a concordant coastline have alternating bands of hard and soft rock parallel to the coast
discordant coastlines have alternating bands of hard and soft rock at 90 degrees to the coast
erosional landforms are more common on discordant coastlines
in Dorset, the coastline consists of Portland limestone making headlands and bays
rocks with joints and faults are more susceptible to the processes of erosion and weathering
bedding planes that dip towards the sea create a gentler cliff profile than those that dip away from the sea
bedding planes that dip towards land tend to create a steeper cliff profile
these cliffs are more vulnerable to erosional processes
the angle that the rock layer forms with the horizontal bedding plane is referred to as the dip
igneous rocks, such as granite, form from the crystallisation of magma
they are more resistant to erosion and weathering
sedimentary rocks, such as limestone, forms from the build up of sediments compacting together
more susceptible to weathering
metamorphic rocks such as marble are formed from the change in the structure of sedimentary rocks and igneous rocks, caused by heat and pressure
resistant to erosion
the existence of sedimentary, igneous and metamorphic rocks affects the rate of recession along a coastline
vegetation is important in supporting the development of sandy coastlines
sand dunes need a continuous supply of sand, wind and obstacles to trap sand, like plants
a typical sand dune transect goes from the mobile dune, nearest the sea (embryo, fore and yellow) to the fixed dunes nearest the back ( grey dunes and dune slack)
xerophytes can withstand periods of dry weather
halophytes can withstand high concentrations of salt water