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C. Glotzbach, P. van der Beek, J. Carcaillet and R. Delunel Deciphering the driving forces of erosion rates on millennial to million-year timescales in glacially impacted landscapes: An example from the Western Alps Journal of Geophysical Research: Earth Surface 118

Version of Record online: 16 AUG 2013 | DOI: 10.1002/jgrf.20107

Key Points

  • Glacially caused transient morphology and perturbation of erosion rates.
  • The perturbation is independent of Myr-scale erosion rates.
  • Glacial erosion acts irrespective of tectonic uplift, and regulates morphology.

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