
Caption
Rapid coastal erosion of soft cliffs between Benacre and Kessingland on the Suffolk coast England. The cliffs were formed by glacial outwash of sands and pebbles which overly older clay strata. This structure of permeable rock over impermeable clay makes the cliff especially prone to slumping and mass movement
Date
Nov 11, 2012
Credit line
Photo12/imageBROKER/Ian Murray
Reference
BRK24B57_353
Model release
NA
Property release
NA
License type
Rights managed
Available size
34,5Mb (1,6Mb) / 9,4in x 14,3in / 2805 x 4296 (300dpi)