Maizhokunggar County

Maizhokunggar County or Meldro Gungkar County is a county of Lhasa and east of the main center of Chengguan, Tibet Autonomous Region. It has an area of 5,492 square kilometres (2,120 sq mi) with an average elevation of over 4,000 metres (13,000 ft). Most of the people are ethnic Tibetan and are engaged in agriculture or herding. Mining is a major source of tax revenue, but has created environmental problems. The county has various tourist attractions including hot springs and the Drigung Monastery.

Maizhokunggar

墨竹工卡县མལ་གྲོ་གུང་དཀར་རྫོང་།
County
View from Drigung monastery
Location of Maizhokunggar County (red) within Lhasa City (yellow) and Tibet Autonomous Region
Coordinates: 29.8393°N 91.7298°E / 29.8393; 91.7298
CountryPeople's Republic of China
Autonomous regionTibet
Prefecture-level cityLhasa
SeatKunggar
Time zoneUTC+8 (China Standard)
Maizhokunggar County
Chinese name
Simplified Chinese墨竹工卡县
Traditional Chinese墨竹工卡縣
Tibetan name
Tibetanམལ་གྲོ་གུང་དཀར་རྫོང་།

Geography

Meldro Gungkar means "The Place where Nagaraja Meldro lived" in Tibetan. "Mozhugongka" means a town at the end of the earth. It is a twin city of Nanjing. The county is located on the middle and upper sections of the Lhasa River (or Kyi River) and the west of Mila Mountain.[1] The Gyama Zhungchu, which runs through Gyama Township, is a tributary of the Lhasa River.[2] Mila (or Mira) Mountain, at 5,018 metres (16,463 ft), forms the watershed between the Lhasa River and the Nyang River.[3][4] The tree line on the north-facing slope of Mt. Mila is at 4,360 metres (14,300 ft).[5]

Mozhugongka is about 68 kilometres (42 mi) east of Lhasa. It has an area of 5,492 square kilometres (2,120 sq mi) with an average elevation of more than 4,000 metres (13,000 ft).[6] Carboniferous sediments are found in the Lhunzub district of the Lhasa Terrane and to the south of Jang Co in the north of the terrane, but fossiliferous Lower Carboniferous has been found in the terrane only in the Maizokunggar district. The 600 metres (2,000 ft) stratum is mainly composed of alternating layers of quartose sandstone, slates and subordinate limestones that include the coral Kueichowphyllum sp.[7]

Climate

Mozhugongka County is in the semi-arid plateau temperate monsoon climate zone, with cold, dry and thin air, and high winds in winter and spring. The annual average temperature is 5.1 to 9.1 °C (41.2 to 48.4 °F). The highest temperature recorded was about 30 °C (86 °F) in June, but the average highest temperature is 14 to 16.1 °C (57.2 to 61.0 °F). The lowest temperature is −16 to −23 °C (3 to −9 °F) in January. There are about 90 frost-free days each year. Annual rainfall is 515.9 millimetres (20.31 in).[8]

Population

The total population as of 2010 was 48,561 people in 9,719 households, the great majority engaged in farming and herding.[6] 98% of the population are ethnic Tibetan.[9]

Administrative divisions

From 1987 the seat of government has been in Kunggar in the west of the county.[8] The main towns and villages include Kunggar and Zaxoi. Administrative divisions are:[4]

  • Kunggar Town (གུང་དཀར་, 工卡镇)
  • Gyama Township (རྒྱ་མ་, 甲玛乡)
  • Tanggya Township (ཐང་སྐྱ་, 唐加乡)
  • Zhaxigeng Township (བཀྲ་ཤིས་སྒང་, 扎西岗乡)
  • Nyimajangra Township (ཉི་མ་ལྕང་རྭ་, 尼玛江热乡)
  • Zaxoi Township (རྩ་ཞོལ་, 扎雪乡)
  • Rutog Township (རུ་ཐོག་, 日多乡)
  • Mamba Township (རྨམ་པ།་, 门巴乡)

Economy

Sketch map showing rivers

Many of the people depend on agriculture, including farming and herding. Development efforts include increased farm animal husbandry, feedstock production, greenhouses for vegetables, and breeding programs.[10] Crops include barley, winter wheat, spring wheat, canola, peas, cabbage, carrots, eggplant, cucumbers, lettuce, spinach, green peppers, pumpkins, potatoes and other greenhouse crops.[9] In 2007 the county produced 23,189,100 kilograms (51,123,200 lb) of food products, and had 235,000 livestock excluding horses.[10] Traditional folk handicrafts include pottery, willow basketwork, wooden objects, mats and gold and silver items.[9] The county is especially noted for its pottery, which does not corrode, retains heat and has an ethnic style. It has a more-than-1000-year-old history.[11]

China National Highway 318 runs through the county from east to west.[6] The section in Mozhugongka County is 80 kilometres (50 mi) long. There are over 70 rural roads in the county, with a total length of 650 kilometres (400 mi).[9] Television is available to 36% of the population and radio to 48%. There is one high school, 14 full primary schools and 74 village schools.[9] Mozhugongka has been selected as a Cooperative Medical System experimental site, which has resulted in a very high percentage of people with health care coverage.[12] Efforts are being made to improve telecommunications and the road system and to attract tourists.[10]

