Coastal Landforms Flashcards
Properties of constructive waves
- strong swash
- weak backwash
- builds up a gently sloping beach
- wave crests far apart
- gently sloping wave front
Properties of destructive waves
- weak swash
- strong backwash
- destroy beach creating a steep slope
- waves close together
- steep wave fronts
describe freeze-thaw
- water collects in cracks or holes in rock
- at night, water freezes and expand, making cracks bigger
- when temperature rises, ice thaws (melts), it seeps deeper into rock
- repetition causes fragments of rock to break off and fall to foot of the cliff
what is scree
fragments of rock that have fallen and collected at the foot of the cliff
describe salt weathering
- seawater contains salt, when water evaporates, it leaves behind salt crystals
- in cracks, these salt crystals grow and expand
- this puts pressure on the rocks and flakes may eventually break off
describe carbonation
- rainwater absorbs CO2 from air and becomes slightly acidic
- contact with alkaline rocks (e.g. chalk, limestone) produces a chemical reaction causing rocks to slowly dissolve
coastal erosion - solution
dissolving of soluble chemicals in rocks
coastal erosion - corrasion
fragments of rock are picked up and hurled by the sea at a cliff.
act like tools scraping to erode the rock
coastal erosion - hydraulic action
- power of the wave as they smash onto a cliff
- trapped air is forced into cracks in rock, causing the rock to break
coastal erosion - attrition
rock fragments carried by the sea knock against one another, causing them to become smaller and more rounded
coastal erosion - abrasion
‘sandpapering’ effect of pebbles grinding over a rocky platform causing it to become smooth
describe long-shore drift
when wave approach the coast at an angle, the sediment will be moved along the beach in a zig zag pattern
where does coastal deposition take place
where the flow of water slows down
waves lose energy in sheltered bays and where water is protected by spits/bars
here sediment can no longer be carried of mvoed and is therefore deposited
discordant and concordant coastlines
discordant - bands of soft and hard rock are alternating perpendicular to the coastline, meaning headlands and bays are formed
concordant - bands of soft and hard rock are aligned parallel to coastline
how are cliffs and wave-cut platforms formed
- when waves break against a cliff, erosion close to the high tide line will wear away the cliff to form a wave cut notch
- over time, notch will get deeper, undercutting the cliff
- eventually overlying cliff can no longer support its own weight and it collapses
- this repeats causing the cliff to retreat
- in its place will be a gently sloping platform called a wave-cut platform
- smooth due to the process of abrasion