coastal systems and landscapes Flashcards

(109 cards)

1
Q

What is a coastline?

A

a part of land near the sea that is an open system, as it interacts with its surroundings

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2
Q

What is a closed system?

A

one that doesnt interact with its surroundings

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3
Q

What is a dynamic equilibrium?

A

when inputs and outputs of a system are balanced

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4
Q

What are the inputs of a coastline?

A

-energy from waves, wind, tides, currents
-sediment
-geology
-sea level change

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5
Q

What are the ouputs of a coastline?

A

-dissipation of wave energy
-accumulatioon of sediment above tidal limit
-sediment removed beyond coastline

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6
Q

What is fetch?

A

the distance a wave has travelled

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7
Q

What are the different zones of a coastline?

A

-backshore
-foreshore
-nearshore
-inshore
-offshore

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8
Q

What is the backshore zone?

A

the area above the high tide mark, affected by wave action only during major storm events. Where sand dunes are located

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9
Q

What is the foreshore zone?

A

the area between the high tide and the low tide mark

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10
Q

What is the nearshore zone?

A

the area of shallow water beyond the low tide mark, where a wave breaks

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11
Q

What is the inshore zone?

A

area between LWM and point where waves cease to have influence on land beneath them

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12
Q

What is the offshore zone?

A

area beyond the point where waves don’t have impact on land beneath them

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13
Q

What are the characteristics of a constructive wave?

A

-long wave length
-little wave height
-strong swash
-weak backwash
-found on low energy coastline

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14
Q

What are the characterisitics of a destructive wave?

A

-short wave length
-wave height over 1m
-weak swash
-strong backwash
-found on high energy coastline

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15
Q

What is wave refraction?

A

the distortion of wave fronts as they approach an intended shoreline

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16
Q

What are tides?

A

changes in water levels of the sea/ocean due to the gravitational pull of the moon

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17
Q

Explain spring tides

A

when the sun and moon are both align in a straight line with the earth, highest tidal range

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18
Q

Explain neap tides

A

when the moon and sun are positied at 90 degrees from the earth, lowest tidal range

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19
Q

What is a sediment cell?

A

a stretch of coastlin usually bordered by 2 prominent headlands where movement of sediment is more or less contained

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20
Q

What are the inputs of a sediment cell?

A

-cliff erosion
-onshore currents
-river transport
-wind blown sediment from land
-subaerial processes (weathering/mass movement)
-marine organisms

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21
Q

What are the outputs of a sediment cell?

A

-sand dunes (backshore)
-beaches (foreshore)
-bars (nearshore)
-barrier islands (offshore)

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22
Q

What are the transfers in a sediment cell?

A

-longhsore drift
-swash/backwash
-tidal currents
-sea/ocean currents
-wind

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23
Q

What is the coastal sediment budget?

A

balance between sediment added and removed in a sediment cell

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24
Q

What is weathering?

A

the breakdown/disintegration of rock from its orgignal place (in situ)

