Gorkha District
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Gorkha District
Gorkha District ( ne, गोरखा जिल्ला ), a part of Gandaki Province, is one of the 77 districts of Nepal, which is the fourth largest district (by area) of Nepal and connected historically with the creation of the modern Nepal and the name of the legendary Gorkha soldiers. The district, with Gorkha Municipality (previously known as Prithivi Narayan Nagarpalika) as its district headquarters, covers an area of and has a population of 252,201 according to the 2021 Nepal census. Gorkha district is the site of the Manakamana Temple. The temples of Gorakh Nath and Gorakh Kali are found in the district. Several major rivers—the Chepe, Daraudi, Marsyangdi, Budi Gandaki, and Trishuli—run through the district. Origin"Gorkha" * * Myth holds that a saint named Gorakhnath appeared for the first time in Nepal in Gorkha. There remains a cave with his ''paduka'' ('footprint') and a likeness which supports the myth. As the city was established in the place where Sage ...
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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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Gorakh Nath
Gorakh Kalyan is a raga in Hindustani classical music. Its name is attributed to its origins in a regional type of song of Gorakhpur in Uttar Pradesh. Since it does not resemble Kalyan Kalyan (Pronunciation: Help:IPA/Marathi, əljaːɳ is a city on the banks of Ulhas River in Thane district of Maharashtra state in Konkan division. It is governed by Kalyan-Dombivli Municipal Corporation. Kalyan is a subdivision (Taluka) ... very much, some musicians prefer to just call it ''Gorakh''. References Hindustani ragas {{India-music-stub ...
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Manaslu
Manaslu ( ne, मनास्लु, also known as Kutang; muh-NAA-slu) is the eighth-highest mountain in the world at above sea level. It is in the Mansiri Himal, part of the Nepalese Himalayas, in the west-central part of Nepal. The name Manaslu means "mountain of the spirit" and is derived from the Sanskrit word ''manasa'', meaning "intellect" or "soul". Manaslu was first climbed on May 9, 1956, by Toshio Imanishi and Gyalzen Norbu, members of a Japanese expedition. It is said that, given the many unsuccessful attempts by the British to climb Everest before New Zealander Edmund Hillary, "just as the British consider Everest their mountain, Manaslu has always been a Japanese mountain".Mayhew, p. 326 Manaslu is the highest peak in the Gorkha District and is about east of Annapurna. The mountain's long ridges and valley glaciers offer feasible approaches from all directions and culminate in a peak that towers steeply above its surrounding landscape and is a dominant feature wh ...
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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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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 ...
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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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Paduka
''Paduka'' is an ancient form of footwear in India, consisting of a sole with a post and knob which is positioned between the big and second toe. It has been historically worn in South Asia and Southeast Asia. ''Paduka'' exist in a variety of forms and materials. They might be made in the shape of actual feet, or of fish, for example, and have been made of wood, ivory and silver. They may be elaborately decorated, such as when used as part of a bride's trousseau, but could also be given as religious offerings or themselves be the object of veneration. Although simple wooden ''padukas'' could be worn by common people, ''padukas'' of fine teak, ebony and sandalwood, inlaid with ivory or wire, were a mark of the wearer's high status. In the modern world, ''padukas'' are worn as footwear by mendicants and saints of Hinduism, Buddhism,and Jainism. Its significance in Hinduism is linked to the epic ''Ramayana''. ''Paduka'' can also refer to the footprints of deities and saints that ar ...
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Gorakshanath
Gorakhnath (also known as Goraksanath, c. early 11th century) was a Hindu yogi, saint who was the influential founder of the Nath Hindu monastic movement in India He is considered one of the two notable disciples of Matsyendranath. His followers, found all over India, are called yogis, ''Gorakhnathi'', ''Darshani'' or ''Kanphata''. He was one of nine saints also known as Navnath and is widely popular in Maharashtra, India. Hagiographies describe him as more than a human teacher and someone outside the laws of time who appeared on earth in different ages. Historians state Gorakhnath lived sometime during the first half of the 2nd millennium CE, but they disagree in which century. Estimates based on archaeology and text range from Briggs' 15th to 12th century to Grierson's estimate of the 14th century. Gorakhnath is considered a ''Maha-yogi'' (or great yogi) in the Hindu tradition. He did not emphasise a specific metaphysical theory or a particular Truth, but emphasised that the ...
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Trishuli River
The Trishuli River ( ne, त्रिशूली नदी) is one of the major tributaries of the Narayani River basin in central Nepal. It originates in Tibet as a stream and enters Nepal at Gyirong Town. Etymology The Trishuli is named after the ''trishula'' or trident of Shiva, the most powerful god in the Hindu pantheon, There is a legend that says high in the Himalayas at Gosaikunda, Shiva drove his trident into the ground to create three springs – the source of the river and hence its name Trisuli. Course The stream in Tibet crosses the Nepalese border at Gyirong Town, with the Kyirong gorge opens out at Ragma (3000 m). Thereafter, it flows through Nepal and joins at Devghat the Narayani River, which at a lower stage flows into India and joins the Ganges. Basin data More than 60 per cent of the total drainage basin of the Trishuli lies in Tibet with about 9 per cent being covered by snow and glaciers. 85 per cent of its catchment area of lies above out of which 11 per ...
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