Construction of the Zhikong Hydro Power Station in Maizhokunggar County began in May 2003.[13] The reservoir is at an elevation of 12,660 feet (3,860 m) above sea level.[14] The project cost 1.37 billion yuan. The dam impounds 225,000,000 cubic metres (7.9×109 cu ft) of water. The 100 MW power station came into operation in September 2007.[15] Another 26 small and medium-sized hydropower stations have a total installed capacity of 2,310 kilowatts.[9]

The economy is driven by mineral extraction, which was expected to account for 73.85% of total tax revenue in 2007 while employing 419 people.[10] Extensive mining in the mountainous regions between Gyama and Zibuk have turned areas of what was green pasturage into a grey wasteland. The authorities are reported to have suppressed protests by the local people.[16]

The Gyama mine, located at 29°43′58.9″N 91°41′29.5″E at an elevation of 4,034 meters in the Gyama Valley, is operated by a subsidiary, Tibet Huatailong Mining Development, of a subsidiary, Vancouver based China Gold International Resources Corporation, of China National Gold Group Corporation. It produces gold, molybdenum, and copper. Mining by the state-owned firm replaced small private mines in the area in 2006. About $500 million was invested in construction of the mining facility between 2008 and 2010. The mine, which is upstream of Lhasa, presents water pollution issues and has a history of rocky relations with local residents, many of whom have been displaced and relocated. In March 2013 the 2013 Gyama Mine landslide which killed 83, mostly Han miners, resulted in international attention by the media.[17][18]

Landmarks

Drigung Monastery in the east of the county

Scenic spots include the Bri-gung (Drigung) Monastery and the Dezhong Hot Spring, as well as the nature reserves.[19] The Drikhung Thil Monastery of the Kagyu Sect was founded in 1179 by Lingchen Repa, a disciple of Phagmo Drupa. The monastery is the home of the Drikhung Kagyu School of the Kagyu sect.[20] The Dezhong Hot Spring has abundant supplies of water, and was historically thought to have magical curative powers. It is popular with both tourists and local people.[21] There are 47 religious sites with 634 Buddhist monks and nuns as of 2010. The 29 the monasteries consist of 11 of the Gelug sect, 16 of the Kagyu, 1 of the Nyingma and 1 of the Sakya.[6] Jama wetland in Mozhugongka county is vulnerable to grazing and climate change.[22]

The ruined Gyama Palace, in the Gyama Gully in the south of the county, was built by Namri Songtsen in the 6th century after he had gained control of the area from Supi. Songtsän Gampo, his son, was born in the palace. The traces of the mountainside palace indicate that it was an impressive complex. Three more recent white pagodas mark Songtsen Gampo's birthplace. Later the dynasty moved the capital of Tubo (Tibet) to Lhasa in 633 AD.[23] Gyama was the site of fierce battles against the Mongolian Güshi Khan, who had been invited to Tibet by the Gelug sect. Beside the palace there are ruins of various fortifications from the Yuan (1271–1368) and Ming (1368–1644) dynasties.[23]

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References

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    • Bai, Wanqi; Shang, Erping; Zhang, Yili (2012). "Application of a New Method of Wetland Vulnerability Assessment to the Lhasa River Basin". Resources Science. 34 (9). Archived from the original on 2015-02-10. Retrieved 2015-02-09.CS1 maint: ref=harv (link)
    • Barboza, David (March 29, 2013). "China: Landslide Buries Workers at Mine in Tibet". The New York Times. Retrieved March 30, 2013.CS1 maint: ref=harv (link)
    • Brown, Kerry (2013-08-13). "Mining Tibet, Poisoning China". China Digital Times. Retrieved 2015-02-09.CS1 maint: ref=harv (link)
    • Buckley, Michael (2014-11-11). Meltdown in Tibet: China's Reckless Destruction of Ecosystems from the Highlands of Tibet to the Deltas of Asia. St. Martin's Press. ISBN 978-1-137-47472-8. Retrieved 2015-02-06.CS1 maint: ref=harv (link)
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    • Shi, P.; Körner, C.; Hoch, G. (April 2008). "A Test of the Growth-Limitation Theory for Alpine Tree Line Formation in Evergreen and Deciduous Taxa of the Eastern Himalayas". Functional Ecology. British Ecological Society. 22 (2): 213–220. doi:10.1111/j.1365-2435.2007.01370.x. JSTOR 20142794.CS1 maint: ref=harv (link)
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    • Wong, Edward (April 2, 2013). "Fatal Landslide Draws Attention to the Toll of Mining on Tibet". The New York Times. Retrieved April 3, 2013.CS1 maint: ref=harv (link)
    • Yin, Jixiang; Xu, Juntao; Liu, Chengjie (1988-12-12). "The Tibetan Plateau: Regional Stratigraphic Context and Previous Work". Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. The Royal Society. 327 (1594: The Geological Evolution of Tibet: Report of the 1985 Royal Society -- Academia Sinica Geotraverse of Qinghai-Xizang Plateau): 5–52. doi:10.1098/rsta.1988.0121. JSTOR 38183.CS1 maint: ref=harv (link)
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