Large earthquakes initiate chains of surface processes that last much longer than the brief
moments of strong shaking. Most moderate‐and large‐magnitude earthquakes trigger …

Mountain building results in high erosion rates and the interaction of rocks with the
atmosphere, water and life. Carbon transfers that result from increased erosion could control …

Terrestrial carbon export via inland aquatic systems is a key process in the global carbon
cycle. It includes loss of carbon to the atmosphere via outgassing from rivers, lakes, or …

Rapid permafrost thaw in the high-latitude and high-elevation areas increases hillslope
susceptibility to landsliding by altering geotechnical properties of hillslope materials …

The deposition and long-term burial of organic carbon in marine sediments has played a key
role in controlling atmospheric O2 and CO2 concentrations over the past 500 million years …

Rivers are dynamic components of the terrestrial carbon cycle and provide important
functions in ecosystem processes. Although rivers act as conveyers of carbon to the oceans …

Steep hillslopes in mountain belts are eroded by landslides, and landsliding is ultimately
driven by the topographic relief produced by fluvial and glacial erosion,,,,. Landslide erosion …

Residual solid products of erosion display a wide range of size, density, shape, mineralogy,
and chemical composition and are hydrodynamically sorted in large river channels during …

The role played by river networks in regional and global carbon (C) budgets is receiving
increasing attention. Despite the potential of radiocarbon measurements (Δ14C) to elucidate …

Assessing the impact of glaciation on Earth's surface requires understanding glacial erosion
processes. Develo** erosion theories is challenging because of the complex nature of the …