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Rasuwa District
Rasuwa District ( 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. Its District Post Office (DPO) has a Rasuwa DPO code of 45000. There are five post offices in the district. As per census 2011 total households in Rasuwa district were 9,778. It is the smallest district by area, among 16 districts in the ''Himalaya'' region of Nepal. Etymology The name, formerly ''Rasowa'', is believed to be derived from two Tibetan words ''ra'' (lamb) and ''sowa'' (grazing), as it was known for its lamb and grazing lands. 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. Sightseeing places including Gosaikunda Lake, Langtan ... [...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 into municipalities and rural municipalities. There are seven provinces and 77 districts in Nepal. After the 2015 reform of administrative divisions, Nawalparasi District and Rukum District were respectively divided into Parasi District and Nawalpur District, and Eastern Rukum District and Western Rukum District. District officials 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 the Provincial Assembly to establish coordination between the Provincial Assembly and rural muni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Districts Of Bagmati Province
Bagmati Province is divided into 13 districts. A district is administrated by the head of the District Coordination Committee and the District Administration Officer. The districts are further divided to municipalities or rural municipalities. 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 the Provincial Assembly to establish coordination between the Provincial Assembly and rural municipalities and municipalities and to settle disputes, if any, of political nature. It also maintains coordination between the provincial and Federal government and the local bodies in the district. See als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Standard Tibetan
Lhasa Tibetan or Standard Tibetan is a standardized dialect of Tibetan spoken by the people of Lhasa, the capital of the Tibetan Autonomous Region. It is an official language of the Tibet Autonomous Region. In the traditional "three-branched" classification of the 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 tonal and do not preserve the word-initial consonant clusters, which makes them very far from Classical Tibetan, especially when compared to the more conservative Amdo Tibetan. Registers Like many languages, Lhasa Tibetan has a variety of language registers: * ( Wylie: , literally " demotic language"): the vernacular speech. * ( Wylie: , "honorifics or deference, courtesy"): the ... [...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 in cooperation with the 58 municipalities and the 3,915 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 in 2001: 3,343,081 *Annual population growth rate (exponential growth): 1.35 * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Langtang
Langtang Valley () also known as Lamtang 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 Rasuwa District, Rasuwa district of the Bagmati Province in Nepal. Situated about 80 kilometres north of the Kathmandu Valley, the valley lies within the Langtang National Park, which borders the Tibet Autonomous Region in Southwest China. Prior to the 2015 earthquake, 668 individuals were estimated to be living within the 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 Asiatic black bear, Himalayan black bear, Himalayan tahr, Monkey, Red monkey, languer Assam macaque, snow leopard, yak, red ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an mean, average surface level of one or more among Earth's coastal Body of water, 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 Navigation, marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to Calibration, calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead a long-term average of tide gauge readings at a particular reference location. The term ''above sea level'' generally refers to the height above mean sea level (AMSL). The term APSL means above present sea level, comparing sea levels in the past with the level today. Earth's radius at sea level is 6,378.137 km (3,963.191 mi) at the equator. It is 6,356.752 km (3,94 ... [...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", a mean annual temperature of is used as an isotherm so that a location with a ''BW'' type climate with the appropriate temperature above this isotherm is classified as "hot arid subtype" (''BWh''), and a location with the appropriate temperature below the isotherm is classified as "cold a ... [...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 and 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperate Climate
In geography, the temperate climates of Earth occur in the middle latitudes (approximately 23.5° to 66.5° N/S of the 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; they usually differ only in the amount of precipitation. In temperate climates, not only do latitudinal positions influence temperature changes, but various 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 persistence of frost. However, some adaptations of Köppen set the minimum at . Continental climates are classified as D and considered to be varieties of temperate climates, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subtropics
The subtropical zones or subtropics are geographical and climate zones immediately 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° to 40° 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 (Köppen climate classification: Cfa/Cwa), where rainfall is often concentrated in the warmest months, for example Southeast China and the Southeastern United States, and dry summer or Mediterranean climate (Köppen climate classification: 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 an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. Nepal has a very high degree of geographic diversity and can be divided into three main regions: Terai, Hilly, and Himal. The Terai region, covering 17% of Nepal's area, is a lowland region with some hill ranges and is culturally more similar to parts of India. The Hilly region, encompassing 68% of the country's area, consists of mountainous terrain without snow and is inhabited by various indigenous ethnic groups. The Himal region, covering 15% of Nepal's area, contains snow and is home to several high mountain ranges, including Mount Everest, the world's highest peak. Nepal, with elevations ranging from less than 100 meters to over 8,000 meters, has eight climate zones from tropical to perpe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
