Namcha barwa

"Scroll to left" Namche Barwa Weather (Days 0-3): A heavy fall of snow, heaviest during Fri night. Extremely cold (max -13\°C on Fri afternoon, min -15\°C on Fri night). Winds decreasing (fresh winds from the WSW on Fri afternoon, calm by Sat night). (Days 3-6): A heavy fall of snow, heaviest during Tue night. Extremely cold (max -11\°C on Wed afternoon, min -14\°C on Tue morning). Winds decreasing (fresh winds from the WSW on Mon night, light winds from the NW by Wed night). (Days 6-9): A moderate fall of snow, heaviest on Thu afternoon. Extremely cold (max -13\°C on Thu afternoon, min -16\°C on Fri night). Winds decreasing (strong winds from the NNW on Fri afternoon, calm by Sat night). (Days 10-12): A heavy fall of snow, heaviest during Tue morning. Temperatures will be well below freezing (max -10\°C on Tue afternoon, min -13\°C on Sun night). Winds increasing (calm on Sun night, fresh winds from the WSW by Mon night). light snow snow shwrs some clouds snow shwrs snow shwrs snow shwrs light snow snow shwrs snow shwrs snow shwrs snow shwrs mod. snow light snow snow shwrs some clouds snow shwrs snow shwrs snow shwrs snow shwrs snow shwrs some clouds clear snow shwrs snow shwrs some clouds snow shwrs snow shwrs snow shwrs snow shwrs snow shwrs snow shwrs snow shwrs light snow light snow -15 -14 -14 -14 -13 -13 -13 -12 -13 -13 -12 -12 -13 -11 -12 -12 -13 -13 -14 -14 -15 -14 -14 -13 -13 -12 -12 -12 -11 -11 -11 -10 -10 -11 -10 -10 -10 -9 -9 -9 -9 -8 -9 -9 -8 -8 -9 -7 -8 -7 -...

29°09′22″N 93°58′59″E / 29.156°N 93.983°E / 29.156; 93.983 The Yarlung Tsangpo Grand Canyon, also known as the Yarlung Zangbo Grand Canyon, the Tsangpo Canyon, the Brahmaputra Canyon or the Tsangpo Gorge ( 雅魯藏布大峽谷; Yǎlǔzàngbù Dàxiágǔ'), is a Canyon depth [ ] Map all coordinates using: Download coordinates as: As the canyon passes between the peaks of the overall is about 2,268 m (7,440 feet), the deepest depth reaches 6,009 m (19,714 feet). This is the deepest canyon on land. [ citation needed] This part of the canyon is at 29°46′11″N 94°59′23″E / 29.769742°N 94.989853°E / 29.769742; 94.989853 ( Tsangpo Canyon, 16,000 feet deep). Namcha Barwa, 7,782 m (25,531 feet) high, is at 29°37′33″N 95°03′26″E / 29.62583°N 95.05722°E / 29.62583; 95.05722 ( Namjabarwa), and Gyala Peri, at 7,234 m (23,733 feet), is at 29°48′48″N 94°58′02″E / 29.81333°N 94.96722°E / 29.81333; 94.96722 ( Gyala Peri). Ecosystem [ ] The gorge has a unique The Everest of Rivers [ ] Map all coordinates using: Download coordinates as: Western interest in the Tsangpo began in the 19th century when British explorers and geographers speculated where Tibet's east-flowing Tsangpo ended up, suspecting the Brahmaputra. Since British citizens were not allowed to enter Tibet they recruited Indian " In 1913, The area was closed after China invaded Tibet and disputed the location of the The largest waterfalls of the gorge (near Tsangpo Badong, 藏布巴东瀑布群 There are two waterfalls in this section: Rainbow Falls (about 21 metr...

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In …Kashmir region, and Namjagbarwa (Namcha Barwa) Peak (25,445 feet [7,756 metres]), in the Tibet Autonomous Region of China. Between those western and eastern extremities lie the two Himalayan countries of Nepal and Bhutan. The Himalayas are bordered to the northwest by the mountain ranges of the Hindu Kush

The presence of unique elevated low relief relict landscape in the transient Dibang catchment, at the orographic edge of Tibet-Himalaya in the tectonically active Namcha Barwa syntaxial zone, is modelled to understand evolving regional landscape, drainage reorganization and tectonics. This elevated low relief landscape represents a Mio-Pliocene abandoned paleo-channel of the Yarlung river, which was captured by the headward eroding Siang river owing to >600 m base level advantage. The river capture caused isolation of the Dibang river, which evolved as a transient parched catchment since 3–6 Ma after loss of ~17 times drainage area and 4–17 times discharge. The drainage area and discharge gained by the Siang river triggered enormous incision causing aneurysm leading to the accelerated growth of the Tsangpo gorge and affected regional tectonics. This paleo-drainage reorganization is reflected in the Mio-Pliocene sedimentation pattern in the southern Tibet-Himalaya and foreland basins. The landscape evolution in an active mountain belt is a function of competing processes of tectonic uplift and erosion into positive feedback by the drainage system in-situ development of low relief upland in a transient system in-situ evolution as parched low relief landscape with decreased erosion potential of the channel leading to a net surface uplift viz. erosion [E]

Namche Barwa Trekking Namche Barwa Trekking Normally the trekking starts from Lhasa via Samye and Tsedang; which is close to the Indian border area. The trail follows the route of the Tsangpo river and reaches to the village of Lusha which is located at a big bend in the river. During trekking, interval trail passes through several villages of the Loba people who belong to (a Tibetan minority group), But we follow the route which passes through the forested region of Pei that leads to the Namche Barwa Base Camp. Hence the low elevation of the base camp area (1600 m) offers incredible views of the vertical snow-capped peak of mighty Namche Barwa. Nepal Wonders Treks & Expedition P. Ltd provides a tailor-made itinerary as per trekkers interest and Holiday schedule. We will like to assure you that all the trip goes well. So that you could accomplish your mission to trek around this pristine land. Namche Barwa Trekking