The Sierra Nevada of the central Betic Cordillera is a 3000m-high mountain range
surrounded by Neogene–Quaternary sedimentary basins, having been uplifted since Late …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

A hypsometric integral (HI) is a topographical index with important geomorphological
meaning. It can both describe the development state of the watershed and reflect the …

The present-day great availability of high-resolution Digital Elevation Models has improved
tectonic geomorphology analyses in their methodological aspects and geological meaning …

Active tectonic deformation influencing the streams and hillslopes of the Sierra Alhamilla
ridge (anticlinorium) in southeast Spain is related to the dextral-reverse Polopos Fault Zone …

Several landscape evolution models have been proposed so far to explain the dynamic
feedback between Earth surface processes and tectonics in the Zagros Mountains …

Tectonics modify the base-level of rivers and result in the progressive erosion of landscapes.
We propose here a new method to classify landscapes according to their erosional stages …

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 …

In terms of hydro-geomorphic characteristics, catchments in Peninsular India remained
mostly unexplored except a few regional and local works that deal with tectonic, structural …

The Mountain Front Flexure marks a dominant topographic step in the frontal part of the
Zagros Fold–Thrust Belt. It is characterized by numerous active anticlines atop of a …