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Dolakha District
Dolakha, often known as Dolkha or Dholkha (Nepal Bhasa:दोलखा जिल्ला)), a part of Bagmati Province, is one of the seventy-seven districts of Nepal. The district, with Charikot as its district headquarters, covers an area of and had a population of 204,229 in 2001 and 186,557 in 2011. It is a district with a strong religious affiliation. It is popularly known amongst most Nepalese for the temple of Dolakha Bhimeshawor. The name Dolkha arose from Newar Community. In the classical Nepal Bhasa language "Dol" or "Dwal" means Thousand (Hajar), and "Kha" means houses or temple (Ghar va mandirharu) which means "The place that have thousand houses and temples" (Hajar ghar va mandir bhaeko thau). Bhimeshwar Temple The Bhimeshwar temple is located in Dolakha Bazar of Bhimeshwar. The main statue of this temple is God Bhim. Bhimsen, Bhimeshwar, or Bhim of Dolakha is noted as one of the most popular throughout the country. He was the second prince of Panch Pandav and not ... [...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 w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Classical Newar
Classical Newar (Modern: पुलां भाय्, Classical: पुलाङ्गु नेपाल भाय्), also known as Old Newar or Classical Nepal Bhasa, is the pre-1850 literary form of Nepal Bhasa. It is an important source language for historians and linguists. The classical Newari language has also been considered a hybrid in which an extensive Sanskrit superstrate was grafted on to the Tibeto-Burman base. Ancient era The earliest known (dated) document in Nepal Bhasa is called "The Palmleaf from Uku Bahal" which dates back to 1114 AD (235 NS). new, छीन ढाको तृसंघष परिभोग। छु पुलेंग कीत्य बिपार वस्त्र बिवु मिखा तिवु मदुगुन छु सात दुगुनव ल्है।''chīna ḍhākō tr̥saṃghaṣa paribhōga, chu pulēṃga kītya bipāra vastra bivu mikhā tivu maduguna chu sāta dugunava lhai.'' which is a general dis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thangmi Language
Thangmi, also called Thāmī, Thangmi Kham, Thangmi Wakhe, and Thani, is a Sino-Tibetan language spoken in central-eastern Nepal and northeastern India by the Thami people. The Thami refer to their language as ''Thangmi Kham'' or ''Thangmi Wakhe'' while the rest of Nepal refers to it as ''Thāmī''. The majority of these speakers, however, live in Nepal in their traditional homeland of Dolakhā District. In India, the Thami population is concentrated mostly in Darjeeling. The Thangmi language is written using the Devanagari script. Thangmi has been extensively documented by Mark Turin. Distribution Thangmi is spoken in Bagmati Province, mainly in the region of Dolakha; villages on Sailung Khola (The northern panhandle of the Ramechhap District; mainly in Gokulganga); eastern regions of Sindhupalchowk District; and by some elders among the population who migrated to the cities in the Kathmandu Valley. Very few ethnic Thami outside Dolakha and Sindhupalcok districts speak Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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] |
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 Arct ... [...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. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropical Climate
Tropical climate is the first of the five major climate groups in the Köppen climate classification identified with the letter A. Tropical climates are defined by a monthly average temperature of 18 °C (64.4 °F) or higher in the coolest month, and feature hot temperatures all year-round. Annual precipitation is often abundant in tropical climates, and shows a seasonal rhythm but may have seasonal dryness to varying degrees. There are normally only two seasons in tropical climates, a wet (rainy / monsoon) season and a dry season. The annual temperature range in tropical climates is normally very small. Sunlight is intense in these climates. There are three basic types of tropical climates within the tropical climate group: tropical rainforest climate (Af), tropical monsoon climate (Am) and tropical wet and dry climate or tropical savannah (Aw for dry winters, and As for dry summers), which are classified and distinguished by the precipitation and the precipitation lev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
