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Lake Paiku
Lake Paiku (or ''Peiku'', Tibetan: ''Paiku-Tso'' or ''-Tsho'') is a lake at elevation on the Tibetan Plateau at , south of the Yarlung Tsangpo (Brahmaputra) River. The lake is long and wide at its narrowest. It is surrounded by mountains reaching . Streams fed by glaciers cascade to the valley floor, but most sink into alluvial deposits before reaching the lake. The surrounding catchment is an endorheic basin with no outlet. It would overflow into the Yarlung Tsangpo with a water level about higher. The lake's brackish Brackish water, sometimes termed brack water, is water occurring in a natural environment that has more salinity than freshwater, but not as much as seawater. It may result from mixing seawater (salt water) and fresh water together, as in estuari ... water is evidence that it has not overflowed in hundreds if not thousands of years. Climate ReferencesNational Aeronautics and Space Administration Paiku {{Tibet-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tibet Autonomous Region
The Tibet Autonomous Region or Xizang Autonomous Region, often shortened to Tibet or Xizang, is a Provinces of China, province-level Autonomous regions of China, autonomous region of the China, People's Republic of China in Southwest China. It was overlayed on the traditional Tibetan regions of Ü-Tsang and Kham. It was formally established in 1965 to replace the Tibet Area (administrative division), Tibet Area, the former Administrative divisions of China, administrative division of the People's Republic of China (PRC) established after the annexation of Tibet by the People's Republic of China, annexation of Tibet. The establishment was about five years after the 1959 Tibetan uprising and the dismissal of the Kashag, and about 13 years after the original annexation. The current borders of the Tibet Autonomous Region were generally established in the 18th century and include about half of historic Tibet, or the Tibet, ethno-cultural Tibet. The Tibet Autonomous Region spans ov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shigatse Prefecture
Shigatse, officially known as Xigazê (; Nepali: ''सिगात्से''), is a prefecture-level city of the Tibet Autonomous Region of the People's Republic of China. Its area of jurisdiction, with an area of , corresponds to the historical Tsang region of Tibet. Overview The administrative center of the prefecture-level city is the Samzhubzê District. It is roughly equivalent to the historical Shigatse urban center, the second-largest city in Tibet, located about southwest of Lhasa and home to the Tashilhunpo Monastery, traditionally the seat of the Panchen Lama. Some of the towns in the prefecture are: Gyantse (Gyantse County), Tingri (Tingri County), and Nyalam (Nyalam County). On 11 July 2014 Shigatse Prefecture was upgraded into a prefecture-level city (the same status as Lhasa). Transport Rail The Lhasa–Xigazê Railway connects Xigazê Railway Station with Lhasa and further connects with Qinghai via Qinghai–Tibet Railway. It takes about 3 hours t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gyirong County
Gyirong (alternatively romanized as sKyid-grong, Kyirong, ; ) is a county of Xigazê Prefecture, Tibet Autonomous Region. It is famous because of its mild climatically conditions and its abundant vegetation which is unusual for the Tibetan plateau. The capital lies at Zongga. Its name in Tibetan, Dzongka means "mud walls". It is one of the four counties that comprise the Qomolangma National Nature Preserve (Gyirong, Dinggyê, Nyalam, and Tingri). In 1945 Peter Aufschnaiter counted 26 temples and monasteries which covered the area of sKyid-grong and the neighboring La-sdebs. The most famous temple of sKyid-grong is the Byams-sprin lha-khang, erected by the famous Tibetan king Srong-btsan sgam-po (Songtsän Gampo) as one of the four Yang-´dul temples in the 7th century A.D. During the 11th century the famous South Asian scholar Atisha visited sKyi-grong. sKyid-grong was one of the favorite meditation places of the Tibetan Yogin Mi-la ras-pa (Milarepa). The local Gyirong lan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nyalam County
Nyalam County (; Tibetan: gnya' lam rdzong) is a county in Tibet's Shigatse Prefecture. It borders on Nepal. The land area of the county is . The population as of 2003 was 10,000. The postal code for the county is 858300. The county seat is in Nyalam Town. The other town of the county is Dram, also known under its Tibetan name Dram, or Nepali Khasa. It is located near the border and is the point of entry from Nepal. At "merely" 2300 meters elevation about the sea level, Zhangmu has mild and humid subtropical climate, which is a rarity for Tibet. It is one of the four counties that comprise the Qomolangma National Nature Preserve (Nyalam, Tingri, Dinggyê, and Kyirong).Department of Forestry, Government of the Tibet Autonomous Region, People’s Republic of China, ‘’Report on Protected Lands in the Tibet Autonomous Region’’ Lhasa: Tibet Autonomous Region Government Publishing House, 2006 Towns and townships * Nyalam Town (, ) * Dram Town (, ) * Yarlêb Township (, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brackish
