Understanding the manner and degree to which topography in active mountain ranges
reflects deformation of the Earth's surface remains a first order goal of tectonic …

The study of drainage network response to uplift is important not only for understanding river
system dynamics and associated channel properties and fluvial landforms, but also for …

We present a statistical technique for analyzing longitudinal channel profiles. Our technique
is based on the integral approach to channel analysis: Drainage area is integrated over flow …

The Earth's topography is shaped by surface processes that operate on various scales. In
particular, river processes control landscape dynamics over large length scales, whereas …

One of the most conspicuous features of a mountain belt is the main drainage divide. Divide
location is influenced by a number of parameters, including tectonic uplift and horizontal …

We use a computer landform evolution model to show that Noachian‐Hesperian‐aged, late‐
stage valley network formation required numerous and repeated moderate flood events …

The transient response of bedrock rivers to a drop in base level can be used to discriminate
between competing fluvial erosion models. However, some recent studies of bedrock …

Abstract The Mountain Front Flexure marks a dominant topographic step in the frontal part of
the Zagros Fold–Thrust Belt. It is characterized by numerous active anticlines atop of a …

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

A natural experiment in landscape evolution is a case study of landform development in
which only one element varies significantly, and for which the driving forces, initial …