For over a century, geomorphologists have attempted to unravel information about
landscape evolution, and processes that drive it, using river profiles. Many studies have …

The landscape, developed by the interaction of geological processes, is represented by
Digital Elevation Models (DEMs) of various spatial resolutions. These DEMs can be …

The eastern margin of the Tibetan Plateau represents one of the morphologically most active
regions on Earth, where the interplay of recent crustal deformation and subsequent fluvial …

Landscape evolution is driven by factors like tectonics and climate, and unraveling such
factors can reveal the history recorded in landscape morphology. The northern US …

Streams commonly respond to base‐level fall by localizing erosion within steepened,
convex knickzone reaches. Localized incision causes knickzone reaches to migrate …

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 …

Two empirically consistent explanations exist for the morphology and dynamics of bedrock
rivers. The stream power law appears to explain rates of rock incision at large scale (large …

Exploring the long-term mechanism of hazard formation and identifying prospective hazard
areas is critical for human survival and the risk management of crucial engineering facilities …

The distribution of rock uplift rates in the interior of the western Qilian Shan is not yet fully
resolved, which limits our knowledge about the uplift pattern and landscape evolution in the …

River is one of the geomorphic units that are the most sensitive to tectonic activity, of which
the longitudinal profile serves as a key archieve to record information on active tectonics …