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Dynamic zone
Zone of rapid change with constantly changing inputs and outputs of energy and material
Swash
The forward movement of a wave up a beach
Backwash
The backward movement of water down a beach when a wave has broken
Fetch
Distance a wave travels over
Solution
Where sea water reacts with soluble
Abrasion
Waves lift sand and sediment and throw it at coastline and slowly erode it
attrition
In the sea, sediment is moved over hits other sediments and sediments get smaller and rounder
Hydraulic action
The force of the water breaks rock particles away from the river channel
Prevailing wind direction
The direction from which the wind blows most
often.
Longshore drift
The movement of water and sediment down a beach caused by waves coming in to shore at an angle
headland vs bays
headland=hard rock
bays=soft rock so erodes quicker
wave cut notch platforms
-sea attacks base of cliff
-wave cut notch formed by erosion
-notch increases in size, cliff is unstable so collapses leading to retreat of cliff face
-backwash carries eroded material and leaves wave cut platform
Deposition
when waves deposit material they loose energy, they depose the heaviest material first.
how are caves, arches, stacks and stumps formed
-cracks widen in headland via hydraulic action
-waves grind cracks to form an a cave
-cave becomes larger and breaks to form arch
-base of arch gets wider due to erosion until collapses to form stack
-stack is undercut at base until collapses to form stump
landforms of deposition
spits
estuaries
beaches
spits
areas of beach that only joins to main part of land at one end
form when there is a change in direction of coastline
beaches
pieces of land which separates inland area from a body of water
estuaries
where rivers meet the sea
when there is less water, river deposits silt to form mudflats
Erosion-hydraulic action
-lines of weakness on cliff=vulnerable
-waves reach base of cliff
-air trapped inside cracks
-when waves retreat-explosions of air back into notch
-distinct wave cut notch forms
-cliff is slowly undercut
-large overhang develops
-cliff collapses
-wave cut platform forms
-cliff erodes backwards
Traction
Heavy sediment that settle down on ocean floor
Saltation
Materials bounce along sea bed E.g small pebbles
Suspension
Sediments remain in the water as not heavy enough to settle on the floor but not light enough to float
Solutions
Minerals are dissolved in water and are carried in a solution
Erosion
Processes by which rock, sand, and soil are broken down and carried away
Weathering
The breaking down of rocks and other materials on the Earth's surface.
Chemical examples
Acid rain
Biological example
Plant roots
Permeable rocks
Rocks that allow water to seep through
Impermeable rocks
rock through which liquids cannot flow
Soft engineering
Managing erosion by working with natural processes to help restore beaches and coastal ecosystems
Hard engineering
Building artificial structures such as sea walls aimed at controlling natural processes
Rock armour
Large boulders dumped on the beach as part of the coastal defences.
Recurved sea wall
Wall of concrete which is curved to refract the waves
Groynes
Wooden, stone or concrete barrier built at right angles to the beach.
Gabion
Steel wire mesh filled with boulders used in coastal defences.
Beach replenishment
The process by which sand that was lost through long shore drift or erosion is replaced from a source outside of the beach it was lost from.
Marram grass
type of grass that is adapted to windy, exposed conditions and is used in coastal management to stabilise sand dunes
Wetland creation
Creation of marshes- land that is wet for significant periods of time.
Holderness coast
east coast of england
extends 61km from flamborough head in the north to spurn head in south
2metres of erosion per year
23 towns lost since roman times
Hornsea management strategy
Sea wall and beach replenishment
Mappleton management
- 1991 £2million spent on rock revetments and rock groynes.
Attwick management
No management
Spurn Head, Holderness Coast
example of salt marsh ecosystem - recurved spit shelters mud flats behind it
Wallasea island
NE of southend
lies at heart of internationally- important estuary
lots of farmland but no housing so project was suitable
Wallasea island management
-breached sea walls and the land has been able to flood
Holding the line
Keep current defences and maintaining them
Advance the line
A coastal management strategy which involves pushing the coastline further towards the sea e.g. Bournemouth.
Managed retreat
Allowing controlled flooding of low-lying coastal areas or cliff collapse in areas where the value of the land is low.
Do nothing
Where no action is taken to protect the coastline
conflicted views on management
farmers-want land protected due to farmland
council-want to spend money on services for locals
how might climate affect coastal processes
higher sea levels speed up erosion and attack coastal land
freezing temps also increase weathering
what human activities impact coastal landscapes
cattle farming
tourism
fishing
coastal management
water sports
storm surges
a temporary localised rise in sea level caused by low pressure in atmosphere
how might storm surges influence coastal processes
erosional-increase coastal erosion
transportation- increase longshore drift
depositional-when surges ends=increased deposition
how might geology influence coastal landscapes- Tee-Exe line
-where area of high land meets sea, there will be a cliff
-erosional landforms e.g caves are more common to N and W of Tee-Exe line-harder
-depositional landforms more common in S and E of line-softer
how might geology affect rates of erosion
less resistant rocks=more eroded so more to deposit
HIC coastal community
jaywick
jaywick
north essex
most deprived neighbourhoods
at sea level and at threat of being flooded
protection in jaywick
£10 million project to improve defences
150 steel piles to raise and strengthen sea wall
over 14000 tonnes of rock armour placed in front of sea wall
why is it difficult to manage the consequences of climate change and sea level rise in UK
-economy
-inevitable
-location
-community
-sustainability
LIC coastal communites
Maldives and Tuvalu