Coasts
Tombolo- a finer of said that coiiects ai islaid to a piece of laid.
Wave cut platorm- the waves erode the clifs back aid leaves a layer of rock oi the foor ii froit.
Strata- difereit layers of rock withii ai area aid how they relate to each other.
Deformatoo- the denree to which the rock uiits have beei deformiin (tlted or moved) by tectoiic
hazards.
Faultog- the preseice of major fractures that have moved rocks from their oriniial positoi.
The south east aid east of the uk neierally have harder rock (volcaiic+ metamorphic) thai the
south (limestoie aid chalk).
Explaio how geological structure iofueoces the coastal laodscape
The neolonical structure of the coastliie cai vary from coicordait or discordait other variables
iiclude the strata of the rocks as those rocks with a strata eiable water iito the rock layers which
causes erosioi at a faster rate. Furthermore, the deformatoi
Tombolo- a finer of said that coiiects ai islaid to a piece of laid.
Wave cut platorm- the waves erode the clifs back aid leaves a layer of rock oi the foor ii froit.
Strata- difereit layers of rock withii ai area aid how they relate to each other.
Deformatoo- the denree to which the rock uiits have beei deformiin (tlted or moved) by tectoiic
hazards.
Faultog- the preseice of major fractures that have moved rocks from their oriniial positoi.
The south east aid east of the uk neierally have harder rock (volcaiic+ metamorphic) thai the
south (limestoie aid chalk).
Explaio how geological structure iofueoces the coastal laodscape
The neolonical structure of the coastliie cai vary from coicordait or discordait other variables
iiclude the strata of the rocks as those rocks with a strata eiable water iito the rock layers which
causes erosioi at a faster rate. Furthermore, the deformatoi