Brackish water, sometimes termed brack water, is water occurring in a natural environment that has more salinity than freshwater, but not as much as seawater. It may result from mixing seawater (salt water) and fresh water together, as in estuaries, or it may occur in brackish fossil aquifers. The word comes from the Middle Dutch root '' brak''. Certain human activities can produce brackish water, in particular civil engineering projects such as dikes and the flooding of coastal marshland to produce brackish water pools for freshwater prawn farming. Brackish water is also the primary waste product of the salinity gradient power process. Because brackish water is hostile to the growth of most terrestrial plant species, without appropriate management it is damaging to the environment (see article on shrimp farms). Technically, brackish water contains between 0.5 and 30 grams of salt per litre—more often expressed as 0.5 to 30 parts per thousand (‰), which is a specific grav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endorheic Basin
An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes or swamps, permanent or seasonal, that equilibrate through evaporation. They are also called closed or terminal basins, internal drainage systems, or simply basins. Endorheic regions contrast with exorheic regions. Endorheic water bodies include some of the largest lakes in the world, such as the Caspian Sea, the world's largest inland body of water. Basins with subsurface outflows which eventually lead to the ocean are generally not considered endorheic; they are cryptorheic. Endorheic basins constitute local base levels, defining a limit of erosion and deposition processes of nearby areas. Etymology The term was borrowed from French ''endor(rh)éisme'', coined from the combining form ''endo-'' (from grc, ἔνδον ''éndon'' 'wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Standard Tibetan
Lhasa Tibetan (), or Standard Tibetan, is the Tibetan dialect spoken by educated people of Lhasa, the capital of the Tibetan Autonomous Region of China. It is an official language of the Tibet Autonomous Region. In the traditional "three-branched" classification of Tibetic languages, the Lhasa dialect belongs to the Central Tibetan branch (the other two being Khams Tibetan and Amdo Tibetan). In terms of mutual intelligibility, speakers of Khams Tibetan are able to communicate at a basic level with Lhasa Tibetan, while Amdo speakers cannot. Both Lhasa Tibetan and Khams Tibetan evolved to become Tone (linguistics), tonal and do not preserve the word-initial consonant clusters, which makes them very far from Classical Tibetan, especially when compared to the more Linguistic conservatism, conservative Amdo Tibetan. Registers Like many languages, Lhasa Tibetan has a variety of Register (sociolinguistics), language registers: * (Wylie transliteration, Wylie: , literally "wikt:demot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tibetan Plateau
The Tibetan Plateau (, also known as the Qinghai–Tibet Plateau or the Qing–Zang Plateau () or as the Himalayan Plateau in India, is a vast elevated plateau located at the intersection of Central, South and East Asia covering most of the Tibet Autonomous Region, most of Qinghai, western half of Sichuan, Southern Gansu provinces in Western China, southern Xinjiang, Bhutan, the Indian regions of Ladakh and Lahaul and Spiti (Himachal Pradesh) as well as Gilgit-Baltistan in Pakistan, northwestern Nepal, eastern Tajikistan and southern Kyrgyzstan. It stretches approximately north to south and east to west. It is the world's highest and largest plateau above sea level, with an area of (about five times the size of Metropolitan France). With an average elevation exceeding and being surrounded by imposing mountain ranges that harbor the world's two highest summits, Mount Everest and K2, the Tibetan Plateau is often referred to as "the Roof of the World". The Tibetan Plateau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yarlung Tsangpo
The Yarlung Tsangpo, also called Yarlung Zangbo () is the upper stream of the Brahmaputra River located in the Tibet Autonomous Region, China. It is the longest river of Tibet and the fifth longest in China. The upper section is also called Dangque Zangbu meaning "Horse River." Originating at Angsi Glacier in western Tibet, southeast of Mount Kailash and Lake Manasarovar, it later forms the South Tibet Valley and Yarlung Tsangpo Grand Canyon before passing into the state of Arunachal Pradesh, India. Downstream from Arunachal Pradesh the river becomes far wider and is called the Siang. After reaching Assam, the river is known as Brahmaputra. From Assam, the river enters Bangladesh at Ramnabazar. From there until about 200 years ago it used to flow eastward and joined the Meghna River near Bhairab Upazila. This old channel has been gradually dying. At present the main channel of the river is called Jamuna River, which flows southward to meet the Ganges, which in Bangladesh is call ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brahmaputra
The Brahmaputra is a trans-boundary river which flows through Tibet, northeast India, and Bangladesh. It is also known as the Yarlung Tsangpo in Tibetan, the Siang/Dihang River in Arunachali, Luit in Assamese, and Jamuna River in Bangla. It is the 9th largest river in the world by discharge, and the 15th longest. With its origin in the Manasarovar Lake region, near Mount Kailash, on the northern side of the Himalayas in Burang County of Tibet where it is known as the Yarlung Tsangpo River, It flows along southern Tibet to break through the Himalayas in great gorges (including the Yarlung Tsangpo Grand Canyon) and into Arunachal Pradesh. It flows southwest through the Assam Valley as the Brahmaputra and south through Bangladesh as the Jamuna (not to be confused with the Yamuna of India). In the vast Ganges Delta, it merges with the Ganges, popularly known as the Padma in Bangladesh, and becomes the Meghna and ultimately empties into the Bay of Bengal. About long, the Bra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvion'' (the F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
