Yangtze River Estuary from Batang County, Yushu in Qinghai Province to the east of Yibin, Sichuan Minjiang River Estuary of the river city. Flows through Sichuan, Tibet, and Yunnan provinces. 2308 km long. Most of the river for the gorge, the world famous Tiger Leaping Gorge in northwest Yunnan. Divide large, with plenty of water.
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No. 2
Jinsha River Telephone complaints Lhasa Tourism complaints Tel 0891 66508080891 -6324691 Tibet Tourism complaints Tel 0891 -6834193 National Tourism complaints Tel :010-65275315 Originates in Qinghai Province Tanggula of Gela Dan Winter Snow Mountains, marks the border of Tibet and Sichuan. It borders the river into Qamdo County and Shiqu County in Sichuan junction (Jiang Ke Tang Daxian cover Ha Heung estuary), Batang County, near the eastern edge of the river up through the centerline, Gongjue and Markam County, to Sands sinks wheat mouth curved into the river estuary southwest Yunnan, and then off to the east in Lijiang, Yunnan, upstream of the Yangtze River. Section of the Jinsha River in Chamdo area 587 kilometers long, the river elevation from 3340 to 2296 m, 1044 m drop, the basin area of 2.3 million square kilometers, the average annual flow of 957.3 m3 / s, the annual runoff of 301. 900 million cubic meters (Batang station). Jinsha River valley landscape features can Dege County near the mouth of the White song and Matang County Maqu estuary into upper, middle and lower segment. Gap width of which is the upper valley white, middle to deep gorge, a narrow gorge between the lower section of the valley segment. Above: Wide Gap white valley segment, since Deng Ke Ha Heung cover the mouth of the estuary to Barry White song length 207 km, the river elevation 3340 - 2980 meters, drop 360 meters, with an average gradient of 1.74 ‰. This paragraph valley of cutting depth of 1000 - 1500 meters, the valley valley slope is generally around 30 °. Geological structure and morphology of the valley by valley slope rock influence, was a narrow canyon and valley (dale) phase distribution. Single river gorge, terraces are not developed. River is generally 90 meters or so, the river Qieru Ji Yan. Average width of the bottom section of the narrow valley at about 500 meters, or mudslides support Mizoguchi alluvial terraces development. One of the biggest valley in the northern end of the valley this paragraph Deng Ke gully, which is about 40 km long section of the river, the river is about 3,300 meters above sea level, open valley and straight, was NWW direction, is structurally controlled by the valley. Wide bottom 2 - 3 kilometers, paragraph multisection braided river, floodplain, riverbank development, both sides of the tributary alluvial fan development, prompting a circuitous meandering river, river terraces were asymmetrically distributed, the valley is Qamdo major segment river valley to the most generous. In other Valley section, the river bed is still the single main river beach is very rare. Middle: deep gorge, Barry White song from Batang Maqu estuary to estuary, river length of 291 km, the river at an altitude of 2980 - between 2482 meters, drop 498 meters, with an average gradient of 1.71 ‰. This paragraph valley in 1500 relative to the cutting depth - between 2000 m, the valley valley slope is generally 30 ° or more. Valley River valley phenomenon obviously, valleys moderate upper valley slope, the lower steep valley there is another star on the shoulder platform distribution valley. Valley slope instability, collapse, landslides and mudslides occur frequently. Deep bedrock rivers, river rapids in multiple, rapids, the vast majority of the lot is the bottom of the riverbed. In some of the smaller tributary of the occasional import landslide fan platform development, local bands and occasionally slightly wider distribution in the valley, near the river as there are two levels of terraces Gangtok, 25 meters above the river and 65 meters respectively. This segment within the Jinsha River Valley is Chamdo narrowest section of the valley. The following paragraph: a narrow valley between the canyon section, this paragraph to the mouth of the valley from Batang Batang County Maqu centerline near the mouth of the southwest wheat Qu Hui Jinsha river mouth, 87 km long, the river elevation 2482 - 2296 meters, drop 186 m, with an average gradient of 2.14 ‰. This paragraph relative depth of cut in the valley around 2000 meters, the valley valley slope is generally about 30 °. Canyon section of the river is about 100 meters wide, single bed, river rock 切入基, terraces are not developed. Narrow section of the river valley sandwiched, bottom width is generally about 500 meters wide river, with narrow terraces and alluvial or mudslides support Mizoguchi platform development. As the river near Batang Zhubalong Jinsha River Bridge width of 200 meters, the downstream floodplain and riverbank development visible.
