Rugged peaks, large intermontane basins and frequent seismicity all characterize the active
extensional tectonic setting of the southern Apennines. The Matese ridge typifies the active …

It is generally agreed that the channel‐head steady‐state elevations (zs) across a drainage
divide are different when the drainage divide is moving. However, whether it is the hillslope …

The Chenghai Fault in the Chuan–Dian block terminates at the northwestern segment of the
Red River Fault, and is a significant seismogenic structure. The kinematic evolution of this …

Drainage divides are dynamic features of a landscape that migrate over time during the
development of river networks. In this study, we focused on the geomorphic response of a …

The stability of drainage divides is widely used for tectonic reconstruction. A drainage divide
migrating from the high-uplift side towards the geometric center is usually thought to indicate …

A main drainage divide is a high terrain that separates neighboring drainage basins. It is
dynamic through time and naturally evolves towards a steady state, which depends on …

Studies have shown that the growth of the Qilian Shan, the northeastern margin of the
Tibetan Plateau, started~ 10 Ma ago. However, when and how it expanded northwards is …

Active faults within the southern Apennines fold-and-thrust belt modulate the present-day
upwelling of hydrothermal fluids at surface. In the Monte Alpi area, we investigated the …

Drainage divides play significant roles in sha** landscapes. Nevertheless, they are not
static through space and time. Previous numerical models have demonstrated divide …

Mountain asymmetry is defined by the ratio of the lengths of two river systems across a
drainage divide and is determined by the normalized location of the drainage divide …