Coasts Flashcards

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1
Q

What is the littoral zone?

A

Boundary between land and sea. Defined as wider coastal zone.

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2
Q

Coasts are open systems, what does that mean?

A

Matter and energy can be transferred in and out of the system

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3
Q

4 inputs:

A

-Marine (tides, storm surges)
-Atmospheric (climate change, solar energy)
-Land (rock type, tectonic activity)
-People ( human activity)

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4
Q

5 processes:

A

-Weathering
-Mass movement
-Erosion
-Transport
-Deposition

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5
Q

3 outputs:

A

-Erosional landforms (arch, stack, headland, bay)
-Depositional landforms (spits, beaches)
-Different types of coasts

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6
Q

Coastal zones=

First one, Backshore
One feature of this zone:

A

Changes only during storms

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7
Q

Coastal zones=

Last one, Offshore
One feature of this zone:

A

Beyond point where waves cease to impact the seabed

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8
Q

4 factors that influence wave size:

A

.Fetch (distance wave has travelled)
.Wind speed
.Time wind has blown for
.Prevailing wind direction

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9
Q

What are high-energy coastlines?

A

Cornwall
Very rocky due to high energy waves, only hard rock remains.
Rate of erosion is higher than deposition.
Cliffs tend to be steep with little vegetation

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10
Q

What are low-energy coastlines?

A

Lincolnshire
Sandy beaches, salt marshes and estuaries with much less powerful waves.
Rate of deposition is higher than rate of erosion.
Land with gentle relief and low elevation

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11
Q

3 differences between destructive and constructive waves:

A

-Destructive waves are high and constructive waves are low
-High frequency of waves for destructive and low frequency for constructive
-Strong backwash in destructive (erodes), strong swash in constructive (deposits)

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12
Q

Examples for erosional landforms:

A

Headlands (Peveril Point) and bays (Swanage Bay)
Wave cut platforms
Caves, arches, stacks, stumps

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13
Q

Examples of depositional landforms:

A

Spits
Salt marshes
Cuspate forelands
Double spit
Bars
Tombolos

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14
Q

3 types of mass movement:

A

Landslide, material falls in straight line quickly

Rotational slumping, down curved angle

Blockfall (rockfall), broken blocks fall in steep cliff

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15
Q

Different landforms caused by mass movement:

A

Rotational scar, caused by rotational slumping, bit of cliff without vegetation

Terraced cliff profile, caused by multiple rotational slumps

Talus scree slope, caused by rockfall, larger rocks fall to bottom while smaller ones are at the top

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16
Q

3 types of weathering:

A

Mechanical -

Freeze thaw, wetting and drying, salt weathering

Chemical (Flamborough head cliff in Holderness) -

Carbonation, oxidation

Biological -

Plants and animals

17
Q

How does mass movement decrease rate of recession?

A

Mass movement adds rock material to beaches, strengthening beaches by increasing their size, slowing down and decreasing wave force.

18
Q

How is climate change affecting Nile delta?

A

Rising sea level is making low lying areas more saline, more difficult to farm and affects some fish species.

19
Q

What percent of Nile’s sediment does Aswan Dam hold?

A

98%

20
Q

Examples of emergent coastlines:

A

Raised beaches - West coast of Scotland
Fossil cliffs

21
Q

Examples of submergent coastlines:

A

Rias - Milford Haven in South Wales
Fjords - Norway, some over 1000 m deep
Dalmatian coastline - Croatia

22
Q

Where are there environmental refugees and where do they move to?

A

SIDS, Small Island Developing States, people in little islands like Tuvalu will move to countries unaffected by sea level rise like Australia

23
Q

Why is there political tension in Happisburgh, England?

A

Policy of managed retreat was introduced in late 90s, making the locals unhappy.

24
Q

Why did the Happisburgh residents’ protests not go their way?

A

Happisburgh did not qualify for new sea defences under the cost-benefit analysis, would have cost £15 million ( more than value of properties there).

25
Q

What actions are being made by North Norfolk District council?

A

Relocating caravan sites, public toilets and car parks
Purchasing the properties most at risk, at 40% of their value

26
Q

Case studies for each type of hard engineering strategy for coastal erosion:

A

Sea walls and groynes: Hornsea which led to increased erosion in Mappleton, by the 1990s nearly 4 meters of cliff were being eroded each year
Rock armor: Mappleton in 1991

27
Q

Disadvantages of offshore breakwaters and revetments (placed on foot of cliff)

A

Offshore breakwaters - can be navigation hazard and visually unappealing

Revetments - need high levels of maintenance

28
Q

Disadvantages of Dune stabilization and salt marsh creation (soft engineering strategies)

A

Dune stabilization - Time consuming to plant marram grass, people may respond negatively to being kept off an area too

Marsh creation - Agricultural land is lost, farmers need to be compensated

29
Q

Case study for salt marsh creation:

A

Blackwater estuary (1990s)

-3.5 km sea wall built hundreds of years ago was too expensive to maintain
-CBA showed not worth maintaining due to soil quality and land value being low
-Creeks were dug to promote formation of salt marshes
-Habitat created for Brent geese and marine invertebrates

30
Q

How are offshore bars formed?

A

Destructive waves erode sand from the beach with their strong backwash and deposit it offshore in bars

31
Q

Maldives facts:

A

-Very low lying nation that will be completely submerged within the next 50 to 100 years, 80% of land is less than 1 meter above sea level
-Maldives government asked Japanese government to give them $60 million to build 3 m sea wall to protect the capital (Male)