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Manang District, Nepal
Manang District ( ne, मनाङ जिल्ला , a part of Gandaki Province, is one of the seventy-seven districts of Nepal. The district, with Chame as its district headquarters, covers an area of and had a population (2011) of 6,538. The pass of Thorung La at 5415 meters above the sea connects the district to Mustang District by providing a route between the towns of Manang and Muktinath. Manang district gets least amount of rainfall among districts of Nepal as it lies to the north of the Himalayas which blocks monsoon air. The Manang Valley, which lies close to the Nepal-Tibet border, offers tremendous opportunities due to its rich natural flora and fauna. Three tracks start from here. The first, via Thorangla, Muktinath, and Mustang to Lhasa—a journey that takes four days; the second via Naur Khola and Naurgaon, which takes five days to Lhasa; and finally the third via Larkiya bazar, which is the one most commonly used by the people of Central Nepal. Along with ...
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Districts Of Nepal
Districts in Nepal are second level of administrative divisions after provinces. Districts are subdivided in municipalities and rural municipalities. There are seven provinces and 77 districts in Nepal. After the state's reconstruction of administrative divisions, Nawalparasi District and Rukum District were divided into Parasi District (officially Nawalparasi (West of Bardaghat Susta) District) and Nawalpur District (officially Nawalparasi (East of Bardaghat Susta) District), and Eastern Rukum District and Western Rukum District respectively. District official include: * Chief District Officer, an official under Ministry of Home Affairs is appointed by the government as the highest administrative officer in a district. The C.D.O is responsible for proper inspection of all the departments in a district such as health, education, security and all other government offices. * District Coordination Committee acts as an executive to the District Assembly. The DCC coordinates with ...
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Manang
Manang ( ne, मनाङ) is a town in the Manang District of Nepal. It is located at 28°40'0N 84°1'0E with an elevation of . According to the preliminary result of the 2011 Nepal census it has a population of 6,527 people living in 1,495 individual households. Its population density is 3 persons/km2.. It is situated in the broad valley of the Marshyangdi River to the north of the Annapurna mountain range. The river flows to the east. To the west, the Thorong La pass leads to Muktinath shrine and the valley of the Gandaki River. To the north there is the Chulu East peak of . Most groups trekking around the Annapurna range will take resting days in Manang to acclimatize to the high elevation, before taking on Thorong La pass. The village is situated on the northern slope, which gets the most sunlight and the least snow cover in the winter. The cultivation fields are on the north slope with terraces. There are now motorable road as well as trails where goods are transported on ...
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Sherpa Language
Sherpa (also Sharpa, Xiaerba, or Sherwa) is a Tibetic language spoken in Nepal and the Indian state of Sikkim, mainly by the Sherpa. The majority speakers of the Sherpa language live in the Khumbu region of Nepal, spanning from the Chinese (Tibetan) border in the east to the Bhotekosi River in the west. About 200,000 speakers live in Nepal (2001 census), some 20,000 in Sikkim (1997) and some 800 in Tibetan Autonomous Region (1994). Sherpa is a subject-object-verb (SOV) language. Sherpa is predominantly a spoken language, although it is occasionally written using either the Devanagari or Tibetan script. Phonology Sherpa is a tonal language. Sherpa has the following consonants: Consonants * Stop sounds can be unreleased in word-final position. * Palatal sounds can neutralize to velar sounds when preceding . * can become a retroflex nasal when preceding a retroflex stop. * can have an allophone of when occurring in fast speech. Vowels * Vowel sounds have the ...
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Tamang Language
Tamang (Devanagari: तामाङ; ''tāmāng'') is a term used to collectively refer to a dialect cluster spoken mainly in Nepal, Sikkim, West Bengal (Darjeeling) and North-Eastern India. It comprises Eastern Tamang, Northwestern Tamang, Southwestern Tamang, Eastern Gorkha Tamang, and Western Tamang. Lexical similarity between Eastern Tamang (which is regarded as the most prominent) and other Tamang languages varies between 81% to 63%. For comparison, lexical similarity between Spanish and Portuguese, is estimated at 89%. Ethnologue report for Spanish Dialects ''Ethnologue'' divides Tamang into the following varieties due to mutual unintelligibility. *Eastern Tamang: 759,000 in Nepal (2000 WCD). Population total all countries: 773,000. Sub-dialects are as follows. **Outer-Eastern Tamang (Sailung Tamang) **Central-Eastern Tamang (Temal Tamang) **Southwestern Tamang (Kath-Bhotiya, Lama Bhote, Murmi, Rongba, Sain, Tamang Gyoi, Tamang Gyot, Tamang Lengmo, Tamang Tam) *Western T ...
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Nepali Language
Nepali (; , ) is an Indo-Aryan language native to the Himalayas region of South Asia. It is the official, and most widely spoken, language of Nepal, where it also serves as a '' lingua franca''. Nepali has official status in the Indian state of Sikkim and in the Gorkhaland Territorial Administration of West Bengal. It is spoken by about a quarter of Bhutan's population. Nepali also has a significant number of speakers in the states of Arunachal Pradesh, Assam, Himachal Pradesh, Manipur, Meghalaya, Mizoram and Uttarakhand. In Myanmar it is spoken by the Burmese Gurkhas. The Nepali diaspora in the Middle East, Brunei, Australia and worldwide also use the language. Nepali is spoken by approximately 16 million native speakers and another 9 million as a second language. Nepali is commonly classified within the Eastern Pahari group of the Northern zone of Indo-Aryan. The language originated from the Sinja Valley, Karnali Province then the capital city of the Khasa K ...
