Where is the birthplace of the Yangtze River?

The birthplace of the Yangtze River The Yangtze River originated from the glacier on the south side of the Xuefeng Mountain in Gladin, Kangqu, Tibet. Tibetan is called "Solidification Qu", which means "Cattle River", because the two sources of the Yangtze River seem to flow out from the nostrils of cattle. Like the Yellow River, the Yangtze River is the cradle of the Chinese nation and the birthplace of culture. The source of the Yangtze River is Tuotuo River, which originates from the main peak of Tanggula on the Qinghai-Tibet Plateau at an altitude of 662 1 m-Jianggendiru Snow Mountain in the southwest of Gladandong Snow Mountain. Gladden Snow Mountain and 20 surrounding snow-capped mountains with an altitude of more than 6 kilometers form a snow-capped mountain group with a length of more than 50 kilometers from north to south and a width of about 20 kilometers from east to west. Above 5800 meters above sea level, there is snow all year round, covering an area of more than 600 square kilometers. Nearly 40 modern glaciers in the snow-capped mountains descend the valley, and some form glacier tongues. The end of glacier tongue is about 5400 meters above sea level. Glittering snow-capped mountains and glaciers store an inexhaustible supply of solid water. The Jianggen land in the southwest of the Snow Mountain is like a snow mountain, with an altitude of 6548 meters, surrounded by north-south 1 glaciers and shaped like two front paws of crabs. The South Glacier is 12.6 km long and10.6 km wide. The northern glacier is 10. 1 km long and 1.3 km wide. At the end of the glacier, many strange ice peaks are formed on the tongue of the glacier due to melting, forming magnificent ice towers and waterfalls. The two sides and ends of glacier tongue are close to the exposed area of rocks and gravel, which absorbs more heat and melts violently. A string of water droplets melted under the ice formed a waterfall, and the sound of water gurgled forward. This is the birthplace of the Yangtze River, and the meltwater of these two glaciers is the initial water flow at the source of the Yangtze River. ? The Yangtze River was called "Jiang" or "Great River" in ancient China. Different regions have different names. Since a long time ago, people have been looking for its source. Due to various conditions at that time, it has not been clear. China's famous ancient book Shangshu Gong Yu once regarded Jialing River and Minjiang River, which originated from Minshan Mountain, as the upstream sources of the Yangtze River, so it was said that "Minshan River leads to the river" and "the source of the river is in Min". Until the Ming Dynasty, A.D. 164 1 year, Xu Xiake, a famous geographer in China, went up the Jinsha River and made a field trip to Sichuan, Qinghai and other places, and found that Jinsha River was the upstream source of the Yangtze River, and wrote a book "A Study on the Source of the Yangtze River", which overthrew the previous misconceptions that "Minshan leads the Yangtze River" and "the source of the Yangtze River is in Min", and greatly advanced the birthplace of the Yangtze River. However, he failed to follow the Jinsha River upstream, nor did he find the real birthplace of the Yangtze River. By the Qing Dynasty, that is, in the middle of17th century, people had a further understanding of the water system at the source of the upper reaches of the Yangtze River. At that time, the Tongtian River and Mulu Wusu River had been drawn on the map drawn on the spot, but the understanding of the source of the Yangtze River was still vague. In A.D. 1720, Emperor Kangxi of the Qing Dynasty sent a special envoy to explore the source of the upper reaches of the Yellow River and also visited the upper reaches of the Tongtian River. Seeing that there are many rivers at the southern foot of Bayan Kara, which are as dense as cobwebs, it is impossible to determine which river is the positive source, so we have to say in general: "The source of the river is like a broom, which is wide and scattered." The source of the Yangtze River was really known after the founding of New China. 1In August, 956, the Yangtze River Water Conservancy Committee organized manpower to go to Qumalai and other places at the source of the Yangtze River, and found that the Yangtze River was divided into two sources: the south source was the Muluwusu River, which originated at the northern foot of Tanggula, and the north source was the Chumar River, which originated at the southern foot of Hoh Xil. Although a big step forward than in the past, but still did not find the real birthplace. 1977, the Jiangyuan investigation team organized by the Yangtze River Basin Planning Office and other units came to the source area of the Yangtze River again, and found that the real source of the Yangtze River was under the Gladden Winter Ice Peak at the northern foot of Tanggula, Qinghai Province, and the real source was Tuotuo River. This is the first time in history to find out the real birthplace of the Yangtze River. On the south and north sides of Jianggendiru Snow Mountain (6,548 meters above sea level) in the southwest of Gladden Snow Mountain Group, there are two modern valley glaciers, which are surrounded by pincers. Glacier in the south is 12.8km long, glacier tongue is 8.5km long and10.7km wide, glacier in the north is 10.3km long and glacier tongue is 6km long and10.4km wide. The largest glacier in the south is the source of the Yangtze River. The starting point of the glacier on the south side of Jianggendiru is located at 9 1.07 minutes east longitude, 33.28 minutes north latitude and 6543 meters above sea level. It belongs to the Tanggula Mountain area under the jurisdiction of Golmud City, with the highest starting point among the major rivers in the world. The snow line is about 5820m above sea level, and the end of glacier tongue is 5400m above sea level. Because the two sides and ends of the glacier tongue are close to the exposed gravel area, it absorbs more heat, melts violently, and trickle overflows between the gravel, forming the initial water source of the mighty Yangtze River. Like the melting water of glaciers on the north and south sides, Jianggen Land flows to the northwest along two broad valleys covered with gravel for three or four kilometers, breaking through the mounds and ridges in front respectively, then merging and turning to the north. At this time, the river gradually widened and continued to flow for thousands of meters. At the foot of Badong Mountain, it meets the glacier melt water from the southeast of Gaqiadirugang Snow Mountain Group. After the intersection of east and west branches, it is called Naqinqu. Gaqiadirugang Snow Mountain Group is located in the west of Gladdan Winter Snow Mountain Group, with a length of about 23km from north to south and a width of 10 ~ 12km from east to west. Its main peak is 6573m above sea level, surrounded by 13 snow peaks and more than 20 modern glaciers, with an area of about 190km, among which the snow mountain.