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Pabil
Pabil, also known as Ganesh IV, is a mountain in Nepal. Description Pabil is a glaciated summit in the Ganesh Himal subrange of the Himalayas. It is situated north-northwest of Kathmandu on the common boundary shared by Bagmati Province and Gandaki Province. The peak ranks as the highest point in Dhading District and the 69th-highest in Nepal. Precipitation runoff from the mountain's slopes drains into tributaries of the Budhi Gandaki River. Topographic relief is significant as the west face rises 1,100 metres (3,609 ft) in , the northeast slope rises 2,300 metres (7,546 ft) in , and the south slope rises 3,900 metres (12,800 ft) in . The first ascent of the summit was achieved on October 20, 1978, via the south face and southeast ridge by T. Tomita, H. Yoshio, K. Aoyagi, M. Hashimoto, Y. Hashimoto, Y. Okuma, T. Shimoji, T. Suzuki, I. Yasuda, Yogendra Thapa, Kamal Bhandari, Mingma Tenzing Sherpa, and Sonan Wolang Sherpa. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ganesh Himal
Ganesh Himāl is a sub-range of the Himalayas located mostly in north-central Nepal, but some peaks lie on the border with Tibet. The Trisuli Gandaki valley on the east separates it from the Langtang Himal; the Budhi (Buri) Gandaki valley and the Shyar Khola valley on the west separate it from the Sringi Himal and the Mansiri Himal (home of Manaslu, the nearest eight-thousander, 8000m peak). The highest peak in the range is Yangra with an elevation of . Three other peaks are over and fourteen others over . The name for the range comes from the Hindu deity Ganesha, usually depicted in the form of an elephant. Names and elevations for this range differ from source to source; see the notes below the table. The least ambiguous way to refer to the different peaks would be "Ganesh NW", but this is not the standard practice in the literature for this range. Highest peaks Notes # The names Ganesh II, Salasungo (Ganesh III), and Pabil (Ganesh IV) are from the FinnmapFinnmap topograph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dhading District
Dhading District ( ), a part of Bagmati Province, is one of the seventy-seven districts of Nepal. The district, with Dhading Besi as its district headquarters, covers an area of , had a population of 338,658 in 2001 and 336,067 in 2011. Geography and climate Dhading District spreads from 27'40" E to 28'17" E and 80'17"N to 84'35"N. The mountain range Ganesh Himal is the predominant mountain range located within Dhading. Some of the peaks are over . The highest point in the district is 7,104-metre Pabil. The and the mountain Manaslu is clearly visible from much of Dhading, although it is located within the bounds of Gorkha. The transnational Prithivi Highway connecting Kathmandu and Pokhara runs through the southern portion of the district, making for easy access to the Kathmandu valley. The road parallels the Trishuli River. The western border with Gorkha is bisected by the Budigandaki River. The district is bounded by *East: Kathmandu, Rasuwa and Nuwakot *West: Gorkh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yangra
Yangra (Ganesh I) is the highest peak of the Ganesh Himal, which is a subrange of the Himalayas. Although not an eight-thousander, 8,000 metre peak, and little visited, it enjoys great vertical relief over the nearby valleys. __NOTOC__ Location Yangra, and the entire Ganesh Himal, lie between the Budhi Gandaki and Trisuli Gandaki valleys, northwest of Kathmandu. Yangra lies on the border between Nepal and Tibet, and is east-southeast of Manaslu, the nearest 8,000 meter peak. Climbing history The Ganesh Himal was first seriously reconnoitered for climbing by H. W. Tilman and party in 1950. The first attempt on the peak was in 1953. The first ascent, in 1955, was by a France, Franco-Switzerland, Swiss expedition led by Raymond Lambert, via the Southeast Face and Ridge. The ascent was most notable for the presence of a woman, Claude Kogan, in the summit party, which was very rare at the time. Lambert, Kogan, and Eric Gauchat achieved the summit, but Gauchat fell to his death ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ganesh NW (Ganesh II/III)
Ganesh NW (or Ganesh II, or sometimes Ganesh III) is a peak of the Ganesh Himal, which is a subrange of the Himalayan range. Ganesh NW, and the entire Ganesh Himal, lie between the Budhi Gandaki and Trisuli Gandaki valleys, about northwest of Kathmandu. Ganesh NW lies about seven km west of Yangra (Ganesh I). Nomenclature for this peak is ambiguous and confusing, and varies between sources. Many sources refer to this peak as Ganesh III, and also as Salasungo. However Salasungo more properly refers to a different peak in the Ganesh Himal, Ganesh SE or Ganesh III. The name Ganesh II is used on the Finnmap, the most recent authoritative source. __NOTOC__ Notable features Although low in elevation among the major mountains of Nepal, Ganesh NW is exceptional in its steep rise above local terrain. For example, it rises from the Burhi Gandaki in a horizontal distance of about . Climbing history There were six unsuccessful attempts on this peak, including attempts in 1953 and 1954, b ... [...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] |
Mountains Of The Gandaki 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 ... [...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] |
Salasungo
Salasungo (also known as Ganesh III/IV, Ganesh SE, Sangjing Ri, Tsala Sungo, Chaglasumgo or Kang LomboE. Jurgalski at 8000ers.comHimalayan Database) is a peak of the Ganesh Himal, on the border between Nepal and Tibet (China). Salasungo, and the entire Ganesh Himal, lie between the Burhi Gandaki and Trisuli Gandaki valleys, about 70 km northwest of Kathmandu. Salasungo lies about 6 km south of Yangra Yangra (Ganesh I) is the highest peak of the Ganesh Himal, which is a subrange of the Himalayas. Although not an eight-thousander, 8,000 metre peak, and little visited, it enjoys great vertical relief over the nearby valleys. __NOTOC__ Location ... (Ganesh I). The name "Salasungo" is also often used to refer to another peak located 4 km further west, Ganesh NW. Nomenclature and altitude Nomenclature for this peak is ambiguous and confusing, and varies between sources. The mountain was previously known as Ganesh II till resurveyed in the early 1990s. Elder map ... [...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] |
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] |
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] |
