Crowded Coasts Flashcards

Unit 2

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1
Q

What is the literal zone?

A

Area where the and meets the sea including the shoreline and the shallow water near the coast

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2
Q

3 Main zones for the literal zone

A

Backshore-Area between high tide mark and the lanward limit

Nearshore-Extends from the low tide mark to where waves break at low tide

Offshore-Beyon the nearshore zone where water depth increases rapidly

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3
Q

What is the dynamic zone

A

Where the land and sea interact, leading to constant changes in the coastal landscape

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4
Q

How does jointing effect coastal morphology

A

Jointing-natural fractures or cracks

-influence, shape and stability
-Differential erosion can lead to stacks and stumps

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5
Q

How does Dips affect coastal morphology

A

The angle at which rock layers incline from the horizontal

-can effect stability of rocks and rate of erosion
-Steep dipping = more erosion

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6
Q

How does faulting effect coastal morphology

A

Displaced fracures

-Creates weak rock

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7
Q

How does folding affect coastal morphology

A

The bending of rock layers due to tectonic forces

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8
Q

What does coastak bedrock lithology mean

A

Refers to the type of rock that makes up the coastal cliffs or headlands

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9
Q

Types of bedrock

A

Sedimentary
- formed by the depision of material at the earths surface and within bodies of water (not very resistance) E.g limestone

Igneous
-rock found near volcaones. cooled and solidifies magma or lava (resistant)

Metamorphic
-Physica/chemical changes to pre-existing rock (resistat)

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10
Q

What is unconcolidated rock?

A

loose, material such as sand,gravek and clay found in coastal areas

Influence on coastal ression- increase ersion

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11
Q

Erosion processes

A

hydraulic action - force of water hitting cliff face (leads to cracks and crevices

Abrasion- wearing away of the cliff face by material carried by the sea (undercutting)

Attrition- the wearing away of rocks particles as they collide with each other (forms sediment)

Corrosion - Weak acid n the sea water reacts with particular rock material, causing erosion and weakening

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12
Q

Types of weathering

A

Biological- living organism ( increase pressure = breack)

Chemical- chemical reaction that alters the comparision of rocks. Changes the mineral composion of rocks, breacking them down, forming new minerals

Physical- Freeze thaw and onion skin

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13
Q

Definition of mass movement

A

Large downhill movemnt of material usually from a cliff face

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14
Q

Types of mass movement

A

Rockfal-rapid downhill movement of rock from a steep slope or cliff (caused by weathering)

Rotational slide - Movement of rock or soil along a curved surface (caused by saturation of soil or rock- decrease friction and stability)

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15
Q

What is longshore drift

A

Movement of sediment along a coast at an angle to the shoreline, driven by waves approaching the beach at an angle

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16
Q

Process of longshore drift

A

Waves approches at an angle due to prevaling winds

Waves breack, swash carries sediment up the beach at an angle

BAckwash carries sediment straight back down the beach

Affected by
-wave energy
-beach gredient
-obsticles-headlands and groynes

17
Q

What is the sediment cell cycle concept

A

Divides the coastline into distinct units or cells, each woth its own source, ransfer and sinks of sedniment

18
Q

processes and examples of the sediment cell cycle concepts

A

Source of sediemnt
- erison
-river sedement
-offshore sources

Transerfer
-long shore drift

Sinks
-Beaches
-sand dunes
-off shore deposional features

Impotance
- Effective coastal managment
-biodiversity
-erosion and depesion ballance

19
Q

What is pant succession

A

process by which plants communities change over time in a particular area

Primary- area where no soil exits
Secondary-soil is present but has now been disturbed

20
Q

How are sand dunes made

A

1) sand builds up aorund obsticle
2) Pioneer plants like mariam grass colonisebare sand
3) Marram grass has deep roots that bind the sand, reducing erosion and stablising dune
4) as amrium grass grows, it traps more sand, creating a more stable envorment for other plants to colonise
5) over time a diverse plany community develops, futher stabilising the dune

21
Q

Benefits of sand dune

A

Physical barrier

Wave dissipation - veg absorb waveenergy

perventing erosion -root syste, binds soil together

Habitat creation

22
Q

Stabilisation of salt marshes

A

Colinisation-pionner palnst like cordgrass clonises muddy areas

the plant then trap sediment, builiding up siil, raising marsh surface

Root system decreases erosion therefore increadeing marsh stability

Marsh rises =more species increasing diversity

23
Q

Enviromental benifits of salt marshes

A

Carbon sequenstatration
Water filtration
ecosystem services

24
Q

mangroves

A

Coastal wetlands found in tropical and subtropical regions consisting of salt tolorent mangrive tress

ecosystem services
- coastal protection -decrease erosion
- bioloveristy
-Carbon sequenstration

Economic oppotinities
-fisheris
-timer and non-timber product

Threats
-deforestation
-pollution
-Climate change

25
Q

Coral reefs

A

underwater calcium arbonate stirctures

Ecosystem services
-biodiversity
-fisheries
-coastal protection

Economic opotunities
-torism
-mesicine

Threats
-sea level
-overfishing
-pollution

26
Q

Global threats to coastal ecosystesms

A

Rising water temp

Sea level rise

ocean acidification (harmful to calcim carbonate sheels and disrupt =s food chain)

27
Q

land reclimation

A

Creating new land from ocean riverbeds or lakes

1) sedminent removed
2) Transporte and deposoted
3) reinforcent
4)development

28
Q

Environmental impact assessment (EIA)

A

Identifying predict and evalute potential enviromental impacts of proposed poject or development

Limitations:
Focus on technical aspects
Timing
predictive nature

29
Q

Cost and benifit analysis (CBA)

A

systematic proces for calculating and comparing the beifits and costs of poject or decisions . Asses the economic vialibilty of the project

process:
Identifying cost and benifits
-monetisation
-dicounting
-comparasion

limitations
- valuation issues
-subjectivity
-incomplete analysis