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Outline
China Yangtze River upstream. Merged into a river after a long 江江源 Tongtianhe to Yushu county into the Hengduan Mountains, began to be called the Jinsha River. Flows through northwestern Yunnan Plateau, Southwest Mountain to the southwest of Yibin, Sichuan Basin Minjiang accepted until the total length of 2,316 km, the basin area of 340,000 square kilometers. Since the cross-sectional flow through the high mountains and deep in the mountains, fast-flowing, straight down to the southeast Pentium, to near Lijiang Naxi Autonomous County of Yunnan Shek Kwu suddenly turned northeast, forming the famous Tiger Leaping Gorge, on both sides of the mountains and the river elevation of 2,500 to 3,000 public feet, is one of the world's deepest canyon. Jinsha drop 3,300 meters, water resources hundred million kilowatts, accounting for over 40% of the water resources of the Yangtze River. Rich mineral resources in the basin, but the current is swift and steep ridge, Jiang potential thriller, shipping difficulties. Due to the steep river, water erosion and strong, the Jinsha River is the main source of the Yangtze River at Yichang station sediment. Originates in Qinghai Province Tanggula of Gela Dan Winter Snow Mountains, marks the border of Tibet and Sichuan. It borders the river into Qamdo County and Shiqu County in Sichuan junction (Jiang Ke Tang Daxian cover Ha Heung estuary), Batang County, near the eastern edge of the river up through the centerline, Gongjue and Markam County, to Sands sinks wheat mouth curved into the river estuary southwest Yunnan, and then off to the east in Lijiang, Yunnan, upstream of the Yangtze River. Section of the Jinsha River in Chamdo area 587 kilometers long, the river elevation from 3340 to 2296 m, 1044 m drop, the basin area of 2.3 million square kilometers, the average annual flow of 957.3 m3 / s, the annual runoff of 301. 900 million cubic meters (Batang station). Jinsha River valley landscape features can Dege County near the mouth of the White song and Matang County Maqu estuary into upper, middle and lower segment. Gap width of which is the upper valley white, middle to deep gorge, a narrow gorge between the lower section of the valley segment.
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The previous paragraph
Gap white wide valley segment, since Deng Ke Ha Heung cover the mouth of the estuary to Barry White song length 207 km, the river elevation 3340 - 2980 meters, drop 360 meters, with an average gradient of 1 74 ‰.. This paragraph valley of cutting depth of 1000 - 1500 meters, the valley valley slope is generally around 30 °. Geological structure and morphology of the valley by valley slope rock influence, was a narrow canyon and valley (dale) phase distribution. Single river gorge, terraces are not developed. River is generally 90 meters or so, the river Qieru Ji Yan. Average width of the bottom section of the narrow valley at about 500 meters, or mudslides support Mizoguchi alluvial terraces development. One of the biggest valley in the northern end of the valley this paragraph Deng Ke gully, which is about 40 km long section of the river, the river is about 3,300 meters above sea level, open valley and straight, was NWW direction, is structurally controlled by the valley. Wide bottom 2 - 3 kilometers, paragraph multisection braided river, floodplain, riverbank development, both sides of the tributary alluvial fan development, prompting a circuitous meandering river, river terraces were asymmetrically distributed, the valley is Qamdo major segment river valley to the most generous. In other Valley section, the river bed is still the single main river beach is very rare.
