Quantifying spatial variations in weathering across hillslopes is crucial to understanding hydrological, ecological, and geomorphological processes in...

Quantifying the controls of soil production rates is essential for understanding hillslope evolution and morphology in soil-mantled landscapes. Previo...

The subsurface critical zone is fundamentally challenging to study, it resides hidden just beneath Earths surface. Our current understanding of the sc...

Active faults significantly influence landscape morphology by tectonic and erosional processes. These faults drive surface movementsuplift, subsidence...

The lithospheric stress field induces topography, faulting, and non-brittle deformation. At long wavelengths, these stress fields arise both from vari...

In northern California, the complex geometry of the San Andreas Fault system, and how it steps and propagates across the Earths surface, is revealed i...

Quantifying the controls of soil production rates is essential for understanding hillslope evolution and morphology in soil-mantled landscapes. Previo...

We used seismic refraction surveys and observations from four deep boreholes to quantify the relative importance of the ambient stress field and litho...