Mountain Profile
The Brahmaputra originates from the snow-capped peaks in the western part of the Himalayas and goes eastward along the valley on the northern slopes of the Himalayas. It travels more than 1,000 kilometers and flows to the tail of the eastern section of the Himalayas. It turns at the junction of the four counties of Nyingchi, Miling, Medog and Bomi. Down south, a large horseshoe shaped fjord formed. On the inside of this gorge, it is 74.6° East longitude and 35.25° North latitude is the 15th highest peak in the world and Nanjiabawa peak of 7792 metres above sea level. On the outside of the fjord, that is, 95.O° east longitude, 29.8° north latitude, and 20 km away from Nanjiabawa peak, and the opposite of the river is the Gallar white base peak at an altitude of 7294 metres. Nanjiabawa Peak, meaning "The snow is burning like a fire." It is a short axially inclined structure that is inclined to the north in the compound folds. The main body of the mountain is gneiss. It mainly consists of three ridges: northwest ridge, northeast ridge and south ridge. The northeastern ridge is about 30 kilometers long and reaches the Yarlung Tsangpo River. There are six ridges above and below 6,000 meters on the ridgeline. There is a guard peak at two kilometers on the southern ridge, which is Pengfeng, 7043 meters above sea level. The "South aid." There are two herringbone ridges extending from south to southeast and southwest respectively from Naipengfeng, and two snow peaks of 6,936 and 7,146 meters are prominent on the northwest Shanken line. The three slopes of the Nanga Bawa Peak are mostly cut into weathered and eroded steep cliffs by snow and ice, with the western slope as the most. The bedrock on the slope is bare, leaving a ditch left by the track and avalanche. The gorge is covered with huge glaciers.
climate
The direction of the Gala White Base peaks is east to west. The main ridge line is lined with southward and northwestern sides with several branch ridges, mostly steep cliffs. There are dozens of glaciers in the valley. Its top is flat and covered with ice and snow all year round. Most of the glaciers in this area belong to oceanic glaciers and they move faster. They are affected by temperature and precipitation, and the steep terrain makes ice and avalanches very frequent. The rainy season in this area is longer, generally extending from May to September, especially in the months of July, August and September. The precipitation is almost daily, and at the same time, the amount of clouds is also very large, and the peaks and clouds are lingering all day long. From November to April of the following year, the weather in 9 dry seasons is dominated by sunny weather. The annual February-April and October-November are alternate periods between the dry season and the rainy season. It is also a good time to choose mountaineering. On this day, the high-altitude winds are strong. The wind speed is 40 meters/second left, and the temperature is -20°C to 30°C.
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