Rates of Erosion Determined From 10Be Analysis of Alluvial Sediments, Great Smoky Mountains, Tennessee and North Carolina (original) (raw)

Agu Fall Meeting Abstracts, 2001

Abstract

We measured 10Be in quartz extracted from sediment samples (n=22) collected from a network of 22 rivers and streams draining the Great Smoky Mountains and calculated model erosion rates that average 31+/-5 m My-1. Network analysis and mass balance calculations verify two main assumptions on which model erosion rate calculations depend: no significant storage within the sampled basin (also indicated

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