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Tsoboje
Tsoboje, also known as Chobuje or Cho Buje, is a mountain in Nepal. Description Tsoboje is a summit in the Nepalese Himalayas. It is set in the Dolakha District of Bagmati Province. Precipitation runoff from the mountain's slopes drains to the Tamakoshi River via Rolwāliṅ Khola. Topographic relief is significant as the summit rises 2,125 metres (6,972 ft) above Tsho Rolpa in . The first ascent of the summit was achieved on April 24, 1972, by Wolfgang Weinzierl, Peter Vogler, Gustav Harder, and Klaus Harder via the east ridge/face. The west face was climbed solo by Mingma Gyalje Sherpa on October 28, 2015. The northwest face was first climbed in October 2021 by Luka Stražar and Nejc Marčič. Climate Based on the Köppen climate classification, Tsoboje is located in a tundra climate zone with cold, snowy winters, and cool summers. Weather systems coming off the Bay of Bengal are forced upwards by the Himalaya mountains (orographic lift), causing heavy precipitati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Takargo (Nepal)
Takargo, also known as Thakar Go or Dragker Go, is a mountain in Nepal. Description Takargo is a summit in the Nepalese Himalayas. It is set in the Dolakha District of Bagmati Province. Precipitation runoff from the mountain's slopes drains to the Tamakoshi River via Rolwāliṅ Khola. Topographic relief is significant as the summit rises over 2,200 metres (7,218 ft) above Tsho Rolpa in . The first ascent of the summit was achieved on March 12, 2010, by David Gottlieb and Joe Puryear via the east face. Climate Based on the Köppen climate classification, Takargo is located in a tundra climate zone with cold, snowy winters, and cool summers. Weather systems coming off the Bay of Bengal are forced upwards by the Himalaya mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Mid-June through early-August is the monsoon season. The months of April, May, September, October, and November offer the most favorable weather for viewing o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Nepal
Most of Nepal is mountainous, and it contains a large section of the Himalayas, the highest mountain range in the world. Eight of the fourteen eight-thousanders are located in the country, either in whole or shared across a border with China or India. Nepal has the highest mountain in the world, Mount Everest at a height of 8,848.86m as well as 1,310 peaks over 6,000 m height. Mountains Other ranges North of the Greater Himalayas in western Nepal, ~6,100 metre ''Tibetan Border Ranges'' form the Ganges-Brahmaputra divide, which the international border generally follows. South of the Greater Himalayas, Nepal has a ''High Mountain'' region of ~4,000 metre summits, then the '' Middle Hills'' and Mahabharat Range with 1,500 to 3,000 metre summits. South of the Mahabharats, an outer range of foothills with ~1,000 metre summits is called the Siwaliks or ''Churiya Hills''. Gallery of highest peaks File:Everest kalapatthar crop.jpg, Everest File:Kanchenjunga from Tiger Hills.JPG, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Bagmati 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
China–Nepal Border
The China–Nepal border is the international boundary between the Tibet Autonomous Region of the China, People's Republic of China and Nepal, Federal Democratic Republic of Nepal. It is in length and runs in a northwest–southeast direction along the Himalayas, Himalayan mountain range, including Mount Everest, the world's highest mountain. The boundaries of this particular border have changed dramatically over time, especially when considering relatively recent events such as the Annexation of Tibet by the People's Republic of China, Annexation of Tibet in 1949. However, some of the most significant developments of modern times would be the signing of the "''Agreement on Maintaining Friendly Relations between the People’s Republic of China and the Kingdom of Nepal''" in 1956 and the "Sino-Nepalese Treaty of Peace and Friendship" in 1960, both of which formally recognised Tibet as a part of China and confirmed the limits of the countries of China and Nepal as they are known ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tengi Ragi Tau
Tengi Ragi Tau, also known as Agole, is a mountain in Nepal. Description Tengi Ragi Tau is a summit on the western boundary of Sagarmatha National Park in the Nepalese Himalayas. It is set on the border shared by the Dolakha District and the Solukhumbu District. Precipitation runoff from the mountain's east slope drains to the Bhotekoshi River, whereas the west slope drains to the Tamakoshi River via Rolwāliṅ Khola. Topographic relief is significant as the summit rises 1,400 metres (4,593 ft) above the Drolambao Glacier in , and 2,560 metres (8,400 ft) above Dig Tsho Lake in . The first ascent of the summit was achieved on December 4, 2002, by Koichi Ezaki, Ruchia Takahashi, Pasang Tamang, and Tul Bahadur Tamang via the southeast face. The second ascent, first via the west face, was made on October 16, 2019, by Tino Villanueva and Alan Rousseau via a route they named ''Release the Kraken''. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sagarmatha National Park
Sagarmāthā National Park is a national park in the Himalayas of eastern Nepal that was established in 1976 and encompasses an area of in the Solukhumbu District. It ranges in elevation from and includes Mount Everest. In the north, it shares the international border with Qomolangma National Nature Preserve in Tibet Autonomous Region. In the east, it is adjacent to Makalu Barun National Park, and in the south it extends to Dudh Kosi river. It is part of the Sacred Himalayan Landscape. History Sagarmatha National Park was established on July 19, 1976. In 1979, it became the country's first national park that was inscribed as a Natural World Heritage Site. In January 2002, a Buffer Zone comprising was added. Conservation of forests, wildlife, and cultural resources received top priority under the ''Buffer Zone Management Guidelines'', followed by conservation of other natural resources and development of alternative energy. Tourism in the area began in the early 1960s. In 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drangnag Ri
Drangnag Ri, also known as Thaknak Ri or Thāngnāk Ri, is a mountain in Nepal. Description Drangnag Ri is a summit on the western boundary of Sagarmatha National Park in the Nepalese Himalayas. It is set on the border shared by the Dolakha District and the Solukhumbu District. Precipitation runoff from the mountain's north slope drains east to the Bhotekoshi River, whereas all other slopes drain to the Tamakoshi River via Rolwāliṅ Khola. Topographic relief is significant as the southwest face rises 1,000 metres (3,280 ft) in 0.5 kilometre (0.31 mi). The first ascent of the summit was achieved on April 30, 1995, by Chris Bonington, Ralph Høibakk, Pem Dorjee Sherpa, Bjørn Myrer Lund, and Lhakpa Gyalu Sherpa.''Asia, Nepal, Drangnag-Ri, First Ascent'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
