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sediment from rivers
beaches, sand dunes, spits and bars here
lowland
deposition and transport occur here
short fetch
less powerful waves
sheltered
sediment from offshore currents
stormy conditions
erosion and transport occur here
destructive waves
long fetch= stronger wind
sediments from mass movement
cliffs, wave cut platforms and stacks here
hard/igneous rock
coasts are exposed
Energy inputs e.g waves, tides, currents to classify coasts as high or low energy coasts.
Sediment inputs help to classify as an eroding coastline or outbuilding coastline.
Geology e.g lithology, or arrangements so coastlines can be classified as rocky, sandy, estuarine, concordant and discordant.
Sea level changes can classify coasts as submergent or emergent.