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

Terrestrial cosmogenic nuclides, produced by secondary cosmic-ray interactions in the
atmosphere and in situ within minerals in the shallow lithosphere, are widely used to date …

The tectonic and climatic boundary conditions of the broken foreland and the orogen interior
of the southern Central Andes of northwestern Argentina cause strong contrasts in elevation …

Recent elevation reconstructions of the Andean Plateau suggest a rapid 2.5±1.0 km rise of
the central Andes between~ 10 and 6 Ma. This rapid rise has been attributed to a …

Rock uplift rates can be difficult to measure over 103–105 yr time scales. If, however, a
landscape approaches steady state, where hillslope erosion and rock uplift rates are steady …

Understanding climatic influences on the rates and mechanisms of landscape erosion is an
unresolved problem in Earth science that is important for quantifying soil formation rates …

Erosional exhumation and topography in mountain belts are temporally and spatially
variable over million year timescales because of changes in both the location of deformation …

Past variations in climate and tectonics have led to spatially and temporally varying erosion
rates across many landscapes. In this contribution I examine methods for detecting and …

The response of surface processes to climatic forcing is fundamental for understanding the
impacts of climate change on landscape evolution. In the Himalaya, most large rivers feature …

This paper reviews the traditional approach to sediment budget studies in geomorphology,
new approaches and more specifically the potential impact of new methodological …