Spurn Point provides evidence of longshore drift on the Holderness Coast. It is an excellent example of a spit. Around 3% of the material eroded from the Holderness Coast is deposited here each year.
Boulder clay cliffs near Mappleton – what’s happening? Would you choose to defend this stretch of coast?
Landslips: also known as rotational slumps, are occasional rapid movements of a mass of earth or rock dropping down along a concave plane. Water percolating through sandstone gets into the clay beneath, saturating it. With the weight of the rock above forcing down on it the clay moves seawards as a mud flow. With the clay moving sideways the sandstone above slumps down. Undercutting of a steep slope by the sea weakens the rock above, making a slump more likely.
Rockfall: rapid, free-fall of rock from a steep cliff face due to gravity. This is made worse by freeze-thaw action loosening the rock - water enters the joint (vertical crack), freezes and expands, breaking up the rock. A scree slope of fallen rock is formed at the bottom of the cliff. It is also possible for free falls to occur in very dry conditions – for example clay cracks as it dries out and then crumbles easily
Mudflow: occurs on steep slopes over 10°. It's a rapid sudden movement which occurs after periods of heavy rain. When there is not enough vegetation to hold it in place, saturated clay flows out of the cliff face, almost like a river of mud.
Annotate the photograph showing features of erosion