What controls the chemical weathering of soils in tectonically active landscapes? Recent
field and modeling studies suggest that tectonic forcing and associated increases in erosion …

Landscapes evolve in response to external forces, such as tectonics and climate, that
influence surface processes of erosion and weathering. Internal feedbacks between erosion …

Soil‐covered upland landscapes constitute a critical part of the habitable world. Our
understanding of how they evolve as a function of different climatic, tectonic and geological …

The relationships among climate, physical erosion, and chemical weathering have remained
uncertain, because long-term chemical weathering rates have been difficult to measure …

Biogeochemical cycling within the Critical Zone depends on the interactions between
minerals and fluids controlling chemical weathering and physical erosion rates. In this study …

In a headwater catchment in the Oregon Coast Range, we find that solid-phase mass losses
due to chemical weathering are equivalent in the bedrock and the soil. However, the long …

Quantitative understanding of variability in weathering fluxes on the modern Earth is limited
because little is known about where the most important weathering reactions take place …

We used cosmogenic nuclide and geochemical mass balance methods to measure long-
term rates of chemical weathering and physical erosion across a steep climatic gradient in …

Tectonic uplift is one of the key factors controlling the supply of material to weathering
environments. At present however, there is debate about whether tectonics or climate plays …

Quantifying long-term rates of chemical weathering and physical erosion is important for
understanding the long-term evolution of soils, landscapes, and Earth's climate. Here we …