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Middle
Deep gorge, Barry White song from Batang Maqu estuary to estuary, river length of 291 km, the river at an altitude of 2482 - between 2 9 8 0 meters, drop 498 meters, with an average gradient of 1.71 ‰ . This paragraph valley in 1500 relative to the cutting depth - between 2000 m, the valley valley slope is generally 30 ° or more. Valley River valley phenomenon obviously, valleys moderate upper valley slope, the lower steep valley there is another star on the shoulder platform distribution valley. Valley slope instability, collapse, landslides and mudslides occur frequently. Deep bedrock rivers, river rapids in multiple, rapids, the vast majority of the lot is the bottom of the riverbed. In some of the smaller tributary of the occasional import landslide fan platform development, local bands and occasionally slightly wider distribution in the valley, near the river as there are two levels of terraces Gangtok, 25 meters above the river and 65 meters respectively. This segment within the Jinsha River Valley is Chamdo narrowest section of the valley.
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Under section
Narrow valley between the canyon section, this paragraph from the valley to the vicinity of the mouth of Batang Batang County Maqu centerline koji Jinsha River estuary west side of the creek mouth sinks, long 87 km, the river elevation 2482 - 2296 meters, 186 meters drop The average gradient of 2.14 ‰. This paragraph relative depth of cut in the valley around 2000 meters, the valley valley slope is generally about 30 °. Canyon section of the river is about 100 meters wide, single bed, river rock 切入基, terraces are not developed. Narrow section of the river valley sandwiched, bottom width is generally about 500 meters wide river, with narrow terraces and alluvial or mudslides support Mizoguchi platform development. As the river near Batang Zhubalong Jinsha River Bridge width of 200 meters, the downstream floodplain and riverbank development visible.
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Jinsha is how named?
The upper reaches of the Jinsha River is China's longest Yangtze River, in the early years of the Warring States period in 2000 into a book, "Yu Gong" called Blackwater, the subsequent "Shan Hai Jing" called rope water, Han Xu Shen "Dictionary" and "Han Geography" section above will now be called the Yalong River flooding, and to Flow (Yalong) for the mainstream. Three Kingdoms period, known as filtered water, Zhuge Wuhou "May crossing Lu, in-depth barren." Wei Li Tao Yuan in the "Waterways" for the first time for a detailed description of the Jinsha River, but failed implicit relationship of the Jinsha River and the Yangtze River. In addition, there are Lishui Jinsha River, MA Lake River, Sichuan and other names of God. Along the rich alluvial gold, "was born in Lishui gold and silver from Zhuti." Because a lot of the Song Argonauts and renamed the Jinsha river appeared. After the Ming Dynasty geographer Xu fieldwork that "those who push the Jiang Yuan, will be led as to the Sands", thus confirming the source of the Yangtze River and Jinsha River as corrected since "Yu Gong" "Minshan River" continues two millennia fallacy. What is shakin it? Alluvial gold, are produced in low-lying areas or river bottom, then mixed with sand stone, after washing out the gold. Shakin originated in mining, gold ore out of the ground due, after a long wind and rain, and crack rocks north of the gold veins associated with it from sailing down the sediment, sand stone in natural sedimentation, sand and gravel in the river bottom or below gold layer is deposited, thereby forming alluvial gold. Shakin features are: particle sizes, big as beans, small sand-like shapes. Color due to the level of different fineness, over ninety percent of red yellow, eight became yellow, seven became greenish yellow.
