Coasts Flashcards
1
Q
Swash
A
The movement of a wave up a beach
2
Q
Backwash
A
The movement of a wave down a beach to the sea.
3
Q
Concordant coastline
A
-same type of rock all along the coastline
4
Q
Discordant coastline
A
-hard soft rock arranged in layers at 90 degree angles to the coast
5
Q
Fetch
A
-the distance the wave has travelled
6
Q
What is a spit?
A
-a ridge of sand connected to the coast at one end where the coast changes direction due to longshore drift
7
Q
What determines the size of a wave?
A
Fetch
Wind strength
Wind duration
8
Q
Destructive
A
- formed from strong winds
- waves have long fetch
- tall and steep
- closely spaced (11-15 wave breaks every minute)
- stronger backwash than swash
- very powerful so causes coastal erosion- beach removal
9
Q
Constructive wave
A
- formed from weak/light wind
- shorter fetch
- low in height
- widely spaced (6-9 wave breaks per minute)
- stronger swash than backwash
- beach building due to deposition
10
Q
Formation of headlands and bays
A
- headlands and bays form on discordant coastlines
- hard rock e.g. granite erodes more slowly forming a headland e.g. Peveril Point
- soft rock such as sandstone erodes more quickly, forming a bay e.g. swanage bay
- abrasion and hydraulic action most significant here
- beach forms in the bay due to wave refraction
11
Q
Formations of a wave-cut platform
A
- the sea attacks the headland at high tide
- hydraulic action and abrasion cause a wave-cut notch to form at the base of the cliff/headland
- overtime, the wave0cut notch grows in size becoming bigger and bigger
- the overhang above the notch collapses as it lacks support
- the process repeats causing the cliff to retreat inland
- this causes the wave cut platform to grow in site
- the wave cut platform is visible at low tide
- rock pools can form at wave-cut platforms
12
Q
Formation of a stack
A
- the crack forms along weaknesses in the rock due to erosion
- the crack widens due to hydraulic action and abrasion forming a cave
- the cave grows in size and is eroded through the headland forming an arch
- the roof of the arch collapses due to lack of support forming a stack
- the stack erodes down - weathering also breaks down the stack- forming a stumo
- real life examples are Old Harry, Dorset
13
Q
Longshore drift
A
- the swash moves the pebble up the beach in a north-east direction due to the direction of the prevailing wind whihc comes from the south-west
- the backwash takes the pebble straight down the beach in a southerly direction 90 degree angles to the coast due to the force of gravity
- the whole process repeats causing the pebble to move from west to east in a zig zag formation.
14
Q
Formation of a spit
A
- longshore drift moves material along the coast from west to east
- when the coastline changes direction, longshore drift continues, forming a spit
- a hook forms on the end of the spit if direction of the prevailing wind changes
- the water behind the spit is sheltered so deposition occurs forming a salt marsh
- the fast river flow stops the spit extending across the river mouth
15
Q
Where does a spit form?
A
-where the coastline changes direction