The Shey Phoksundo National Park (Nepali: शे-फोकसुण्डो She-Phoksundo) is the largest and only trans-Himalayan national park in Nepal. It was established in 1984 and covers an area of 3,555 km2 (1,373 sq mi) in the districts of Dolpha and Mugu in the Mid western development region, Nepal. The protected area ranges in elevation from 2,130 m (6,990 ft) to 6,885 m (22,589 ft). Pohoksundo Lake is the park's prominent feature, located at an elevation of 3,612 m (11,850 ft).The Park’s climatic differences, altitude variations, and different zoo-geographical regions support a diverse range of biotic systems. In 1998, an area of 1349 km2 surrounding the park was declared as buffer zone, which consists of forests and private lands. The buffer zone is jointly managed by the park and local communities. Together they initiate community development activities and manage the natural and cultural resources.
Additional Description:
Features: Shey Phoksundo National Park provides a diversity of spectacular landscapes. Elevations in the park range from 2,130m in Ankhe to 6,883m at the summit of Kanjiroba Himal. Much of the park lies north of the Himalayan crest. Nepal’s deepest and second largest lake, Phoksundo Lake, lies in upper regions of Suligad. Near the lake’s outlet is the country’s highest waterfall. The major rivers in the park are the Khung, Nmajung and Panjang, The Suligad and Jugdual Rivers, which are the major tributaries of the Thuli Bheri River; and the Langu Rilver, which drains the high dolpo plateau to the east and flows westward. Phoksundo Lake is famous for its magnificent turquoise color and te spectacular scenery clearly rank it with the most scenic mountain parks in the world. Ringmo village, a typical Tibetan village, is scenically nestled in the area. Many beautiful glaciers can be found near and above the lake area. The Park contain many Gompas (Monasteries) and religious area. The most famous, Shey Gompa was established in the 11th Century. Thashung Gompa located near Phoksundo Lake was built about 900 years ago to conserve wildlife.
Climate: As a result of its spanning both the northern and southern aspects of the Himalayan crest, the park experience a wide climatic range. Most of the precipitation in the area occurs during the monsoon (July-September), although the Dhaulagari and Kanjiroba Ranges from a massive barrier preventing most of the rain from reaching the Trans-Himalayan area. The park contains the transition form a monsoon dominated climate with 1500 mm.of annual precipitation in the south (Suligad) to an arid climate with less than 500 mm. a year in the northern slopes. Winters are quite severe, with frequent snowfalls above 2,500m. and temperature’s remaining below freezing above 3,000m. through much of the winter.
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