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Red Army crossed the Jinsha River ferry
Jinsha River upstream of the Yangtze River. It is walking in the valley between the mountains of the Sichuan-Yunnan border, the river is wide, water and waves. If the Reds make life difficult for the river, the mountains have been the enemy pressed into the valley, the military destruction of stricken dangerous. When the Red Army brigade troops advance to the Jinsha River, Chiang wake up suddenly, the Red Army's aim is neither identified in Guiyang, nor in Kunming, but "crossing the Jinsha River will no doubt." April 28, 1935, he issued the command, control ferry, Jiang Feng ruined ship. On the eve of the Red Army arrived in the Jinsha River, the river's north shore Luedao enemy boats have all the. May 3, 1935, the CMC group cadres comrades accepted snatch Jiao level crossing task. They did not say two words, day and night over the mountains 180 years, the night came the same day the Jinsha River. In the ferry, they are lucky enough to find a boat. The original ship was sent spies to probe the case of South Shore, spies do not know where to go. Later, they with the help of local farmers, a wreck out of the water, the holes stuffed with cloth. Then they take it quietly boats crossing to the north shore. Enemy sentry that spies came back, did not care. They come to a sudden attack, stroke eliminated consecutive regular army and a security team, Jiao level crossing control the strait ferry. Later, they found the five boats, mobilized 36 Shaogong. Meanwhile, the Red Army arrived at the Long Street ferry, crossing the Red Army arrived freemason, but the two are not the ferry boats, coupled with acute water Jiangkuan not bridge. CMC ordered them to quickly go through Jiao Ping River. From May 3 to 9, in seven days and seven nights of the time, the Red Army main force to rely on these seven boats calmly over the river. As the defender of 9 Corps crossed the Wujiang River after Bong CMC command has been Qianxi circle, when the East when the West, suddenly suddenly south north, some troops to contain the enemy. May 6, they came to between Dongchuan, Yunnan and Qiaojia County, and on May 9 smoothly through the transition section of the Jinsha River in the tree. Two days later, the enemy was rushed to the south bank of the pursuers. But the Red River has destroyed the ship seal, fly away without a trace. Mao Zedong, "Sands warm water shot cliffs, cold iron chain cross Bridge" in the "Long March" in an expression of the Red Army's tough.
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Jinsha River (see Yangtze)
Jinsha River (see Yangtze) Jinsha Jiang Jinsha Iiang Jinsha River (Jinsha Jiang) See the Yangtze River.
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Wikipedia Encyclopedia
Jinsha Jiang Jinsha River Jinsha Jiang Yibin above the upper Yangtze River, is a typical river gorge. Aka rope water, flooding, filtered water. Yellow sand because the river is named, or that the result of production Jinfeng Wang named. Yangtze River source Tuotuohe long 358 km; the ON Milky Way, 813 km long; to Yushu Batang River below said before the Jinsha River, crossed between Sichuan and Tibet, Yunnan three provinces, there have been the largest tributary of the Yarlung Jiang import, hereinafter referred to Yibin Yangtze River. 2308 km long Jinsha River basin area 500,000 square kilometers, estuaries average flow 4920 m3 / s. Jinsha River water changes, from July to September water year accounted for 50 to 60 percent, flood low water level than the value of 19 to 30 times. Shiqu to within 1174 km from Gold River Street canyon stretching, Jin Jiang Street, less still the main canyon. Tiger Leaping Gorge in Yunnan Province, 16 kilometers long, the river is only 30 meters from the valley ridge height of over 3000 meters, drop of about 200 meters, one of the world's deep gorge. Dale found only in Long Street, Meng Gu and Qiao family and other local river. Jinsha also anxious to Bay Beach is known for more than just a thousand kilometers of new towns to reach