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Flamborough Head
North of Holderness Coast
Chalk headlands and cliffs
Highly permeable
Hydraulic action
Hydraulic action, weathering and mass movement combined can form wave cut platforms
Wave refraction causes notches, arches, caves, stacks and stumps
Holderness Cliffs
Middle of Holderness Coast
Retreating clay cliffs of the Holderness Bay
Made from easily eroded boulder clay
Retreating by 1.8m/y
Rain causes land slides
Fine clay removed by longshore drift (carries half a million tones of sediment - suspension - per year)
Winter storms threatening
Spurn Head
South of Holderness Coast
6km spit at Spurn Point
Longshore drift
6km long
Growing 10cm/y
Winter storms threatening
Home to sand dunes and salt marshes
Differential Erosion
Different types of rocks erode at different speeds