coastal erosion
Permanent loss of land along the shoreline
natural causes
Changes in wave climate
Height
Angle of approach
Frequency of high magnitude waves
Reduction in the amount of sediment delivered to the coast from reef
Rising sea levels
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coastal erosion
Permanent loss of land along the shoreline
natural causes
Changes in wave climate
Height
Angle of approach
Frequency of high magnitude waves
Reduction in the amount of sediment delivered to the coast from reef
Rising sea levels
human induced
Sand extraction from the beaches - reduces sand volume of the coast
Coral mining
Insertion of structures that locally alter wave processes - change sediment transport patterns
Seawalls
Removal of mangroves
contirbuting factors
Coastal development
Loss of dune protection
Disruption to the sand cycle
Climate change
Storms and rise in sea levels
Removal of dune vegetation - stability lost
shaping coastlines
wind erode headlands
Controls plants that grow on them
Strong wind = smaller plants
Waves wash against coastline
eroding cliffs
Moving rocks and sand along the coast
Larger river systems deposit mud and silt where they meet the ocean
weathering
Re-shaping process where rock of the foreshore is disintegrated and decomposed by the water
physical weathering
Abrasive action of sand particles in the moving sea and wave actions
Waves compress into the crevices of rocks and forces them apart
chemical weathering
Water dissolves minerals out of the rock
Removal of debris
Breaks rock -> sand
rocky coasts
Continually wash against the coastline eroding the cliff base
Forms sheer cliffs
Then forms notches in the headland
Material above the notch eventually collapses
Wind and wave action creates caves, arches, and stacks
caves
Softer rocks are eroded faster than surrounding rocks
arch
Prolonged wave action may turn waves into an arch
stack
Top of arch breaks of to form a stack
blowhole
In a cave a joint of weakness may go further up a cliff to form blowhole
attrition
Materials carried by the waves bump into each other
Smoothed and broken down into smaller particles
hydraulic action
Force of water against the coast
Waves enter cracks (faults) in the coastline and compress the air within the crack
Wave hits
Air in crack expands quickly
Minor explosion
Process repeated continuously
corrosion
Chemical action of sea water
Acids in salt water slowly dissolve rocks
limestone and chalk particularly prone to this process
abrasion/corrasion
Coast is worn down by material carried by the waves
Waves throw particles against the rock
Sometimes at high velocity