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
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

BRK24B59_339

Model release

NA

Property release

NA

License type

Rights managed

Available size

33,6Mb (1,4Mb) / 14,6in x 9,0in / 4368 x 2688 (300dpi)

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