Physical landscapes - coasts Flashcards
(64 cards)
how are waves formed
wind blows over the sea and friction with water surface causes ripples to form
these develop into waves
shallowing water and rising sea floor affects the wave’s orbital movement, becomes more elliptical
wave crest rises up and eventually breaks
constructive waves
low vs length
strong swash and weak backwash
less frequent 6-8per min
produce wide, sandy beaches with a gradual beach angled
destructive waves
tall vs length
weak swash and strong backwash
10-14 per min
break downward with great force, eroding the beach to make a steeper angle
pebble beaches often produced
mechanical weathering
is the disintegration of rocks
piles of fragments are found at the cliff foot
eg salt weathering
type of mechanical
water evaporates, leaves salt crystals which grow and expand, causing pressure on the rock
chemical weathering
caused by chemical changes
rainwater slowly dissolves rocks
eg carbonation
rainwater absorbs co2 and becomes acidic, when it comes into contact with alkaline rocks such as chalk/limestone a chemical reaction is produced
rocks slowly dissolve
mass movement
downward movement of material under the influence of gravity
sliding
large blocks of rock slide down a cliff face as a landslide, often triggered by heavy rainfall or earthquakes
slumping
involves the collapse of saturated or weak rocks e.g sand or clay, often along a curved surface
rock falls
fragments of rock break away from the cliff face to form scree
erosion
the wearing away of earth’s surface by the action of wind or water
hydraulic action
destructive waves hit the base of cliffs
water enters cracks, joints and faults at high speeds
air in these cracks is compressed with explosive force
this, repeated, causes cracks to widen and the cliff to weaken and material breaks off
abrasion
waves have the energy to carry material and at times large rocks
this material is thrown at the cliff face, scratching and scraping the surface
attrition
rock fragments carried by the sea collide and become smaller over time
jagged edges are worn away to produce small pebbles
traction
largest pieces of material are rolled along the seabed by the force of water
good when there is lots of power in the water
saltation
load is bounced along the sea bed e.g shingle
currents cannot keep heavier sediment afloat for longer periods
suspension
small particles are carried in the water
solution
materials often derived from limestone or chalk are dissolved and carried
longshore drift
process by which waves move material along the coast
waves approach the coast at an angle due to the prevailing wind direction
swash carries material toward the beach at an angle
backwash flows back to the sea down the beaches slope at 90 degrees due to gravity
process repeats itself along the coast in a zigzag movement
deposition
waves drop and leave behind the load they were carrying
takes place in areas where the flow of water slows down (low sheltered bays)
here the waves lose energy and sediment can no longer be carried
also occurs when water is trapped by landforms such as spits or engineered structures
headland
a cliff that juts out into the sea, comprised of hard rock
bay
crescent shaped indentation in the coastline, found between headlands
bays and headlands formation
form along discordant coastlines where hard and soft rocks alternate along the coast
these erode at different rates and less resistant rock such as clay is worn away
bays are sheltered by headlands and become low energy environments where deposition occurs