▪ Abstract Bedrock rivers set much of the relief structure of active orogens and dictate rates
and patterns of denudation. Quantitative understanding of the role of climate-driven …

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 …

Bedrock river profiles are often interpreted with the aid of slope–area analysis, but noisy
topographic data make such interpretations challenging. We present an alternative …

The stream power incision model (SPIM) is a cornerstone of quantitative geomorphology. It
states that river incision rate is the product of drainage area and channel slope raised to the …

Abrasion by bed load is a ubiquitous and sometimes dominant erosional mechanism for
fluvial incision into bedrock. Here we develop a model for bedrock abrasion by saltating bed …

Recent theoretical models suggest that topographic characteristics of bedrock channels are
products of interactions among tectonics, substrate resistance, and the climatically …

Erosion by bedrock river channels is commonly modeled with the stream power equation.
We present a two‐part approach to solving this nonlinear equation analytically and explore …

Research in landscape evolution over millions to tens of millions of years slowed
considerably in the mid‐20th century, when Davisian and other approaches to …

Knickpoint behaviour is a key to understanding both the landscape responses to a base‐
level fall and the corresponding sediment fluxes from rejuvenated catchments, and must be …

We utilize topographic analysis of channel profiles combined with field measurements of
erosion rates to explore the distribution of channel incision in the Anyemaqen Shan, a broad …