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 …

The morphological expression of rivers provides a primary medium for human
understanding of river geomorphology and the transmission of geographical information. In …

The evolution of rivers in eroding landscapes plays a key role in determining landscape
relief and modulating climate‐tectonic interactions. A common approach to quantifying river …

Abstract The southern Central Range of Taiwan is in an early stage of orogeny and the
landscape has not yet reached a steady state. To reveal the nature of the transient …

Morphotectonic parameters are sensitive to crustal and/or mantle dynamics, especially in
young convergent margins and contractional orogenic systems. In northwest Africa, the High …

Previous numerical–analytical approaches have suggested that the main range divide
prefers to migrate towards the high uplift flank in the asymmetric tectonic uplift pattern …

We derive erosion rates from detrital zircon fission-track ages and cosmogenic nuclide
concentrations from sediments from the modern rivers of eastern Taiwan in order to …

Abstract The Nepalese Himalaya is well known for ongoing collisional tectonics, witnessed
by major historical and recent earthquakes. The Siwalik Hills in Midwestern Nepalese …

Fold-and-thrust belts (FTBs) develop widely in and around active orogenic belts on Earth.
With the accumulation of structural shortening, thrust-related folds can grow by increasing …

Structural control on drainage patterns has long been suggested to play an important role in
the development of fluvial systems, including their map pattern. Along the western Taiwan …