Gold River Street, there is a greater than 400 rapids. River fall 3300 m, the maximum flow rate 7 meters per second, Lunar water power reserves up to 109.18 million kilowatts, accounting for about 40% of the Yangtze River, development and utilization of hydropower installed capacity of more than 87 million kilowatts, the annual generating capacity of 494.3 billion degrees, 48% of the Yangtze River, China is the most abundant water resources of the river. Luo river crossing, Crane Beach, Second Beach, Tiger Leaping Gorge, and so are large Xiangjiaba hydropower dam. Basin, Sichuan precious metals, rare metals main producing areas. Abundant forest resources. In the area south of latitude 28 °, the Jinsha River valley deep, terrain occlusion, the annual long summer without winter, unique natural landscape, can be regarded as a piece of tropical South China "enclave." Jinsha River Bridge on the Sichuan-Tibet Highway (Zheng Lin)
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English Expression
n.: Jinsha River
Thesaurus
gold dust, diamantine, Jinsha County
Related Phrases
Dianchi Lake
geography
stream
body
Yunnan
Sanjiang cocurrent
natural landscape
World artlessness heritage
hydropower station
huaneng
tunnel
nine Top Mountain
Chuda velocity
gules travel
showplace Scenic Area
Containing Phrases
Chinshakiangosaurus
Jinsha river inkstone
gold dust Jiang Shi
gold dust the river bank
Jinsha river caryopteris divaricata
Jinsha river Cold
Jinsha river Road
Crossing Jinsha Jiang Cleverly
speedily cross Jinsha River
Jinsha River cameo
Jinsha river Road Station
Jinsha River mistletoe
Jinsha River middle reaches (of a river)
Jinsha River hydroelectricity
Jinsha River The west point on the horizon where the sun _set_s Street
Jinsha River branch
gold dust River West Road
Skylarking of Jinsha River
correction Chinshakiangosaurus
Jinsha river Ji Bridge
Sichuan gold dust Jiang Shi
Jinsha river Chiefly bend
Chinshakiangosaurus Jiedu
Jinsha River Hotel
Jinsha River buddleia
Jinsha River Cold pot fish
Jinsha River Occupation College
Jinsha River Bridge at Sanduizi
Yibin Jinsha river Big Bridge
Mingxi Jinsha river Big Bridge
Gangtuo Jinsha river Big Bridge
expedition Jinsha river Zhizhan
Jinsha river Road Gas Station
Zhenguanglu Jinsha river Road
Jinsha river road Luding Road
Danbalu Jinsha river Road
Jinsha river road Feng Chuang Village Road
Jinsha river Address Weihui
Jinsha river road center River Road
Jinsha river Road True north Road
Pacify river road Jinsha river Village Village
Jinsha river and Yulong Mountain
Jinsha river road Apricot ghat
True north Road Jinsha river Road
Jinsha river road Mo Town Road
Jinsha river road Zhenguang Road
Yangtze upper reaches (of a river) Jinsha river tract
Jinsha river International Drift festival
Shanghai Jinsha River Hotel
Sanduizi Jinsha river Big Bridge
Mamingxi Jinsha river Big Bridge
Jinsha river Road Changfeng Park
Jinsha river Road Zhongshan North Road
Zhongshan north road Jinsha river Road
Big cross the river Road Jinsha river Road
Jinsha river Road Big cross the river Road
Jinsha river Road China East Normal
Liaoning university Jinsha River Street
Sichuan Jinsha river Occupation College
Longmucuoheng Jinsha river suture zone
Shanghai city putuo district Jinsha river Road Elementary School
Longmucuo Jinsha river suture zone
Jinsha river Road Zhongshan North Road China East Normal
Jinsha river road Danba Road Gas Station
Jinsha river Road Qilian Mountain South Road
Jinsha river road Zaoyanglu Changfeng Park
Zaoyanglu Changfeng Park Jinsha river Road
Jinsha river road Poplar and willow black Road Changfeng Park
Jinsha river road center River Road Big cross the river Road
Jinsha river road Nujiang river Road Changfeng Park
Yunnan Jinsha river middle reaches (of a river) hydroelectricity development Corporation Ltd.
Shanghai yafan citified business hotel Jinsha river Road Store
Shanghai rujia speedy hotel Jinsha river Road Store
Shanghai rujia speedy hotel Jinsha river Road Store
Sichuan Ningnan Jinsha river Tangye Corporation Ltd.
Zhongshan north road Jinsha river Road China East Normal university