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 …

Determining how and why eruptive outputs are modulated by the loading and unloading of
ice is key to understanding whether ongoing and accelerating deglaciation across mid-to …

We present new geochronological data derived from hillslope boulder armor in the Flint Hills
in northeastern KS, United States, that provides insights into the rates and timing of lateral …

Large-magnitude earthquakes and hydrologic events in mountainous settings commonly
trigger thousands of landslides, and slope failures typically constitute a significant proportion …

Abstract Knowledge of erosion rates through time is of great importance to understand the
effects of tectonics and climate on the topographic evolution of mountain belts. In this study …

Silicate weathering via CO 2 consumption is considered to regulate the long-term climate
change. Discriminating silicate versus carbonate weathering from sedimentary records is …

A feedback between Earth surface weathering and climate is thought to be fundamental in
maintaining Earth's habitability over long times-cales, but investigating this control in the …

Evolution of weathering profiles (WP) is critical for landscape evolution, soil formation,
biogeochemical cycles, and critical zone hydrology and ecology. Weathering profiles often …

We investigate if the commonly neglected riverine detrital carbonate fluxes might
reconciliate several chemical mass balances of the global ocean. Particulate inorganic …

High As groundwater has been reported in aquifers comprising Late Pleistocene and
Holocene sediments worldwide, and could be due to the depositional environment and …