According to Biswas et. al., (1999) morphometric analysis can be used for configuration of the earth’s surface, shape, and dimension of its landforms as well as for prioritization of sub-watersheds (Agarwal, 1998; Biswas et al., 1999; Obi Reddy et. al., 2002).
Hydrological response of a watershed is related with the physiographic features of the drainage basin like size, shape, slope, drainage density and length of the streams (Chorley, 1969; Gregory and Walling 1973).
According to Biswas et. al., (1999) morphometric analysis can be used for configuration of the earth’s surface, shape, and dimension of its landforms as well as for prioritization of sub-watersheds (Agarwal, 1998; Biswas et al., 1999; Obi Reddy et. al., 2002).
Hydrological response of a watershed is related with the physiographic features of the drainage basin like size, shape, slope, drainage density and length of the streams (Chorley, 1969; Gregory and Walling 1973).

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