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Rasuwa District
Rasuwa District ( ne, :ne:रसुवा जिल्ला, रसुवा जिल्ला is one of 13 districts of Bagmati Province and one of seventy-seven districts of Nepal. The district, with Dhunche as its district headquarters, covers an area of and has a population (2011) of 43,300. As per census 2011 total households in Rasuwa district is 9,778. It is the smallest district by area, among 16 districts in the ''Himalaya'' region of Nepal. Etymology Origin of its name had begun as 'Rasowa' which is believed to be derived as a combination of two Tibetan words ''ra'' (meaning: lambs) and ''sowa'' (meaning: grazing) as it was known for its lamb and grazing lands. And later people started to call it Rasuwa. Geography and climate Its territory has elevations ranging from from mean sea Level. Forests cover 31.43% of the land while 16.63% is always snow-covered. Steeply varying territory and plenty of natural blessings make Rasuwa a well-known tourist destination in Nepal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Standard Tibetan
Lhasa Tibetan (), or Standard Tibetan, is the Tibetan dialect spoken by educated people of Lhasa, the capital of the Tibetan Autonomous Region of China. It is an official language of the Tibet Autonomous Region. In the traditional "three-branched" classification of Tibetic languages, the Lhasa dialect belongs to the Central Tibetan branch (the other two being Khams Tibetan and Amdo Tibetan). In terms of mutual intelligibility, speakers of Khams Tibetan are able to communicate at a basic level with Lhasa Tibetan, while Amdo speakers cannot. Both Lhasa Tibetan and Khams Tibetan evolved to become Tone (linguistics), tonal and do not preserve the word-initial consonant clusters, which makes them very far from Classical Tibetan, especially when compared to the more Linguistic conservatism, conservative Amdo Tibetan. Registers Like many languages, Lhasa Tibetan has a variety of Register (sociolinguistics), language registers: * (Wylie transliteration, Wylie: , literally "wikt:demot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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: 26,494,504 *Increase since last census 2001: 3,343,081 *Annual population growth rate (exponental growth): 1.35 *Number of households ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Langtang
Langtang valley is a Himalayan valley in the mountains of north-central Nepal, known for its trekking routes and natural environment. Administrative The Langtang valley lies in the Rasuwa district of the Bagmati Province in Nepal. Situated 80 kilometres north of the Kathmandu Valley, the valley lies within the Langtang national park, which borders the Tibet autonomous region of China. Prior to the 2015 earthquake, 668 individuals are estimated to have lived within the Langtang valley. Ecology The Langtang valley lies within the Langtang National Park. The park contains a wide variety of climatic zones, from subtropical to alpine. Approximately 25% of the park is forested. Trees include the deciduous oak and maple, evergreens like pine, and various types of rhododendron. Animal life includes the Himalayan black bear, Himalayan tahr, Assam macaque, snow leopard, yak, red panda and more than 250 species of birds. Culture Among themselves, the local inhabitants of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Desert Climate
The desert climate or arid climate (in the Köppen climate classification ''BWh'' and ''BWk''), is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive. Covering 14.2% of earth's land area, hot deserts are the second most common type of climate on earth after the polar climate. There are two variations of a desert climate according to the Köppen climate classification: a hot desert climate (''BWh''), and a cold desert climate (''BWk''). To delineate "hot desert climates" from "cold desert climates", there are three widely used isotherms: most commonly a mean annual temperature of , or sometimes the coldest month's mean temperature of , so that a location with a ''BW'' type climate with the appropriate temperature above whichever isotherm is being used is classified as "hot arid sub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
