DOI:
10.6073/pasta/9913b248c50c938d0777e4a3a0c2aced
Data set ID:
528
Muddy banks of marsh channels experience soil creep – a viscous-like slow deformation resulting in a net downslope transport. Here we present the first field evidence of soil creep in a mesotidal salt marsh using
high precision measurements of soil deformation taken with a vibrating-wire extensometer over two years.
Publication Date:
Friday, August 16, 2019
Date Range:
Sunday, June 26, 2016 to Tuesday, March 6, 2018