Hydroclimatic changes associated with global warming over the past 50 years have been
documented widely, but physical landscape responses are poorly understood thus far …

Cosmogenic nuclide techniques have advanced the geosciences by providing tools for
exposure age dating, burial dating, quantification of denudation rates and more. Advances …

Landslide initiation and dynamics are approached with different methods according to the
scale of investigation. Individual landslides are typically described mechanistically, relying …

Oxidative weathering of sulfide minerals in sedimentary rocks releases carbon dioxide
(CO2) into the atmosphere. In permafrost zones, this could be a positive feedback on climate …

Weathering processes prepare and trigger rockfall, which is a key agent of alpine landscape
evolution and a hazardous process. The relative importance of different weathering …

Just as glaciers worldwide left a record of past advances and retreats that shifted latitudinally
in response to oscillating Quaternary climate changes, so too have cold-climate conditions …

Denudation is one of the main processes that shapes landscapes. Because temperature,
precipitation and glacial extents are key factors involved in denudation, climatic fluctuations …

In unglaciated terrain, the imprint of past glacial periods is difficult to discern. The
topographic signature of periglacial processes, such as solifluction lobes, may be erased or …

Weathering is a foundational process in most Earth systems, but there has been a lack of
data directly quantifying what influences mechanical weathering. Here we use multiple …

Characterizing the distribution and dynamics of organic carbon in soil is critical for
quantifying changes in the global carbon cycle. In particular, weathering controls on near …