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Gurung Language
Gurung (Devanagari: ), also known as Tamu Kyi (, ; Tibetan: ) or Tamu Bhaasaa (, ), is a language spoken by the Gurung people of Nepal. The total number of all Gurung speakers in Nepal was 227,918 in 1991 and 325,622 in 2011. The official language of Nepal, Nepali, is an Indo-European language, whereas Gurung is a Sino-Tibetan language. Gurung is one of the major languages of Nepal, and is also spoken in India, Bhutan, and by diaspora communities in countries such as Singapore and Hong Kong. Geographical distribution Gurung is spoken in the following districts of Nepal and India (''Ethnologue''): *Gandaki Province: Kaski District, Syangja District, Lamjung District, Tanahu District, Gorkha District, Manang District and Mustang *Dhawalagiri Zone: Parbat district *Sikkim: South Sikkim, West Sikkim, East Sikkim Classification At higher levels, Gurung is a member of the Tibeto-Burman (or Trans-Himalayan) family. Robert Shafer classified Gurung within the Bodic division, sub-gro ...
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2011 Nepal Census
Nepal conducted a widespread national census in 2011 by the Nepal Central Bureau of Statistics. Working with the 58 municipalities and the 3915 Village Development Committees at a district level, they recorded data from all the municipalities and villages of each district. The data included statistics on population size, households, sex and age distribution, place of birth, residence characteristics, literacy, marital status, religion, language spoken, caste/ethnic group, economically active population, education, number of children, employment status, and occupation. *Total population in 2011: 26,494,504Central Bureau of Statistics of Nepal: ''Major Highlights''.
*Increase since last census 2001: 3,343,081 *Annual population growth rate (exponental growth): 1.35 *Number of households ...
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Snow Line
The climatic snow line is the boundary between a snow-covered and snow-free surface. The actual snow line may adjust seasonally, and be either significantly higher in elevation, or lower. The permanent snow line is the level above which snow will lie all year. Background Snow line is an umbrella term for different interpretations of the boundary between snow-covered surface and snow-free surface. The definitions of the snow line may have different temporal and spatial focus. In many regions the changing snow line reflect seasonal dynamics. The final height of the snow line in a mountain environment at the end of the melting season is subject to climatic variability, and therefore may be different from year to year. The snow line is measured using automatic cameras, aerial photographs, or satellite images. Because the snow line can be established without on-the-ground measurements, it can be measured in remote and difficult to access areas. Therefore, the snow line has become an ...
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Montane Ecology
Montane ecosystems are found on the slopes of mountains. The alpine climate in these regions strongly affects the ecosystem because temperatures fall as elevation increases, causing the ecosystem to stratify. This stratification is a crucial factor in shaping plant community, biodiversity, metabolic processes and ecosystem dynamics for montane ecosystems. Dense montane forests are common at moderate elevations, due to moderate temperatures and high rainfall. At higher elevations, the climate is harsher, with lower temperatures and higher winds, preventing the growth of trees and causing the plant community to transition to montane grasslands, shrublands or alpine tundra. Due to the unique climate conditions of montane ecosystems, they contain increased numbers of endemic species. Montane ecosystems also exhibit variation in ecosystem services, which include carbon storage and water supply. Life zones As elevation increases, the climate becomes cooler, due to a decrease in a ...
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Temperate Climate
In geography, the temperate climates of Earth occur in the middle latitudes (23.5° to 66.5° N/S of Equator), which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation changes. In temperate climates, not only do latitudinal positions influence temperature changes, but sea currents, prevailing wind direction, continentality (how large a landmass is) and altitude also shape temperate climates. The Köppen climate classification defines a climate as "temperate" C, when the mean temperature is above but below in the coldest month to account for the persistency of frost. However, other climate classifications set the minimum at . Zones and climates The north temperate zone extends from the Tropic of Cancer (approximately 23.5° north latitude) to the Arctic ...
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Subtropics
The subtropical zones or subtropics are geographical and climate zones to the north and south of the tropics. Geographically part of the temperate zones of both hemispheres, they cover the middle latitudes from to approximately 35° north and south. The horse latitudes lie within this range. Subtropical climates are often characterized by hot summers and mild winters with infrequent frost. Most subtropical climates fall into two basic types: humid subtropical (Koppen climate Cfa), where rainfall is often concentrated in the warmest months, for example Southeast China and the Southeastern United States, and dry summer or Mediterranean climate (Koppen climate Csa/Csb), where seasonal rainfall is concentrated in the cooler months, such as the Mediterranean Basin or Southern California. Subtropical climates can also occur at high elevations within the tropics, such as in the southern end of the Mexican Plateau and in Da Lat of the Vietnamese Central Highlands. The six climate cl ...
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Geography Of Nepal
Nepal measures about along its Himalayan axis by across. It has an area of . Nepal is landlocked by China's Tibet Autonomous Region to the north and India on other three sides. West Bengal's narrow ''Siliguri Corridor'' separate Nepal and Bangladesh. To the east are Bhutan and India. Landform regions For a country of its size, Nepal has tremendous geographic diversity. It rises from as low as elevation in the tropical Terai—the northern rim of the Gangetic Plain, through beyond the perpetual snow line to 90 peaks over including Earth's highest ( Mount Everest or ''Sagarmatha''). In addition to the continuum from tropical warmth to cold comparable to polar regions, average annual precipitation varies from as little as in its narrow proportion of the rainshadow north of the Himalayas to as much as on windward slopes, the maximum mainly resting on the magnitude of the South Asian monsoon. Forming south-to-north transects, Nepal can be divided into three belts: Terai, ...
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