29. Bank erosion: Bank erosion is a function of factors
such as riparian vegetation, permeability of the substrate, and tensile
strength and cohesiveness of the soil. Consequently, bank erosion can
influence the structure of the stream channel (Leopold and Wolman, 1957).
The types of bank material movement, if present, are noted. These types
include mass wasting (debris avalanche, rotational failure, and slab
failure), and cut-bank scalloping (fig. 9). Indicate the presence of bank
erosion for the left and right banks using the following code:
Debris avalanche DA
Rotational failure RF
Slab failure SL
Cut-bank scalloping CB
None NO