Nimu Maqu River
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Nimu Maqu River
The Nimu Maqu River () is a left tributary of the Yarlung Tsangpo River (upper Brahmaputra) that flows south through Nyêmo County Nyêmo is a county in the Lhasa west of the main center of Chengguan, Tibet. It lies on the north bank of the Yarlung Tsangpo River, the northern part of the Brahmaputra. The county has an area of , and as of 2011 had a population of 30,844 peo ... in Lhasa Municipality, Tibet, China. Course The Nimu Maqu is the main river of Nyêmo County and an important tributary of the Yarlung Tsangpo. The river is long. It rises at in the north of the county, and runs south through the whole length of the county. The Nimu Maqu empties into the Yarlung Tsangpo from the north at an elevation of . The valley is wide in its widest section, which contains the county seat and is the main agricultural area in the county. Flow The climate is temperate semi-arid plateau monsoon, with most precipitation falling in the summer. Annual rainfall is . The average flow i ...
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Yarlung Tsangpo River
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 cal ...
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Lhasa (prefecture-level City)
Lhasa is a prefecture-level city, one of the main administrative divisions of the Tibet Autonomous Region of China. It covers an area of of rugged and sparsely populated terrain. Its capital and largest city is Lhasa, with around 300,000 residents, which mostly corresponds with the administrative Chengguan District, while its suburbs extend into Doilungdêqên District and Dagzê District. The consolidated prefecture-level city contains additional five, mostly rural, counties. The city boundaries roughly correspond to the basin of the Lhasa River, a major tributary of the Yarlung Tsangpo River. It lies on the Lhasa terrane, the last unit of crust to accrete to the Eurasian plate before the continent of India collided with Asia about 50 million years ago and pushed up the Himalayas. The terrain is high, contains a complex pattern of faults and is tectonically active. The temperature is generally warm in summer and rises above freezing on sunny days in winter. Most of the rain ...
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Nyêmo County
Nyêmo is a county in the Lhasa west of the main center of Chengguan, Tibet. It lies on the north bank of the Yarlung Tsangpo River, the northern part of the Brahmaputra. The county has an area of , and as of 2011 had a population of 30,844 people, mostly engaged in agriculture or herding. Location "Nyemo" is the Tibetan word for "wheat". It is located in the middle section of the Brahmaputra, from Lhasa. It is mainly agricultural and pastoral, with an area of and an average elevation of . The county seat is above sea level. The Nimu Maqu River flows through the county from north to south. The Yarlung Tsangpo River forms its southern boundary. The highest point is a peak at above sea level, and the lowest point is where the Maqu River empties into the Brahmaputra at an elevation of . The county has a temperate semi-arid plateau monsoon climate, with about 100 frost-free days. Annual rainfall is . Nyêmo County mineral resources are copper, molybdenum and peat. Wildlif ...
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Rivers Of Lhasa
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, an ...
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Tributaries Of The Brahmaputra River
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream."opposite to a tributary"
PhysicalGeography.net, Michael Pidwirny & S ...
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