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It is an area of steep relief, high rainfall, and very high erosion. In Uttarakhand, the Lesser Himalayas is a homogeneous physiographic unit. In Nepal it can be subdivided into the Lesser Himalayas 24 Ganga–Brahmaputra–Meghna Waters proper, grading to the north into the ranges of High Himalayas; the midland valleys and basin, the most populous part of Nepal with elevations in the range of 600 to 2000 m; and the Mahabharat ranges which rise to altitudes of up to 3000 m. Rivers of the Nepalese Himalayas, which generally follow the east–west trend of the Midland valleys, cut through the Mahabharat in very narrow, deep gorges.

Secondly, a macro as well as micro development of the GBM basin is being emphasized, as detailed later. Therefore, the environmental system is described in considerable detail. The biotic characteristics have undergone considerable change with the growing population and economic development. The abiotic factors, land and water, have also been considerably perturbed. We will first consider them in their natural state. 1. 0137 Source: Encyclopaedia Britannica, 1982. With permission. 2 Location and Physical Geography The GBM basin occupies a dominant position, located in the northern and northeastern part of the Indian subcontinent between north latitudes 21°58’ and 31°30’ and east longitudes 73°30’ and 97°50’.

To the south) over the advancing mass. The individual ranges generally present a steep face toward the south and a gentler inclined slope toward the north. The extremities of the range are generally considered to be marked by the two “syntaxes” or great bends of the Indus in Kashmir and the Brahmaputra in upper Assam. On the southern end of the Himalayas is the Indian peninsular shield consisting of Aravali, the Vindhyan ranges and Southeastern plateau. They traverse almost the whole width of peninsular India.

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