A major question about the Himalaya remains open: does a great earthquake (like the Mw~
8.1 1934 earthquake) release all the strain stored by the Tibet–India convergence during the …

We review the role of landslides in current concepts of the topographic development of
mountain ranges. We find that many studies in this field address basin-or orogen-scale …

ABSTRACT A central question in structural geology is whether, and by what mechanism,
active faults (and the folds often associated with them) grow in length as they accumulate …

We analyze the volume distribution of natural rockfalls on different geological settings (ie,
calcareous cliffs in the French Alps, Grenoble area, and granite Yosemite cliffs, California …

Bedrock landslides shape topography and mobilize large volumes of sediment. Yet,
interactions between landslide‐produced sediment and fluvial systems that together govern …

The Po Plain is a low-relief area characterised by active shortening accommodated by blind
thrust faulting. In this almost flat region depositional rates are similar to tectonic rates and …

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 …

The morphological boundary between the Himalayas and the foreland plain is well
expressed and most often corresponds to the frontal emergence of the Main Himalayan …

The active growth of a fault-and-thrust belt in frontal zones of Himalaya is a prominent
topographical feature, extending 2500 km from Assam to Pakistan. In this paper, kinematical …

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 …