The topographic evolution of orogens is fundamentally dictated by rates and patterns of
bedrock-channel incision. Quantitative field assessments of process-based laws are needed …

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 …

Published by the American Geophysical Union as part of the Water Resources Monograph
Series, Volume 14. I wrote this book in response to a need expressed by one of my Ph. D …

The persistence of topography within ancient orogens remains one of the outstanding
questions in landscape evolution. In the eastern North American Appalachians, this question …

Variation in the erodibility of rock units has long been recognized as an important
determinant of landscape evolution but has been little studied in landscape evolution …

Published by the American Geophysical Union as part of the Water Resources Monograph
Series, Volume 19. What are the forms and processes characteristic of mountain rivers and …

The equilibrium form of the fluvial long profile has been used to elucidate a wide range of
aspects of landscape history including tectonic activity in tectonic collision zones, and in …

We have used early Miocene valley‐filling basalts to reconstruct fluvial long profiles in the
Upper Lachlan catchment, SE Australia, in order to use these as well‐constrained initial …

Bedrock strength is a key parameter that influences slope stability, landscape erosion, and
fluvial incision. Yet, it is often ignored or indirectly constrained in studies of landscape …

The reason for the survival of mountainous topography in ancient orogenic belts is a long‐
standing problem in geomorphology and geodynamics. We explore the geomorphologic …