CL - coastal landforms p18 - Flashcards
4 processes of wave erosion
hydraulic action
abrasion
attrition
solution
hydraulic action
the force exerted onto rocks from pounding waves
abrasion
sand/shingle/boulders picked up by the sea and hurled against the cliff
attrition
the wearing down of rocks and pebbles as they rub against each other - making them smaller and rounder
solution
when fresh water mixes with salt water - carbon-based rocks are broken down
4 processes of wave transporation
traction
saltation
suspension
soltuion
traction
LARGE boulders ROLLED along the seabed
saltation
SMALL stones BOUNCED along the seabed
suspension
SMALL particles carried in moving water
solution
dissolved material
fluvial and aeolian processes
fluvial - water
aeolian - air
hows headlands and bays formed
- when there are different bands of different rock with different resistances to erosion
- weaker rock erodes faster - bay
- harder rock is left - headland
how are shore platforms (wave cut platforms and notch) formed
- high energy waves concentrate erosion at the base of cliff
- cliff is undercut forming a wave-cut notch
- overtime the undercut collapses and the cliff face retreats
- this leaves a wave cut platform
what are geos
narrow, steep-sided inlets on the coastline formed where there is weakness (joint or fault) in the rock which is exposed by erosion processes such as hydraulic action
whats a tombolo and how is it formed
- is a bar or beach that connects the mainland to an offshore island
- is formed due to wave refraction off the coastal island reducing wave velocity, leading to deposition of sediments. They may be covered at high tide if they are low lying.
whats a blow hole and how is it formed
- a pot hole on top of a cliff, created by chemical weathering, and a cave, formed by marine erosion.
- As the cave erodes deeper into the cliff face and the pothole deepens,
- a channel is created for incoming waves to travel into and up the cliff face (occasionally water splashes out of the top of the blowhole when energetic waves hit the cliff face).
the process of how caves, arches, stacks and stumps are formed
- joints and faults in resistant rock are attacked by waves
- hydraulic action and abrasion wide the weaknesses and undercuts the base of cliff - CAVE
- more erosion on the headland and hole is opened - ARCH
- cliff face recedes and forms a wave cut platform. the arch collapses and creates a STACK
- sea attacks base of stack and eventually wave cut notch undercut the stack and the STRUMP is left
how are salt marshes formed
- Behind spits and barrier beaches the area is very sheltered, tidal currents and river currents meet leading to lots of deposition
- This can lead to the formation of salt marshes
- Salt-tolerant species colonise these sheltered, flat muddy areas
- They are covered at high tide and exposed at low tide
list of physical factors that affect the coastline
wind
wave
current
tidal
lithology
structure