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A platform for research: civil engineering, architecture and urbanism
Free degradation of London Clay cliffs
Morphological evidence concerning degradation of London Clay cliffs following cessation of erosion at foot is drawn from sites in Essex and Kent; stages of free degradation on coastal cliffs are traced until angle of ultimate stability against landsliding is reached; this angle is shown to be closely anticipated, at early stage of degradation process, in average inclination of accumulation zone which develops at slope foot; landslides on more mature, inland slopes are generally of different type, probably because these slopes are commonly mantled by solidification deposits.
Free degradation of London Clay cliffs
Morphological evidence concerning degradation of London Clay cliffs following cessation of erosion at foot is drawn from sites in Essex and Kent; stages of free degradation on coastal cliffs are traced until angle of ultimate stability against landsliding is reached; this angle is shown to be closely anticipated, at early stage of degradation process, in average inclination of accumulation zone which develops at slope foot; landslides on more mature, inland slopes are generally of different type, probably because these slopes are commonly mantled by solidification deposits.
Free degradation of London Clay cliffs
Geotechnical Conference -- Shear Strength Properties Natural Soils Rocks -- Proc
Hutchinson, J.N. (author)
Proceedings of Geotechnical Conference -- Shear Strength Properties of Natural Soils and Rocks ; 1967 ; Norway , Oslo
1967
6 pages
Conference paper
English
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The free degradation of London Clay cliffs
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