Gurudongmar (mountain)
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Gurudongmar (mountain)
Gurudongmar is a mountain in northern India. Description Gurudongmar is a glaciated double summit in the Himalayas. The lower peak, Gurudongmar West, rises to an elevation of 6,630 metres and is 1.6 km west of the main summit. The mountain is situated in the state of Sikkim, north of the capital city of Gangtok. Precipitation runoff from this mountain's slopes drains north into the Teesta River drainage basin and south into the Lachung River drainage basin. Topographic relief is significant as the northeast slope rises 1,165 metres (3,822 ft) in . The first ascent of Gurudongmar was achieved in 1936 by Eric Shipton and Edwin Kempson via the west ridge.''Gurudongmar''
G. T. Bhutia, The Himalayan Journal, 2025, The Himalayan Club, Retrieved June 10, 2025.
However, the possibility exists that they only climbe ...
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Khangchengyao
Khangchengyao is a mountain peak located at north-west of Yumesodong, North Sikkim in the Eastern Himalayas. Location Khangchengyao is a revered peak among the locals. It is the 4th highest peak in Sikkim and 10th highest peak in India India, officially the Republic of India, is a country in South Asia. It is the List of countries and dependencies by area, seventh-largest country by area; the List of countries by population (United Nations), most populous country since .... As per folklore, Khangchengyao is known as the ''Male Deity''. References Mountains of Sikkim Six-thousanders of the Transhimalayas {{Sikkim-geo-stub ...
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Edwin Kempson (mountaineer)
Edwin Garnett Hone Kempson (1902–1987) was a schoolmaster at Marlborough College (1925–1967), Mayor of Marlborough (1946) and a member of the British expeditions to Everest in 1935 and 1936. Biography Edwin Kempson was the son of Edwin Hone Kempson, he was born on 4 June 1902 in Castletown, Isle of Man. After schooling at Marlborough College (1916–1921) he went on to study mathematics at University of Cambridge where he was awarded a first-class degree and developed an interest in mountainerring. He returned to Marlborough College where he taught maths from 1925 to 1967 and for a short period in 1961 he was Acting Master of the School. Kempson married Margaret Cecilia Lloyd on 11 April 1939. He was mayor of Marlborough, Wiltshire in 1946. He died on 25 May 1987. Mountaineering Kempson was a member of both the 1935 British Mount Everest reconnaissance expedition and the 1936 British Mount Everest expedition. His experience when he first went to Everest amounted to around ...
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Mountains Of India
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ...
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Chombu
Chombu is a mountain peak with elevation located in the north of Sikkim, India. Location The peak is located in a relatively isolated part of North Sikkim North Sikkim (now officially named as Mangan District) is a district of the Indian state of Sikkim. Its district headquarters is Mangan. It is the seventh least populous district in the country (out of 640). Geography Mangan is the largest ..., along the path that leads to the Thangu-Yumesandong pass. The prominence is . Climbing history There are no documented ascents of Chombu. Also, due to its proximity to the Tibetan border, climbing on it is strictly controlled. Attempts In 2019 and 2022, two mountaineers from London made three attempts to climb the summit, but they were unsuccessful. The peak is still unconquered. References Mountains of Sikkim Six-thousanders of the Transhimalayas {{Sikkim-geo-stub ...
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Sanglaphu
Sanglaphu is a mountain peak location at in northeast of Sikkim, India. Location The mountain is part of the Dongkya range. On its western flank, the water flows from ''Gurudongmar Glacier'' to Gurudongmar Lake, which lies in the headwaters of the Lachen Chu, which in turn feeds the Teesta River. On the opposite side of the glacier is the main summit of Gurudongmar . The southern flank of the Sanglaphu is drained from the Lachung Chu. There is also the mountain lake ''Sanglaphu Cho'' at an altitude of . Climbing history Sanglaphu was first climbed on October 1, 1991, by mountaineers from Sonam Gyatso Mountaineering Institute, Gangtok Gangtok (, ) is the capital and the most populous city of the Indian state of Sikkim. The seat of East Sikkim district, eponymous district, Gangtok is in the eastern Himalayas, Himalayan range, at an elevation of . The city's population of 100 .... The team consisted of Kalden, Beniwal, Tamang, Dawa, Passang, Nima Sangay, Choudhary, Rawa ...
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Tibet Autonomous Region
The Tibet Autonomous Region (TAR), often shortened to Tibet in English or Xizang in Pinyin, Hanyu Pinyin, is an Autonomous regions of China, autonomous region of the China, People's Republic of China. It was established in 1965 to replace the Tibet Area (administrative division), Tibet Area, a former administrative division of the Republic of China (1912–1949), Republic of China. The current borders of the Tibet Autonomous Region were generally established in the 18th century and include about half of Tibet, cultural Tibet, which was at times independent and at times under Mongol or Chinese rule. The TAR spans more than and is the second-largest Administrative divisions of China, province-level division of China by area. Due to its harsh and rugged terrain, it has a total population of only 3.6 million people or approximately . Names and etymologies Tibet Autonomous Region is often shortened to Tibet in English or Xizang in Hanyu Pinyin. The earliest official record of the ...
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Geology Of The Himalayas
The geology of the Himalayas is a record of the most dramatic and visible creations of the immense mountain range formed by plate tectonic forces and sculpted by weathering and erosion. The Himalayas, which stretch over 2400 km between the Namcha Barwa syntaxis at the eastern end of the mountain range and the Nanga Parbat syntaxis at the western end, are the result of an ongoing orogeny — the collision of the continental crust of two tectonic plates, namely, the Indian Plate thrusting into the Eurasian Plate. The Himalaya-Tibet region supplies fresh water for more than one-fifth of the world population, and accounts for a quarter of the global sedimentary budget. Topographically, the belt has many superlatives: the highest rate of uplift (nearly 10 mm/year at Nanga Parbat), the highest relief (8848 m at Mt. Everest Chomolangma), among the highest erosion rates at 2–12 mm/yr, the source of some of the greatest rivers and the highest concentratio ...
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Orographic Lift
Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation. Orographic lifting can have a number of effects, including precipitation, rain shadowing, leeward winds, and associated clouds. Precipitation Precipitation induced by orographic lift occurs in many places throughout the world. Examples include: * The Mogollon Rim in central Arizona * The western slope of the Sierra Nevada range in California. * The western slope of the Wasatch Range in Utah. Specifically the Little and Big Cottonwood Canyons. * The mountains near Baja California North – specifically La Bocana to Laguna Hanson. * The windward slopes of Khasi and Jayantia Hills (see Mawsynram) in the state of Meghalaya in India. * The Western Highlands of Yemen, which rece ...
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Tundra Climate
The tundra climate is a polar climate sub-type located in high latitudes and high mountains. It is classified as ET according to the Köppen climate classification. It is a climate which at least one month has an average temperature high enough to melt snow (), but no month with an average temperature in excess of . If the climate occurs at high elevations, it is known as alpine climate. Despite the potential diversity of climates in the ''ET'' category involving precipitation, extreme temperatures, and relative wet and dry seasons, this category is rarely subdivided. Rainfall and snowfall are generally slight due to the low vapor pressure of water in the chilly atmosphere, but as a rule potential evapotranspiration is extremely low, allowing soggy terrain of swamps and bogs even in places that get precipitation typical of deserts of lower and middle latitudes. The amount of native tundra biomass depends more on the local temperature than the amount of precipitation. Tundra ...
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