Abstract In the Sub-Himalayan zone, the frontal Siwalik range abuts against the alluvial plain
with an abrupt physiographic break along the Himalayan Frontal Thrust (HFT), defining the …

Numerous newly-identified traces of active faults in the Himalayan foothill zone along the
HFF around Chandigarh, in Pinjore Dun, along the piedmont zone of the Lower Siwalik hill …

The Himalaya has experienced three great earthquakes during the last century—1934
Nepal‐Bihar, 1950 Upper Assam, and arguably the 1905 Kangra. Focus here is on the …

This paper focuses on the analysis of geomorphic landform development, particularly
between the Trans Himadri Fault and the Main Central Thrust including Berinag Thrust and …

The central sector of the Himalaya is under very strong compressive strain. Almost all thrusts
that define the boundaries of lithotectonic terranes of the Kumaun Himalaya are active …

Youngest of the five terrane-defining faults, the Himalayan Frontal Fault (HFF) is a series of
reverse faults that demarcates the boundary of the Siwalik front of the Himalayan province …

Until Neolithic times in the middle Holocene, the populated Lesser Himalaya was a gentle
terrain of low relief, less than a thousand metres above sea level, and the Stone-Age people …

Abstract The Kumaun Himalaya is considered as the most active part of the Central Seismic
gap in the Indian Sub-continent. In this paper, we presented active surface deformation rates …

An episode of neotectonic activity on an east–west trending fault in the zone of active
intracrustal North Almora Thrust in the eastern Kumaun Himalaya resulted in the formation of …

We have analysed the geomorphic signatures in aggregation with the geomorphic indices
with respect to hinterland and foreland neotectonic variability across the major Himalayan …