Run 5, with higher surface runoff than uplift rate (r/u = 6.0)

This is the fifth experimental run in this rainfall-runoff-uplift-erosion apparatus, constructed to test stream network stability over long periods of erosion. Surface runoff was the dominant erosion mechanism. This run was conducted in 2000 by Les Hasbargen for his PhD thesis at St. Anthony Falls Laboratory at University of Minnesota.

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