The peaks of the ice peaks of the Brahmaputra in the western part of the Himalayan range from the Himalayan to the east along the slopes of the Himalayas. More than 1,000 kilometers of the ice peaks flow to the tail of the eastern section of the Himalayas in Nyingchi, Milin, and Medog. At the junction of the four counties of Bomi, they turned straight to the south and formed a large horseshoe-shaped fjord.
On the inside of this fjord, longitude 95.0° East, and latitude 29.6° North, it is the 15th highest peak in the world and Nanjiababa peak of 7792 meters above sea level. On the outside of the fjord, which is 95.0° east longitude, 29.8° north latitude, 20 km away from Nanjiawa peak, and facing the other side of the river is the Gallas-Bailar peak at 7294 metres above sea level. The Himalayas, which have risen due to the collision of the Indian and Asia-European plates, extend along the east and west. The central part of the Himalayas extends slightly southwards like a “bow†and forms a “ground knot†at the eastern and western ends of the Himalayas, all standing 8125 metres apart. The Nanga Parbat and Namjagbarwa.
The Himalayas stretches more than 2,400 kilometers to the east. This area is blocked by Nyainqentanglha Mountain in the northeast, and the north-south Hengdang Mountain is squeezed, resulting in the Lhasa and Bomi lone wrinkles in the north. On the east side of the belt and the Hengduanshan fault fold belt in southern China. Extremely complex geological formations have formed extremely rugged terrain in the area. The Brahmaputra in the Yarlung Tsangpo River developed along a series of fault zones. With the staged uplift of the Qinghai-Tibet Plateau, the river flow cuts down accordingly, making the peak-to-height difference reach 5000-6000 meters, making it a rare peak in the world.
Moreover, the river is more than 2,800 meters above sea level at the entrance of the fjord and 900 meters above sea level at the exit. The gap is nearly 2,000 meters. The average slope of the river is as low as 10%. Therefore, the river runs swiftly and snarls. The south side of the Big Fjord area directly faces the Indian Ocean, and the warm and wet southwest monsoon can be seen along the Yarlung Zangbo River, causing the land to be affected by the maritime climate. Peaks, canyons, abundant precipitation, and warm temperatures provide good conditions for the vertical zoning of natural geography. At the bottom of the Yarlung Tsangpo River, there is a large, shaded tropical rain forest. Following the slopes, various broad-leaved trees cross each other. The snow line is a piece of ice. It is no exaggeration to say that the Nanga Bawa region is a rare “natural museum†across the tropics and frigid zones.
However, for the mountaineers, Nanjiabawa Peak is so violent. Nanjiabawa Peak, meaning "The snow is burning like a fire." It is a short axially inclined structure in the folds of the compound in the folds of the northern slope. The main body of the mountain is gneiss. It mainly consists of three ridges, a northwestern ridge, a northeastern ridge, and a southern ridge. The northeastern ridge is about 30 kilometers long and reaches the Brahmaputra Bank. There are 6 peaks and undulations above the elevation of 6000 meters above sea level on the ridge line; there is a Weifeng---Naixonfeng, 7043 meters above sea level, two kilometers south of the ridge. Yamaguchi calls it "Southern."
There are two herringbone ridges extending from south to southeast and southwest respectively from Naipengfeng; two peaks of 6936 and 7146m are highlighted on the northwest ridgeline. Most of the three slopes of the Nanga Bawa Peak were cut by snow and ice into weathering and eroding steep rock cliffs, with the western slope as the most. The bedrock on the slope is exposed, leaving a gutter left by the track and avalanche. The gulch is covered with huge glaciers. The direction of the Gala White Base peaks is arranged in an arc of the east and west, with a number of branch ridges accumulating on the main ridge line to the south and northwest, 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 region belong to the glacier type, and they move faster. They are affected by temperature and precipitation, and the terrain is steep. Therefore, ice and avalanches are frequent.
The rainy season in this area is relatively long, generally extending from May to September, especially in the months of July, August and September. It is almost daily precipitation, and the clouds are also very large. From November to April the following year is the dry season. The weather is mainly sunny. From February to October and October to November of each year, it is the replacement period of the dry season and the rainy season. It is also a good time to choose mountaineering. At this time, the high-altitude winds are strong, wind speeds sometimes reach 40 m/s, and gas temperatures range from -20°C to -30°C, with large changes in temperature. The harsh terrain and bad weather have added great difficulties to the climb of Nanjabava. As early as in 1910, British people entered the area and several decades later, mountaineers from various countries made several attempts. From October 30 to October 1992, it was conquered by the united mountaineering team.
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