Experience in monitoring channel deformations on rivers with broad flood plains (as exemplified by the Kerzhenets river)

Presented are the results of a five-year (2001-2005) monitoring of deformations of the Kerzhenets river channel in its lower part. The concave-bank caving observations were made for three free bights compose d of sand and loamy sand: the steep segmental, segmental developed and segmental gently sloping blights.