Geography in Nepal

For a little nation, Nepal has incredible physical decent variety, extending from the Tarai Plain - the northern edge of the Gangetic Plain arranged at around 300 meters above ocean level in the south - to the very nearly 8,800-meter-high Mount Everest, privately known as Sagarmatha (its Nepali name), in the north. From the swamp Tarai belt, landforms ascend in progressive slope and mountain ranges, including the breathtaking bulwark of the transcending Himalayas, eventually achieving the Tibetan Plateau past the Inner Himalayas.

Nepal normally is partitioned into three expansive physio-graphic zones: the Mountain Region, the Hill Region, and the Tarai Region. Every one of the three parallel one another, from east to west, as persistent environmental belts, once in a while divided by the nation's waterway frameworks. These biological areas were isolated by the legislature into development parts inside the structure of regional advancement planning.

The mountain range is situated above sea level to the north of hill region. It constitutes of central portion of Himalayan range originating in the Pamir’s, a high-altitude region of central Asia. Indeed, the locale is scantily populated, and whatever cultivating action exists is for the most part limited to the low-lying valleys and the stream bowls, for example, the upper Kali Gandaki Valley.

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