The blocking of river courses by mass movements is very common in mountainous areas
with deep and narrow valleys. Landslide dams may pose serious threats to people and their …

Channel steepness index, ks, is a metric derived from the stream power model that, under
certain conditions, scales with relative rock uplift rate. Channel steepness index is a property …

Quantitative geomorphic research depends on accurate topographic data often collected via
remote sensing. Lidar, and photogrammetric methods like structure-from-motion, provide the …

Reconstructing the ages and magnitudes of prehistoric extreme events that are recorded in
landforms and sediments allows us to capture the full range of frequency-magnitudes and …

The concavity index,, describes how quickly river channel gradient declines downstream. It
is used in calculations of normalized channel steepness index,, a metric for comparing the …

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 …

Accurate digital elevation models represent the basic tool for a large spectrum of
applications, including geological, architectonic, archaeological, and urbanistic studies …

Along the coast of the hyperarid Atacama Desert, late Quaternary alluvial fans emerge from
the Coastal Cordillera to the Pacific Ocean between 20.5° S and 25.5° S. Coastal alluvial …

The seismically active Saurashtra horst is located within the intraplate volcanic continental
margin of western India. The region is prone to moderate and low-magnitude earthquakes …