Drainage divides separate Earth's surface into individual river basins. Divide migration
impacts the evolution of landforms, regional climate, ecosystems and biodiversity. In this …

The study of fluvial network rearrangement provides a key to understand past and future
landscape evolution. Large perturbations of hydrographic basins such as the change from …

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 …

Drainage divide migration is of wide interest because it drives changes in topography,
aquatic species habitat, and fluxes of water and nutrients across Earth's surface. To date …

The topographic growth of a mountain belt is commonly attributed to isostatic balance in
response to crustal and lithospheric thickening. However, deeper mantle processes may …

The landscapes on Earth are shaped by the interaction of tectonics and erosion processes
and thus is a recorder for past tectonic and climatic histories. A recently proposed …

We explore the structural and geomorphological evidence for recent tectonic activity in the
Serranía de San Lucas (San Lucas Range, SLR), the northern segment of the Central …

Beryllium isotopes measured in detrital river sediment are often used to estimate rates of
landscape change at a basin scale, but results from different beryllium isotope systems have …

Drainage rearrangements and consequently divide migration are important processes in the
dynamic evolution of landscapes. Two approaches have been used to identify, analyze, and …

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 …