The landform development and valley floor morphology of active regions is significantly
controlled by tectonic processes. In the present study the upper catchments of Kosi and …

The present study has been carried out with special emphasis on the aggradational
landforms to explain the spatial and temporal variability in phases of aggradation/incision in …

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 northeastern Kumaun part of Kumaun Lesser Himalaya is seismotectonically one of the
most active segments of the Central Himalaya. The major as well as minor thrusts and faults …

The present study has been carried out with special emphasis on the spatial and temporal
variability of sedimentary architecture along the strike length of North Almora Thrust (NAT) …

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

In the Kumaun Himalaya, a portion of the Kosi River valley of~ 90 km in length is chosen to
study the fluvial morphology that provides first‐order information about the dynamic …

Abstract The Main Boundary Thrust marking the tectonic junction between the Lesser
Himalaya and Siwalik molasse represents a zone along which underthrusting still occurs …

The Geomorphic structures in the North Almora Thrust zone (NATZ) have been analyzed to
understand active deformation in the North Almora Thrust zone (NATZ). The NAT is an active …

A section of the Main Boundary Thrust (MBT) in the Kumaun Himalaya suggests recent
extensional tectonic activity. The surface expression of the tectonic activity is faulting of …