Strath terraces, an important tool in tectonic geomorphology, have been attributed to
climatic, tectonic, volcanic, and human activity, yet the pathways connecting external …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

Valley width and the degree of bedrock river terrace development vary with lithology in the
Willapa and Nehalem river basins, Pacific Northwest, USA. Here, we present field-based …

Understanding how a bedrock river erodes its banks laterally is a frontier in geomorphology.
Theories for the vertical incision of bedrock channels are widely implemented in the current …

Wide bedrock valleys and their genetic descendants, strath terraces, can serve as
morphological records of past climate that reflect river discharge and sediment load during …

Erosion processes in bedrock‐floored rivers shape channel cross‐sectional geometry and
the broader landscape. However, the influence of weathering on channel slope and …

In this study, we conducted multiple physical experiments to estimate the efficacy and spatial
pattern of erosion by abrading sediment moving through a simple U‐shaped channel bend …

Fluvial planation surfaces, such as straths, commonly serve as recorders of climatic and
tectonic changes and are formed by the lateral erosion of rivers, a process that remains …

In this study, we present direct field measurements of modern lateral and vertical bedrock
erosion during a 2‐year study period, and optically stimulated luminescence (OSL) ages of …

Radiocarbon dates on charred plant remains are often used to define the chronology of
archives such as lake cores and fluvial sequences. However, charcoal is often older than its …