Compaction - broken down sediment carried by rivers and deposited to create layers. As they build up the bottom layers are compacted
Heat and pressure - some rock pushed below earths surface, very hot and high pressure - causes rocks to form crystals
Concordant coastline - has same type of rock along its length
Discordant coastline - geology alternates between strata perpendicular to the coast of more resistant and less resistant rock
Structure of the coastline - a cold form in layers known as beds. These beds are subjected to tectonic forces that tilt and deform them so they dip at an angle
Horizontal bedding - profile is steep but softer rock has u see gone differential erosion producing several notches
Seaward dipping - loose material can slide down the bedding planes making the cliff unstable and dangerous
Landward dipping - these are relatively steep and stable compared to seaward dipping bed planes
Soft engineering - often less expensive, more long term sustainable- made from natural defences
Hard engineering - building of artificial structures to reduce or stop impact of coastal processes - man made defences
Sub-aerial weathering - collective term for weathering and mass movement processes
Spring tide - higher levels due to moon, sun and earth being aligned
Erosion -
abrasion
hydraulic action
solution
attrition
pounding
Weathering -
mass movement
freeze thaw
tree roots
thermal expansion
hydrolysis
solution
carbonation
Transportation -
suspension
solution
saltation
traction
Deltas - landform at mouth of river where the river meets with another water body but with a much lower velocity than itself
3 delta types -
arcuate - similarity to triangular appearance (Nile delta)
cuspate - toothlike appearance-more pointed (Ebro river, Spain)
birds foot - few widely spaced distributaries(Mississippi river)
Berms - smaller ridges that develop at position of mean high tide mark
Cusps - small circular depressions where waves have awash and backwash with similar strength
Nearshore/surface current - caused by wave action in and near the breaker zone
Offshore/deep currents - not well defined, starts from wither edge of the literal zone from breaking of the wave or outer edge of nearshore zone
Rip current - caused by either tidal motion or waves breaking at right angles to the shore
Deep ocean currents - driven by differences in the waters density which is controlled by temperature (thermo) and salinity (haline)- thermohaline circulation