Coasts knowladge Flashcards
How many sediment cells are in the UK?
11
Concordant coasts
occurs where the bands of differing rock types run parallel to the coast.
Discordant coasts
occurs where bands of differing rock type run perpendicular to the coast.
Geological structure
Folds, faults, joints and bedding planes.
Abrasion
Abrasion (also known as Corrasion) is where rocks and other materials carried by the sea are picked up by strong waves and thrown against the coastline
Solution
Carbonic acid within the seawater helps to dissolve rock at the coastline and break it down. This is particularly effective on rocks which have calcium carbonate within them such as limestone and chalk.
Attrition
Rocks and boulders are ground over each other in the water and overtime become smoothed.
First step of the formation in a wave cut notch
Wave cut platforms are usually a result
of both coastal erosion and weathering
acting on a cliff face.
Second step of formation of a wave cut notch
Over time, a wave cut notch in a cliff face will be created, within the wave attack zone, which will
undercut the unsupported cliff above
3rd step of formation of a wave cut notch
This cliff face will collapse
onto the seabed below and slowly
retreat, leading to a build-up of sediment
along the base – a wave cut platform
chemical weathering
describes the process of chemicals in rainwater making changes to the minerals in a rock.
biological weathering
plant roots splitting rocks or causing joints or cracks, as well as bacteria like algae producing chemicals which break down the rock on which they live for nutrients.
eustatic change
global sea level change
isostatic
local variation of land height overtime
How was isostatic change caused during the ice age?
During an ice age, isostatic change is caused by the build-up of ice on the land. As water is stored on the land in glaciers, the weight of the land increases and the land sinks slightly, causing the sea level to rise
slightly.