Glaciers and ice sheets erode mountains and produce vast quantities of sediments that are
delivered to rivers and oceans, impacting global sediment and biogeochemical balances …

Late Cenozoic convergence between the Australian and Pacific Plates has led to extensive
crustal deformation and exhumation in New Zealand. Over the past five decades, the …

Humans are primary agents of geomorphic change, and rates of anthropogenic landscape
change likely far exceed the pace of change expected from natural geologic processes …

In many gravel-bedded rivers, floods that fill the channel banks create just enough shear
stress to move the median-sized gravel particles on the bed surface (D 50). Because this …

The potential link between erosion rates at the Earth's surface and changes in global climate
has intrigued geoscientists for decades, because such a coupling has implications for the …

We evaluate changes to subglacial sediment discharge during glacier retreat by considering
ice dynamics, bedrock erosion, and sediment transport processes. Coupling these …

The temporal variability in sediment export yield from glaciers over a timescale of multiple
glacial cycles (eg 1× 102− 1× 106 years) is of interest for a wide range of applications in …

Airborne LiDAR data collected in 1998 and 2009–2010 were used to measure coastal cliff
erosion and retreat between the Mexico/California border and Bodega Head, California. Cliff …

Mountainous topography reflects an interplay between tectonic uplift, crustal strength, and
climate-conditioned erosion cycles. During glaciations, glacial erosion increases bedrock …

Sea cliff retreat rates are expected to accelerate with rising sea levels during the 21st
century. Here we develop an approach for a multimodel ensemble that efficiently projects …