Siwalik Range

Siwalik Range

 

the southern and lowest step of the Himalayas, located in India and Nepal between the Pir Panjal and Mahabharat ranges. In a broader sense, the range encompasses the southern fringe of the entire system of Himalayan foothills from Kashmir to the Tista River—a length of approximately 1,700 km. Rising abruptly above the Indo-Gangetic Plain, the mountains form a chain of parallel ridges and ranges extending from northwest to southeast, with elevations to 2,591 m (Mount Saonchalia).

The Siwalik Range is built of dislocated series of molasses composed of gravel, sandstones, and conglomerates. It is separated from the Great Himalayas by the main boundary fault, along which lies a system of lenticular valleys; the range is highly seismic. The slopes are deeply dissected by rivers. Mud streams are typical of the western section of the southern slope; swampy jungles in the Terai area characterize the eastern foot of the southern slope. Tropical deciduous (monsoon) forests are found on the slopes; those in the west receive less precipitation than those in the east. In many places the vegetative cover has been seriously damaged as a result of excessive grazing and timbering operations, and there is intensive formation of gullies. A sizable section of the slopes has been artificially terraced and is used for tea plantations.

L. I. KURAKOVA [23–1015–]

References in periodicals archive ?
At the dam site, the river continues through the foothills of Siwalik range and nally enters the plains of Punjab.
The Siwalik Range also called the Sub Himalaya, is the youngest of all, and abuts the plains as foothills dipping to the north.
Pokhrel (2010) The construction of Kohalpur-Surkhet road found as the main causative factor to result landslides and sedimentation problems in many section of the road alignment area in geologically weak Siwalik range and steep hill slopes area of the region (Pokhrel,2010).
Desertification process in geologically weak inner mountain valleys and Siwalik range were found to be suffered from the adverse effect of land use changes.
MORPHOMETRY AND SEDIMENT DYNAMICS OF THE CHURIYA RIVER AREA, SIWALIK RANGE IN NEPAL.
The Siwalik Range (Churiya Range) extends E-W with a width of 10-20 km and rises from the Ganges Plain to an altitude of about 1500 m amsl (above mean sea level).
The Siwalik Range with 1000 m high hills makes distinct contrast with the Mahabharat Range.
02 % between the emergence in the Siwalik Range and the outlet point (FIGURE 2).
The sediments of these terrace deposits were mostly derived from the Lesser Himalayan Ranges from the north during Mid Pleistocene, and were then reworked by the north flowing streams originated from the Siwalik Range of southern region of RRB between Late Pleistocene and Holocene (Kimura, 1994).