Understanding Earth’s eroding surface with 10Be

For more than a century, geologists have sought to measure the distribution of erosion rates on Earth's dynamic surface. Since the mid-1980s, measurements of in situ 10Be, a cosmogenic radionuclide, have been used to estimate outcrop and basin-scale erosion rates at 87 sites around the world. Here, we compile, normalize, and compare published 10Be erosion rate data (n = 1599) in order to understand how, on a globalscale, geologic erosion rates integrated over 103 to 106 years varybetween climate zones, tectonic settings, and different rock types. Drainage basins erodemore quickly (mean = 218 m Myr-1; median = 54 m Myr-1) than outcrops (mean = 12 m Myr-1; median = 5.4 m Myr-1), likely reflecting the…