Geography of Nepal
Nepal
GEOGRAPHY
Location and Size: Landlocked between China and India; total land area 147,181 square kilometers.
Topography: Mountainous and hilly, although with physical diversity. Three broad physiographic areas run laterally--lowland Tarai Region in south; central lower mountains and hills constituting Hill Region; high Himalayas, with 8,796-meters-high Mount Everest and other peaks forming Mountain Region in north.
Of total land area, only 20 percent cultivatable. Deforestation severe problem; by 1988 forests covered approximately 30 percent of land area.
Climate: Five climatic zones based on altitude range from subtropical in south, to cool summers and severe winters in north. Annual rainfall with seasonal variations depending on monsoon cycle, which provides 60 to 80 percent of total annual rainfall; 2,500 millimeters in eastern part of country; 1,420 millimeters around Kathmandu; 1,000 millimeters in western Nepal.
The Land
Source: Based on information from Leo E. Rose and John T. Scholtz, Nepal: Profile of a Himalayan Kingdom, Boulder, 1980, 4; Nanda R. Shreshtha, Landlessness and Migration in Nepal, Boulder, 1990, 6; and Pitamber Sharma, Urbanization in Nepal, Honolulu, May 1989, 132.
Sandwiched between two Asian giants--China and India--Nepal traditionally has been characterized as "a yam caught between two rocks." Noted for its majestic Himalayas, which in Sanskrit means the abode of snow, Nepal is very mountainous and hilly.
Its shape is roughly rectangular, about 650 kilometers long and about 200 kilometers wide, and comprises a total of 147,181 square kilometers of land. It is slightly larger than Bangladesh or the state of Arkansas. Nepal is a landlocked country, surrounded by India on three sides and by China's Xizang Autonomous Region (Tibet) to the north. It is separated from Bangladesh by an approximately fifteenkilometer -wide strip of India's state of West Bengal, and from Bhutan by the eighty-eight-kilometer-wide Sikkim, also an Indian state. Such a confined geographical position is hardly enviable. Nepal is almost totally dependent on India for transit facilities and access to the sea--that is, the Bay of Bengal--even for most of the goods coming from China.
For a small country, Nepal has great physical diversity, ranging from the Tarai Plain--the northern rim of the Gangetic Plain situated at about 300 meters above sea level in the south--to the almost 8,800-meter-high Mount Everest, locally known as Sagarmatha (its Nepali name), in the north. From the lowland Tarai belt, landforms rise in successive hill and mountain ranges, including the stupendous rampart of the towering Himalayas, ultimately reaching the Tibetan Plateau beyond the Inner Himalayas. This rise in elevation is punctuated by valleys situated between mountain ranges. Within this maze of mountains, hills, ridges, and low valleys, elevational (altitudinal) changes rersulted in ecological variations.
Nepal commonly is divided into three broad physiographic areas: the Mountain Region, the Hill Region, and the Tarai Region (see fig. 4). All three parallel each other, from east to west, as continuous ecological belts, occasionally bisected by the country's river systems. These ecological regions were divided by the government into development sectors within the framework of regional development planning.
The rhythm of life in Nepal, as in most other parts of monsoonal Asia, is intricately yet intrinsically intertwined with its physical environment. As scholar Barry Bishop learned from his field research in the Karnali region in the northwest, the livelihood patterns of Nepal are inseparable from the environment.
Data as of September 1991
Next: Chronology | Climate
GEOGRAPHY
Location and Size: Landlocked between China and India; total land area 147,181 square kilometers.
Topography: Mountainous and hilly, although with physical diversity. Three broad physiographic areas run laterally--lowland Tarai Region in south; central lower mountains and hills constituting Hill Region; high Himalayas, with 8,796-meters-high Mount Everest and other peaks forming Mountain Region in north.
Of total land area, only 20 percent cultivatable. Deforestation severe problem; by 1988 forests covered approximately 30 percent of land area.
Climate: Five climatic zones based on altitude range from subtropical in south, to cool summers and severe winters in north. Annual rainfall with seasonal variations depending on monsoon cycle, which provides 60 to 80 percent of total annual rainfall; 2,500 millimeters in eastern part of country; 1,420 millimeters around Kathmandu; 1,000 millimeters in western Nepal.
The Land
Source: Based on information from Leo E. Rose and John T. Scholtz, Nepal: Profile of a Himalayan Kingdom, Boulder, 1980, 4; Nanda R. Shreshtha, Landlessness and Migration in Nepal, Boulder, 1990, 6; and Pitamber Sharma, Urbanization in Nepal, Honolulu, May 1989, 132.
Sandwiched between two Asian giants--China and India--Nepal traditionally has been characterized as "a yam caught between two rocks." Noted for its majestic Himalayas, which in Sanskrit means the abode of snow, Nepal is very mountainous and hilly.
Its shape is roughly rectangular, about 650 kilometers long and about 200 kilometers wide, and comprises a total of 147,181 square kilometers of land. It is slightly larger than Bangladesh or the state of Arkansas. Nepal is a landlocked country, surrounded by India on three sides and by China's Xizang Autonomous Region (Tibet) to the north. It is separated from Bangladesh by an approximately fifteenkilometer -wide strip of India's state of West Bengal, and from Bhutan by the eighty-eight-kilometer-wide Sikkim, also an Indian state. Such a confined geographical position is hardly enviable. Nepal is almost totally dependent on India for transit facilities and access to the sea--that is, the Bay of Bengal--even for most of the goods coming from China.
For a small country, Nepal has great physical diversity, ranging from the Tarai Plain--the northern rim of the Gangetic Plain situated at about 300 meters above sea level in the south--to the almost 8,800-meter-high Mount Everest, locally known as Sagarmatha (its Nepali name), in the north. From the lowland Tarai belt, landforms rise in successive hill and mountain ranges, including the stupendous rampart of the towering Himalayas, ultimately reaching the Tibetan Plateau beyond the Inner Himalayas. This rise in elevation is punctuated by valleys situated between mountain ranges. Within this maze of mountains, hills, ridges, and low valleys, elevational (altitudinal) changes rersulted in ecological variations.
Nepal commonly is divided into three broad physiographic areas: the Mountain Region, the Hill Region, and the Tarai Region (see fig. 4). All three parallel each other, from east to west, as continuous ecological belts, occasionally bisected by the country's river systems. These ecological regions were divided by the government into development sectors within the framework of regional development planning.
The rhythm of life in Nepal, as in most other parts of monsoonal Asia, is intricately yet intrinsically intertwined with its physical environment. As scholar Barry Bishop learned from his field research in the Karnali region in the northwest, the livelihood patterns of Nepal are inseparable from the environment.
Data as of September 1991
Next: Chronology | Climate
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