This video, titled ‘Filling in Nepal in Minecraft’, was uploaded by IsaakGeoEmpire (Anti UTTP) on 2023-12-16 15:00:08. It has garnered 29 views and 1 likes. The duration of the video is 00:01:55 or 115 seconds.
Nepals geography :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 perpetual snow. The majority of the country’s population resides in the tropical and subtropical climate zones. The tropical zone, below 1,000 meters, experiences frost less than once per decade and is suitable for growing various fruits and crops. The subtropical climate zone, from 1,000 to 2,000 meters, is the most prevalent and suitable for growing rice, maize, millet, wheat, and other crops. The temperate climate zone, from 2,000 to 3,000 meters, occupies 12% of Nepal’s land area and is suitable for cold-tolerant crops. The subalpine, alpine, and nival zones have progressively fewer human settlements and agricultural activities.
Seasons are divided into a wet season from June to September and a dry season from October to June. The summer monsoon can cause flooding and landslides, while the winter monsoon is marked by occasional rainfall and snowfall. The diverse elevation results in various biomes, including tropical savannas, subtropical and temperate forests, montane grasslands, and shrublands.
Nepal has three categories of rivers: the largest systems (Koshi, Gandaki/Narayani, Karnali/Goghra, and Mahakali), second category rivers (rising in the Middle Hills and Lower Himalayan Range), and third category rivers (rising in the outermost Siwalik foothills and mostly seasonal). These rivers can cause serious floods and pose challenges to transportation and communication networks. River management involves addressing flooding, sedimentation, and sustainable water sources for irrigation. Building dams in Nepal is controversial due to seismic activity, glacial lake formation, sedimentation rates, and cross-border equity issues between India and Nepal.
Nepal’s land cover is dominated by forests, which cover 39.09% of the country’s total geographical area, followed by agriculture areas at 29.83%. The hill region constitutes the largest portion of Nepal, with significant cultivated lands and natural vegetation. Forests in Nepal face deforestation due to over-harvesting of firewood, illegal logging, clearing for agriculture, and infrastructure expansion. As of 2010, 64.8% of the forested area in Nepal is covered by core forests of more than 500 ha in size. Deforestation and degradation are driven by multiple processes, including firewood harvesting, construction, urban expansion, and illegal logging.
Nepal has consistently been ranked as one of the most polluted countries in the world.[2][3][4][5][6][7]
Landform regions For a country of its size, Nepal has tremendous geographic diversity. It rises from as low as 59 metres (194 ft) elevation in the tropical Terai—the northern rim of the Gangetic Plain, through beyond the perpetual snow line to 90 peaks over 7,000 metres (22,966 ft) including Earth’s highest (8,848-metre (29,029 ft) 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 160 millimetres (6.3 in) in its narrow proportion of the rainshadow north of the Himalayas to as much as 5,500 millimetres (216.5 in) on windward slopes, the maximum .
Himal
Perspective view of the Himalayas and Mount Everest as seen from space looking south-south-east from over the Tibetan Plateau. (annotated version) Himal Region is a mountainous region containing snow. The Mountain Region begins where high ridges (Nepali: लेक; lekh) begin substantially rising above 3,000 metres (10,000 ft) into the subalpine and alpine zone which are mainly used for seasonal pasturage. By geographical view, it covers 15% of the total area of Nepal. A few tens kilometers further north the high Himalaya abruptly rise along the Main Central Thrust fault zone above the snow line at 5,000 to 5,500 metres (16,400 to 18,000 ft). Some 90 of Nepal’s peaks exceed 7,000 metres (23,000 ft) and eight exceed 8,000 metres (26,247 ft) including Mount Everest at 8,848 metres (29,029 ft) and Kanchenjunga at 8,598 metres (28,209 ft).
There are some 20 subranges including the Kanchenjunga massif along with the Mahalangur Himal around Mount Everest. Langtang north of Kathmandu, Annapurna and Manaslu north of Pokhara, then Dhaulagiri further west with Kanjiroba north of Jumla and finally Gurans Himal in the far west.