Drainage networks in continental rifts are generally reported as dynamic features that
produce transitions between endorheic and exorheic conditions. While this is of major …

The occurrence of endorheic basins on the Tibetan Plateau, both in its Pleistocene history
and (fewer in number) at the present day, has been attributed to the 'basin-and …

This paper explores an inverse approach to the problem of characterizing sediment
sources'(“source” samples) age distributions based on samples from a particular depocenter …

Syn‐rift deep‐water muds and mudstones preserve a relatively complete stratigraphic
record of tectonic and climatic events. This paper investigates mud‐dominated deposits and …

Erosion and sedimentation constantly rework topography created by tectonics but also
modulate stresses in the underlying crust by redistributing surficial loads. Decades of …

The top-down drainage basin integration and drainage network evolutionary processes of
lake overflow and aggradational spillover (or aggradational piracy), collectively referred to …

The generation and evolution of continental topography are fundamental geologic and
geomorphic concerns. In particular, the history of landscape development might contain …

Abstract The Salt River and Verde River watersheds provide downstream metropolitan
Phoenix, Arizona, USA with much of its water supply, and this paper explains how these …

Aim Current distributions of widespread North American (NA) species have been shaped by
Pleistocene glacial cycles, latitudinal temperature gradients, sharp longitudinal habitat …

Abstract The Colorado River in the southwestern US provides an excellent natural
laboratory for studying the origins of a continent-scale river system, because deposits that …