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

Climate controls erosion and weathering on soil-mantled landscapes through diverse
processes that have remained difficult to disentangle due to their complex interactions. We …

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 …

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 weathering and erosion processes that produce and destroy regolith are widely
recognized to be positively correlated across diverse landscapes. However, conceptual and …

Chemical weathering rates for landscapes are difficult to quantify because the timescales
over which weathering occurs are often unknown. In this study, we use timescales defined …

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 …

Understanding the controls on chemical weathering, especially of silicate minerals, remains
a major challenge, despite its importance in controlling the evolution of the Earth's surface …

The spacing of hills and valleys reflects the competition between disturbance-driven (or
diffusive) transport on hillslopes and concentrative (or advective) transport in valleys …

We used cosmogenic nuclide and geochemical mass balance methods to measure long-
term rates of chemical weathering and total denudation in granitic landscapes in diverse …