Geomorphology is currently in a period of resurgence as we seek to explain the diversity,
origins and dynamics of terrain on the Earth and other planets in an era of increased …

Currently, the use of numerical models for reproducing the evolution of river systems and
landscapes is part of the day-by-day research activities of fluvial engineers and …

Tectonic displacements consist of vertical uplift or subsidence, and horizontal advection. We
consider the effects of tectonic advection on mountain range topography, surface drainage …

In fold‐and‐thrust belts and accretionary prisms, fault bends induce folding in the hanging
wall that can alter the long‐term loading rate on the megathrust and profoundly influence …

Landscape evolution is a product of the forces that drive geomorphic processes (eg,
tectonics and climate) and the resistance to those processes. The underlying lithology and …

Here we examine the landscape of New Zealand's Marlborough Fault System (MFS), where
the Australian and Pacific plates obliquely collide, in order to study landscape evolution and …

Contrasts in bedrock erodibility have been shown to drive landscape transience, but it is
unclear whether horizontal tectonic displacements would enhance such effects …

Strike‐slip faults have long been known for characteristic near‐fault landforms such as offset
rivers and strike‐parallel valleys. In this study, we use a landscape evolution model to …

Abstract The Mountain Front Flexure is a major structure of the Zagros orogenic system, and
is underlain by the deeply rooted and seismically active Mountain Front Fault system. These …

Sediment flux is known to influence bedrock incision rates in mountain rivers. Although the
widely used stream power incision model lacks any explicit representation of sediment flux …