This study aims at assessing the tectonic and climatic responses to landscape changes
transpired in the Durung Drung basin in the Zanskar Himalaya. We used relevant …

Late Cenozoic fluvial successions are widespread in India. They include the deposits of the
Siwalik basin which represent the accumulations of the ancient river systems of the …

This study focuses on the morphotectonic analysis of the Ujh River basin, examining various
aspects related to geometrical changes in the drainage basin caused by tectonic and …

Criteria for identifying alluvial-valley fills in the geological record have commonly been
derived from coastal areas, where high-magnitude glacioeustatic fluctuations generate …

The quantitative and qualitative analysis of the basin is fundamental to understand the
structural and hydrological control of the basin. In the present study morphometric and …

The Ganga basin in northern India is one of the world's largest fluvial basins and has
attracted enormous attention from earth scientists across the globe with a view to …

Alluvial fans are relatively simple depositional systems, due to the direct coupling of
sediment sources and adjacent accumulation areas. Nonetheless, general models of …

Abstract The Piedmont Zone is the least studied part of the Ganga Plain. The northern limit of
the Piedmont Zone is defined by the Himalayan Frontal Thrust (HFT) along which the …

The Himalayan orogenic belt, formed as a result of collision tectonic processes, shows
abundant evidence of neotectonic activity, active tectonics, and the occurrence of historical …

The present study aims to access the geomorphic analysis of the Baghain river basin and its
implication on landscape evolution. Baghain river originates from the Panna hill, and flows …