Bank erosion is the wearing away of the banks of a stream or river. This is distinguished from erosion of the bed of the watercourse, which is referred to as scour.
The roots of trees growing by a stream are undercut by such erosion. As the roots bind the soil tightly, they form abutments which jut out over the water. These have a significant effect upon the rate and progress of the erosion.[1]
- ^ Ian Rutherford, James Grove (2004), "The Influence of Trees on Stream Bank Erosion", Riparian vegetation and fluvial geomorphology, American Geophysical Union, ISBN 978-0-87590-357-6