Structural Overview and Morphotectonic Evolution of a Strike-Slip Fault in the Zone of North Almora Thrust, Central Kumaun Himalaya, India

Figure 6

(a) Triangular fault facets, colluvial cones, point bar, and abandoned river channel near Naichun; (b) deflecting direction of river flow and meandering channel of Saryu River from Seraghat to Naichun and associated landslides, inset shows close view of huge mass movement activity at right bank of river; (c) meandering of Saryu River with three levels of terraces at Nali; (d) straight river channel with V-shaped valley; (e) landslide along the zone of NAT near Seraghat; (f) the straightening of the Mano gad, a tributary of Saryu River due to reactivation of RF with terrace at Ara.

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