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Chang Himal
Chang Himal, also known as Ramthang Chang or Wedge Peak, is a mountain in Nepal. Description Chang Himal is a glaciated summit in the Nepalese Himalayas. It is situated northwest of Kangchenjunga in the Kanchenjunga Conservation Area. Precipitation runoff from the mountain's slopes drains into the Ghunsa River which is a tributary of the Tamur River. Topographic relief is significant as the summit rises 1,820 metres (5,971 ft) above the Kangchenjunga Glacier in . The first ascent of the summit was made on October 5, 1974, by Janez Gradisar, Bojan Pollak, and Michael Smolej via the southwest ridge.''Chang Himal Overview''
Nepal Himal Peak Profile, Retrieved April 12, 2025.
The north face was first climbed October 29 – November 2, 2009, by Nick Bullock and Andy Houseman (1800 m, ED+ M6).


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Kangbachen
Kangbachen is a subsidiary peak of Kangchenjunga in the Nepalese part of the Himalayas. The Kangchenjunga massif's local name translates to "Five treasures of the high snow" in reference to its five peaks, one being Kangbachen. Kangbachen lies on the west ridge of the Kangchenjunga range, in Nepal. It is the smallest of Kangchenjunga's five peaks and the only one less than eight thousand meters (7,903 m). It is also the only one of Kangchenjunga's peaks entirely in Nepal. Kangbachen has rarely been climbed compared to other mountains on the range. It has only had ten recorded expeditions since 1930, and only two successful summits, according to the The Himalayan Database, ''Himalayan Database''. It was first summitted on May 26, 1974, via the southwest ridge by a Polish expedition team, composed of Kazimierz Olech, Wiesław Kłaput, Marek Malatyński, Zbigniew Rubinowski and Wojciech Brański. The second successful summit, by a Yugoslavian team, took place just over four months ...
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Bay Of Bengal
The Bay of Bengal is the northeastern part of the Indian Ocean. Geographically it is positioned between the Indian subcontinent and the Mainland Southeast Asia, Indochinese peninsula, located below the Bengal region. Many South Asian and Southeast Asian Countries of the Bay of Bengal, countries are dependent on the Bay of Bengal. Geopolitically, the bay is bounded on the west and northwest by India, on the north by Bangladesh, and on the east by Myanmar and the Andaman and Nicobar Islands of India. Its southern limit is a line between Sangaman Kanda, Sri Lanka, and the northwesternmost point of Sumatra, Indonesia. Cox's Bazar Beach, Cox's Bazar, the longest sea beach in the world and Sundarbans, the largest mangrove forest and the natural habitat of the Bengal tiger, are located along the bay. The Bay of Bengal occupies an area of . A number of large rivers flow into the Bay of Bengal: the Ganges–Hooghly River, Hooghly, the Padma River, Padma, the Brahmaputra River, Brahmaputr ...
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Mountains Of Koshi Province
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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Merra
Merra, or Merrā, is a mountain in Nepal. Description Merra is a glaciated summit in the Nepalese Himalayas. It is situated west-northwest of Kangchenjunga in the Kanchenjunga Conservation Area. Precipitation runoff from the mountain's slopes drains into the Ghunsa River which is a tributary of the Tamur River. Topographic relief is significant as the summit rises 2,130 metres (6,988 ft) above the Ghunsa River in . The first ascent of the summit was made on October 18, 2006, by Claus Ostergaard.''Merra Overview''
Nepal Himal Peak Profile, Retrieved April 14, 2025.


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Based on the , Merra is located in a



Nepal Peak (Himalayas)
Nepal Peak is a mountain in the Himalayas. It lies on the border between Nepal and India. Location The peak is located at above sea level in the extreme northeast of Nepal and northwest of Sikkim. It is approximately 2km southwest of Kirat Chuli. Climbers ascending Kirat Chuli from the Nepal Gap, by the southwest ridge, usually traverse the summit of Nepal Peak. Climbing history The first ascent was made in late May 1930 by , a member of an international expedition which included climbers from Germany, Austria, Switzerland and the UK and was led by Günter Dyhrenfurth. Schneider ascended Nepal Peak by himself. Until Schneider went on to make the first ascent of Jongsong Peak Jongsong Peak is a mountain in the ''Janak'' section of the Himalayas. At it is the 57th highest peak in the world, although it is dominated by the 3rd highest, Kangchenjunga, to the south. Jongsong's summit is on tripoint of India, Nepal an ... just a few days later on 2 June 1930, Nepal Pe ...
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Kirat Chuli
Kirat Chuli or Tent Peak is a mountain in the Himalayas. It lies on the border between Nepal and India. Location The peak is located at above sea level in the extreme northeast of Nepal and northwest of Sikkim. It is approximately 2km northeast of Nepal Peak. Climbing history The first ascent to the summit was made by Ernst Grob, Herbert Paidar, and Ludwig Schmaderer in 1939. See also * Kirata * Kirata Kingdom * Kirati people * Kirat Mundhum Kirat Mundhum, (Nepali language, Nepali: किरात मुन्धुम) also known as Kiratism, or Kirati Mundhum, is a traditional belief of the Kirati people, Kirati ethnic groups of Nepal, Darjeeling and Sikkim, majorly practiced by Yak ... References Mountains of Sikkim India–Nepal border International mountains of Asia Seven-thousanders of the Himalayas Mountains of Koshi Province Sacred mountains of Nepal {{Sikkim-geo-stub ...
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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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Himalayas
The Himalayas, or Himalaya ( ), is a mountain range in Asia, separating the plains of the Indian subcontinent from the Tibetan Plateau. The range has some of the Earth's highest peaks, including the highest, Mount Everest. More than list of highest mountains on Earth, 100 peaks exceeding elevations of above sea level lie in the Himalayas. The Himalayas abut on or cross territories of Himalayan states, six countries: Nepal, China, Pakistan, Bhutan, India and Afghanistan. The sovereignty of the range in the Kashmir region is disputed among India, Pakistan, and China. The Himalayan range is bordered on the northwest by the Karakoram and Hindu Kush ranges, on the north by the Tibetan Plateau, and on the south by the Indo-Gangetic Plain. Some of the world's major rivers, the Indus River, Indus, the Ganges river, Ganges, and the Yarlung Tsangpo River, Tsangpo–Brahmaputra River, Brahmaputra, rise in the vicinity of the Himalayas, and their combined drainage basin is home to some 6 ...
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Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ...
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