Temporal variations in coarse river deposits are often attributed to climate change. Cosmogenic nuclide concentrations of river cobbles suggest that climate plays a subordinate role to earthquake-induced landslides in producing coarse sediments in arid Peru.
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Niemi, N. Quake, rubble and roll. Nature Geosci 7, 859–860 (2014). https://doi.org/10.1038/ngeo2297
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DOI: https://doi.org/10.1038/ngeo2297