The hypsometric curve of the study basin and two predicted Ne-21 distributions obtained using different ranges of bedrock erosion rates that vary linearly with slope. Note how the two Ne-21 distributions are markedly different from the hypsometric curve (and also different from each other), illustrating the sensitivity of the cosmogenic nuclide concentration distribution to the spatial distribution and range of erosion rates in the drainage basin.
Image 15546 is a 849 by 1146 pixel WebP
Uploaded:
Jun6 09
