P1: Coastal Landscapes Flashcards
erosion
when soil and rock is worn down
Abrasion
sandpapering effect of pebbles grinding over a rocky platform causing it to become smooth
corrasion
fragments of rock are picked up and hurled by the sea at the cliff acting like tools.
Hydraulic power
waves smash into cliffs. trapped air is forced into holes and cracks the rock
attrition
rock fragments carried by the sea knock against one another causing them to become smaller and more rounded
suspension
floating on the water
solution
dissolved in the water
traction
rolling over sea bed
saltation
bounce over sea bed
Long Shore Drift
prevailing wind send waves. The swash comes up at an angle and backwash perpendicular to the coast. It is then carried to groynes
Destructive waves
Destroy beaches, tall and not wide, strong swash and weak backwash
Constructive wave
Create beaches, Small and wide, strong backwash and weak swash
Wave formation
fetch - the distance the waves travel to coast
Wave speed and duration
Breaking waves
- winds make waves circular
- Friction with seabed stops circular motion
- Increasingly elliptical orbit top moves faster
- Waves break
- Water rushes up the beach
Mass movement
the downslope movement or rock and soul under the influence of gravity
Landslide
blocks of rock sliding down a slide plane
rockfall
rock fragment breaking away down a screeslope
slumping
saturated soil slumping along a curved surface
mudslide
saturated soil flows down a slope
Weathering
the breakdown of rock in situ
Mechanical weathering
water freezes in gaps and expands in size by 9% over time more and more freezes making it bigger.
Biological weathering
plants grow into gaps and loosen rocks breaking them down .animals also dig holes in rocks and open up gaps
Chemical weathering
also called honeycomb weathering is when salts erodes rocks
Deposition
happens when a wave loses energy and drops its sediment load to the seabed
Four conditions for Deposition
constructive waves, shallow beaches, short fetch, low energy
Concordant coastline
bands of resistant and less resistant rock running parallel to the coastline
Discordant coastline
bands or resistant and less resistant rock running perpendicular to the coastline
Bays and Headland formation explanation
. Discordant Coastline
. differential erosion occurs and less resistive material gets erodes very quickly.
. The water becomes deeper at bays and shallower at areas of headlands.
.Wave refraction occurs and the energy is spread out and concentrated at headlands.
Headlands erosion
The wave refraction causes a crack in the cliff.
Expands into a cave.
An arch is formed- holes on both sides after erosion.
The weathering gets too much and it can not bare the weight and collapses.
At low tide, you can see a slump.
Coast retreats
Spits formation
prevailing winds send waves towards the shore causing long shore drift.
This causes deposition which creates a spit at a point where land changes direction.
When half the entrance to the river is covered then the spit cannot increase and waves are refracted to form a hook.
Water gets stuck in the hook creating a salt marsh.
Pioneer species then grow in this area.
e.g. Spurn heads North Yorkshire.
Dunes formation
Onshore winds pick up sand from the beach and transport it inland.
Sand accumulates behind an obstacle such as grass or litter.
As the dunes grow vegetation is used to bind the sands together and stop the dunes from crumbling.
Only form on wide beaches with plenty of sand.
Dunes are blown backwards over time a process known as dune migration
Types of dunes
embryo - <1m tall. exposed and loose sand
foredune - slightly large with more vegetation
yellow dunes - same as above but vegetation is more
Mature dunes - can support shrubs and small trees
Holderness coast
erodes due to bands of less resistive and more resistive parrallel to the sea.
Shoreline management plan in place to slow down erosion
Coastal management strategies
Sea walls
Beach reprofiling
Revetment
Gabions
Beach nourishment
Rock armour
Managed retreat
Offshore breakwater
Groynes
CS : Mappleton
North east England, Yorkshire
Why? Cliff made of boulder clay - very weak.
Large fetch, narrow beaches
Schemes Used : Grannite revetments
two rock groynes
Vegetation
Impacts :
- no further erosion
- new infrastructure to promote tourism
- erosion doubled further south
- Spurn head eroded and become a tidal island.