in East Asia, covering much of the Tibetan Plateau and spanning about . It is the traditional homeland of the Tibetan people. Also resident on the plateau are some other ethnic groups such as Monpa people, Monpa, Tamang people, Tamang, Qiang people, Qiang, Sherpa people, Sherpa and Lhoba peoples and now also considerable numbers of Han Chinese and Hui people, Hui settlers. Since Annexation of Tibet by the People's Republic of China, 1951, the entire plateau has been under the administration of the People's Republic of China, a major portion in the Tibet Autonomous Region, and other portions in the Qinghai and Sichuan provinces. Tibet is the highest region on Earth, with an average elevation of . Located in the Himalayas, the highest elevation in Tibet is Mount Everest, Earth's highest mountain, rising 8,848.86 m (29,032 ft) above sea level. The Tibetan Empire emerged in the 7th century. At its height in the 9th century, the Tibet ...
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Kham
Kham (; ) is one of the three traditional Tibetan regions, the others being Amdo in the northeast, and Ü-Tsang in central Tibet. The original residents of Kham are called Khampas (), and were governed locally by chieftains and monasteries. Kham presently covers a land area distributed between five regions in China, most of it in Tibet Autonomous Region and Sichuan, with smaller portions located within Qinghai, Gansu and Yunnan provinces. Densely forested with grass plains, its convergence of six valleys and four rivers supported independent Kham polities of Tibetan warrior kingdoms together with Tibetan Buddhist monastic centers.Jann Ronis"An Overview of Kham (Eastern Tibet) Historical Polities" The University of Virginia The early trading route between Central Tibet and China traveled through Kham, and Kham is said to be the inspiration for Shangri-La in James Hilton's novel. Settled as Tibet's eastern frontier in the 7th century, King Songtsen Gampo built temples along its ea ...
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Ecoregion
An ecoregion (ecological region) or ecozone (ecological zone) is an ecologically and geographically defined area that is smaller than a bioregion, which in turn is smaller than a biogeographic realm. Ecoregions cover relatively large areas of land or water, and contain characteristic, geographically distinct assemblages of natural communities and species. The biodiversity of flora, fauna and ecosystems that characterise an ecoregion tends to be distinct from that of other ecoregions. In theory, biodiversity or conservation ecoregions are relatively large areas of land or water where the probability of encountering different species and communities at any given point remains relatively constant, within an acceptable range of variation (largely undefined at this point). Three caveats are appropriate for all bio-geographic mapping approaches. Firstly, no single bio-geographic framework is optimal for all taxa. Ecoregions reflect the best compromise for as many taxa as possible. Se ...
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Southeast Tibet Shrub And Meadows
The Southeast Tibet shrub and meadows are a montane grassland ecoregion that cover the southeast and eastern parts of the Tibetan Plateau in China. The meadows in this region of Tibet are in the path of the monsoon rains and are wetter than the other upland areas of the Tibetan Plateau. The "high cold" alpine terrain is one of high species diversity, due to the relatively high levels of precipitation for the region. Precipitation is lower in the northwest, and hence the vegetation thins from shrub to meadow or even desert. Location and description Many mountain ranges support the Southeast Tibet meadows, stretching from the Nyainqêntanglha Mountains in the southwest to the Qilian Mountains in the northeast. Chinese provinces covered by the Southeast Tibet shrub and meadows include the alpine parts of eastern Tibet Autonomous Region, the alpine parts of western and northern Sichuan, extreme southern and eastern Qinghai, and the montane areas of southern Gansu. Human activ ...
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Montane Grasslands And Shrublands
Montane grasslands and shrublands is a biome defined by the World Wildlife Fund. The biome includes high elevation grasslands and shrublands around the world. The term "montane" in the name of the biome refers to "high elevation", rather than the ecological term which denotes the region below treeline. This biome includes high elevation (montane and alpine) grasslands and shrublands, including the puna and páramo in South America, subalpine heath in New Guinea and East Africa, steppes of the Tibetan plateaus, as well as other similar subalpine habitats around the world. The plants and animals of tropical montane páramos display striking adaptations to cool, wet conditions and intense sunlight. Around the world, characteristic plants of these habitats display features such as rosette structures, waxy surfaces, and abundant pilosity. The páramos of the northern Andes are the most extensive examples of this habitat type. Although ecoregion biotas are most diverse in the And ...
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Hengduan Mountains Subalpine Conifer Forests
The Hengduan Mountains subalpine conifer forests are a temperate forest in the Hengduan Mountains of southwestern China. The forests extend within the Jinsha (upper Yangtze) and Yalong River valleys from approximately 32°N to 27°N. In addition, a portion of the Anning River valley and Mianmian Mountains near Lugu Lake support the subalpine conifer forests. This region covers northern Yunnan Province, western Sichuan Province, and the extreme eastern edge of the Tibet Autonomous Region. The Hengduan Mountains subalpine conifer forests are one zone in a range of montane ecosystems that transition between tropical and temperate ecoregions along the southeastern fringe of the Tibetan Plateau. The Hengduan forests reach elevations higher than and extend to the treeline, beyond which are montane grasslands and shrublands classified as the Southeast Tibet shrub and meadows. The Hengduan conifer forests are separated into two arms by the Shaluli Mountains. Environmental group ...
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Yalong River
The Yalong River ( zh, 雅砻江, Pinyin, p ''Yǎlóngjiāng'', Wade–Giles, w ''Ya-lung Chiang'', Help:IPA/Mandarin, IPA ), or Nyag Chu (Standard Tibetan, Tibetan: , Tibetan pinyin, z ''Nyag Qu''), is a major tributary river of the Yangtze, Yangtze River in Southwest China. With a length of , the Yalong River flows from north to south through the Hengduan Mountains in western Sichuan, Sichuan Province. Course The Yalong has its source in the Bayan Har Mountains on the Tibetan Plateau, Tibet–Qinghai Plateau in Chindu County, Yushu Tibetan Autonomous Prefecture, Yushu, Qinghai, where it is known as the Za Qu ( zh, 扎曲). Flowing southeasterly, the Yalong gradually turns south at Garzê Town, Garzê and travels between the Shaluli Mountains to the west and the Daxue Mountains to the east. The Yalong River channel runs through a deep gorge for much of its length south of Garzê. The southern China National Highway 318, Sichuan-Tibet Highway crosses t ...
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Yangtze
The Yangtze or Yangzi ( or ; ) is the longest river in Asia, the third-longest in the world, and the longest in the world to flow entirely within one country. It rises at Jari Hill in the Tanggula Mountains (Tibetan Plateau) and flows in a generally easterly direction to the East China Sea. It is the seventh-largest river by discharge volume in the world. Its drainage basin comprises one-fifth of the land area of China, and is home to nearly one-third of the country's population. The Yangtze has played a major role in the history, culture, and economy of China. For thousands of years, the river has been used for water, irrigation, sanitation, transportation, industry, boundary-marking, and war. The prosperous Yangtze Delta generates as much as 20% of historical GDP of China, China's GDP. The Three Gorges Dam on the Yangtze is the list of the largest hydroelectric power stations, largest hydro-electric power station in the world that is in use. In mid-2014, the Chine ...
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Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ...
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