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To quantitatively measure landscape features we used several classical geomorphic indices (spacing ratio, hypsometric curves and integral, stream frequency drainage, stream length-gradient).
It exhibits high stream frequency drainage and uplift in separate tectonically-uplifted blocks such as Jebel Toubkal which is characterized by asymmetric drainage basins.
Stream frequency (F s) 0.92 17.
The stream frequency shows positive correlation with the drainage density.
The stream frequency of the watershed is 0.04 per ha.
Low stream frequency indicates high permeable geology and low relief.
In the study area, the stream frequency value is 0.92.
Di = Fs/Dd stream frequency (Fs)/drainage density (Dd).
The stream frequency value of the Kanhar basin is 2.45 km/km2.45
The stream frequency relates to permeability, infiltration capability and relief of watershed.
The stream frequency has moderate correlation (loadings of more than 0.60) with third component.
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