HIGHLIGHTS
SUMMARY
The use of in situ 10 Be concentrations measured in river sediments to quantify catchment-wide denudation rates over centennial to millennial timescale is now well-established (e_g Brown et_al, 1995; Granger et_al, 1996; Bierman and Steig, 1996; Granger and Schaller, 2014). Over the Late Cenozoic to Quaternary, temperature fluctuations, increased precipitation and glaciations have participated in a worldwide increase in erosion rates(e_g Peizhen et_al, 2001; Herman et_al, 2013). In the European Alps, climate forcing has led to significant topographic modification through increased slope steepness and relief (e_g Valla et_al, 2011, 2021), which . . .
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