Discordant coastline

Source: Wikipedia, the free encyclopedia.
Durlston Head (limestone) to Handfast Point (chalk), with Peveril Point (limestone) dividing Durlston Bay from Swanage Bay

A discordant coastline occurs where bands of different rock types run perpendicular to the coast.[1]

The differing resistance to erosion leads to the formation of headlands and bays. A hard rock type such as

Bagshot Beds
is easily eroded creating a bay.

Part of the

greensand. North of Swanage, the chalk outcrop creates the headland which includes Old Harry Rocks
.

The converse of a discordant coastline is a concordant coastline.

References

  1. ^ "Landform change – the Dorset coastline - Coastal landscapes – WJEC - GCSE Geography Revision - WJEC - BBC Bitesize". www.bbc.co.uk.

Examples

See also