The last few years have witnessed consistent growth in paleoseismic investigations and
active fault research in India. An overview of relevant publications during 2016-2020 …

Torrential rains, landslides, and seismic activity are the common factors that are causing
unprecedented damage to life, property and infrastructure in Mandakini and Bhilangana …

Active surface deformation, displacement pattern, and erosional variability is estimated
using the geomorphologically sensitive morphometry along with the Persistent Scatterer …

The study of drainage patterns in tectonically active regions is conducive to the prediction of
regional geomorphology. Subtle subsurface changes can be detected by drainage …

The consequence of strain accumulation along various Himalayan thrusts is manifested in
shaping the topography and present day lanscape features of the Himalaya. Consequently …

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 …

In the northwest Himalayan region, the ongoing out-of-sequence deformation caused
emergence of Back Thrust (BT) around 43ka, which attributed the growth of anticlines …

The present research emphasizes to delineate the active tectonic features in the Kashmir
Himalaya by quantitatively analysing the Chenab River basin (CRB) of the NW Himalayas …

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 …

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