2.1 Coasts

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61 Terms

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Dynamic zone

Zone of rapid change with constantly changing inputs and outputs of energy and material

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Swash

The forward movement of a wave up a beach

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Backwash

The backward movement of water down a beach when a wave has broken

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Fetch

Distance a wave travels over

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Solution

Where sea water reacts with soluble

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Abrasion

Waves lift sand and sediment and throw it at coastline and slowly erode it

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attrition

In the sea, sediment is moved over hits other sediments and sediments get smaller and rounder

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Hydraulic action

The force of the water breaks rock particles away from the river channel

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Prevailing wind direction

The direction from which the wind blows most

often.

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Longshore drift

The movement of water and sediment down a beach caused by waves coming in to shore at an angle

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headland vs bays

headland=hard rock

bays=soft rock so erodes quicker

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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

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Deposition

when waves deposit material they loose energy, they depose the heaviest material first.

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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

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landforms of deposition

spits

estuaries

beaches

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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

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beaches

pieces of land which separates inland area from a body of water

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estuaries

where rivers meet the sea

when there is less water, river deposits silt to form mudflats

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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

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Traction

Heavy sediment that settle down on ocean floor

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Saltation

Materials bounce along sea bed E.g small pebbles

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Suspension

Sediments remain in the water as not heavy enough to settle on the floor but not light enough to float

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Solutions

Minerals are dissolved in water and are carried in a solution

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Erosion

Processes by which rock, sand, and soil are broken down and carried away

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Weathering

The breaking down of rocks and other materials on the Earth's surface.

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Chemical examples

Acid rain

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Biological example

Plant roots

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Permeable rocks

Rocks that allow water to seep through

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Impermeable rocks

rock through which liquids cannot flow

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Soft engineering

Managing erosion by working with natural processes to help restore beaches and coastal ecosystems

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Hard engineering

Building artificial structures such as sea walls aimed at controlling natural processes

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Rock armour

Large boulders dumped on the beach as part of the coastal defences.

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Recurved sea wall

Wall of concrete which is curved to refract the waves

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Groynes

Wooden, stone or concrete barrier built at right angles to the beach.

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Gabion

Steel wire mesh filled with boulders used in coastal defences.

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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.

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Marram grass

type of grass that is adapted to windy, exposed conditions and is used in coastal management to stabilise sand dunes

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Wetland creation

Creation of marshes- land that is wet for significant periods of time.

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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

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Hornsea management strategy

Sea wall and beach replenishment

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Mappleton management

- 1991 £2million spent on rock revetments and rock groynes.

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Attwick management

No management

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Spurn Head, Holderness Coast

example of salt marsh ecosystem - recurved spit shelters mud flats behind it

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Wallasea island

NE of southend

lies at heart of internationally- important estuary

lots of farmland but no housing so project was suitable

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Wallasea island management

-breached sea walls and the land has been able to flood

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Holding the line

Keep current defences and maintaining them

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Advance the line

A coastal management strategy which involves pushing the coastline further towards the sea e.g. Bournemouth.

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Managed retreat

Allowing controlled flooding of low-lying coastal areas or cliff collapse in areas where the value of the land is low.

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Do nothing

Where no action is taken to protect the coastline

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conflicted views on management

farmers-want land protected due to farmland

council-want to spend money on services for locals

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how might climate affect coastal processes

higher sea levels speed up erosion and attack coastal land

freezing temps also increase weathering

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what human activities impact coastal landscapes

cattle farming

tourism

fishing

coastal management

water sports

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storm surges

a temporary localised rise in sea level caused by low pressure in atmosphere

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how might storm surges influence coastal processes

erosional-increase coastal erosion

transportation- increase longshore drift

depositional-when surges ends=increased deposition

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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

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how might geology affect rates of erosion

less resistant rocks=more eroded so more to deposit

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HIC coastal community

jaywick

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jaywick

north essex

most deprived neighbourhoods

at sea level and at threat of being flooded

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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

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why is it difficult to manage the consequences of climate change and sea level rise in UK

-economy

-inevitable

-location

-community

-sustainability

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LIC coastal communites

Maldives and Tuvalu