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25
What is freeze-thaw weathering?
-water enters cracks in rock -it freezes and expands widenin gthe crack -ice melts and water goes deeper in crack -process repeats until rock splits
26
What is salt crystallisation?
when sea water evaporates causing salt crystals to grow, exterting pressure on the rock causing cracks to widen. Slat also erodes ferrous rock.
27
What is wetting and drying?
When rocks such as clay expand when they are wet and contract when dried
28
What is carbonation?
rainwater absorbing CO2 from air to create carbonic acid which when reacting with calcium carbinate can easily dissolve it
29
What is solution? (weathering)
when rock minerals such as salt are dissolved
30
What are examples of mechanical weathering?
-freeze thaw - salt crystallisation -wetting and drying
31
What are examples of biological weathering?
root activity seaweed acids rock boring birds
32
What are examples of chemical weathering?
carbonation oxidation solution
33
How does root activity weather rock?
roots grow into cracks and exert pressure, splitting rock
34
How can birds weather rock?
dig burrows in cliffs - weakening the rocks
35
What is hydraulic action?
when a breaking wave traps air as it hits a cliff face and pushes it into cracks in a cliff face. When water draws back, an explosive effect is caused due to the change in pressure (also known as cavitation)
36
What is wave quarrying?
the force of water impacting rocks (also known as wave pounding)
37
What is abrasion/corrasion?
Material hurled at a cliff face or sediment being drawn back and forth on platform (bottom) grinding it away
38
What is attrition?
rocks which carry out abrasion are worn into smaller pieces by bashing against each other - sandpaper effect
39
What is solution? (erosion)
the dissolving of calcium based rocks
40
What is coastal erosion affected by?
wave steepness fetch of wave sea depth human activity
41
What is longshore drift?
occurs when waves approach a shore at an angle. Sediment is pushedup the beach via swash and pulled back into the ocean by backwash sediment in backwash is picked up by oncoming wave ovetime sediment moves in zig zag motion
42
What factors influence mass movement?
level of cohesion in sediment height of slope slope angle temperature level of saturation
43
What are landslides?
occur when sofer rock cliffs or ones with deposited material slip as a result of 'failure'
44
What are rock falls?
occur from cliffs undercut by sea or on slopes affected by mechanical weathering
45
What are mudflows?
when heavy rain causes large amounts of fine material to flow downhill
46
What is slumping/rotational slip?
where softer material overlies more resistant materials . Sections of cliff face rotate and 'slump'
47
What is soil creep?
very slow and continous movement of individual soil particles downslope
48
What are the inputs/ outputs of a coastline?
wave energy, wind currents and tides
49
What are the stores/ components of a coastal system?
barrier beaches, offhsore bars, spits
50
What is an example of negative feedback at a coast?
groynes
51
What is an example of positive feedback at a coast?
Headlands and Bays Wave cut platform
52
What are the sources of energy in coastal environments?
winds waves - constructive and destructive currents and tides
53
What are the different processes of transportation at a coast ?
Traction – larger material rolls along the sea floor Saltation – beach material bounces along the sea floor Suspension – beach material is suspended within the water and moved by the waves Solution - beach material is dissolved in the sea water and moved by the waves longshore drift - sediment moving in zig zag movement
54
How do headlands and bays form? Give a named example
headlands and bays form on a discordant coastline, where there are bands of hard and soft rock. Soft rock (like limestone and clay) is eroded more quickly, which leads to the formation of a bay. Due to wave refraction, bays are eroded more easily and headlands stick out in the ocean which are made of hard rock (like chalk )
55
Describe the formation of wave cut platforms
The waves attack the base of a headland and erode it more quickly A wave cut notch is formed The cliff collapses due to being unstable leaving a wave cut platform which is only visible at low tide. The cliff face retreats
56
Describe the formation of stacks and stumps
Cracks are widened in the headland through the erosional processes of hydraulic action and abrasion Waves continue to grind away at the crack, it opens up to form a cave Cave becomes larger and breaks through the headland to form an arch Roof of the arch becomes too heavy and collapses into the sea. This leaves a stack (an isolated column of rock) The stack is undercut at the base until it collapses to form a stump
57
What are the 2 types of beaches ?
Drift aligned - waves come at and angle so longshore drift takes place Swash aligned - waves are paralle4l to coastline to little horizontal movement
58
How are spits formed?
Drift aligned beach where longshore drift occurs Waves approach the shore at an angle due to the prevailing wind, swash carries sediment onshore Backwash then removes sediment out to sea in a straight line due to gravity Overtime, this transport sediment along the coast in a zig zag There is a change in shape in the headland which causes this to continue and deposit out to sea. Larger sediment is deposited first and begins to accumulate forming a “spit” out to sea The point closest to the headland is the proximal point, the distal point is the furthest away Eventually, spits will curve and “hook” due to the tides, waves and currents This shelters the water behind it leading to a salt marsh A compound spit is different, as it has several “mini spits” which form off of the main spit.
59
What are the 2 types of spits?
Simple - simple spit that cane be hooked Compound -has several “mini spits” which form off of the main spit.
60
How are tombolo's formed?
Drift aligned beach where longshore drift occurs Waves approach the shore at an angle due to the prevailing wind, swash carries sediment onshore Backwash then removes sediment out to sea in a straight line due to gravity Overtime, this transport sediment along the coast in a zig zag There is a change in shape in the headland which causes this to continue and deposit out to sea. Larger sediment is deposited first and begins to accumulate forming a “spit” out to sea The spit will continue out to sea until it connects to an island
61
How are bar's formed?
Drift aligned beach where longshore drift occurs Waves approach the shore at an angle due to the prevailing wind, swash carries sediment onshore Backwash then removes sediment out to sea in a straight line due to gravity Overtime, this transport sediment along the coast in a zig zag. There is a change in shape in the headland which causes this to continue and deposit out to sea. Larger sediment is deposited first and begins to accumulate forming a “spit” out to sea. This forms in coves and headlands and bays, eventually the deposited material re- joins the headlands This forms a lagoon behind it
62
What are barrier islands?
Long, thin, sandy stretch of land, oriented parallel to the mainland coast that protects the coast from the full force of powerful storm waves Between the barrier island and the mainland is a calm, protected water body such as a lagoon or bay
63
How are sand dunes formed?
- wind blows sediment onshore -sediment deposits behind an obstacle - embryo dunes are the youngest, smallest dunes - the first plants that start to from are called pioneer plants e.g maram grass - roots bind sand together making its stable - yellow dunes then form - dune slacks are low-lying areas within dune systems that are seasonally flooded and where nutrient levels are low - grey dunes follow up - mature dunes are the ones at biodiversity climax
64
What are ridges and runnels?
ridges and troughs running parallel to coast near LWM they are formed by deposition during backwash broken by drainage channels
65
What are ripples?
small elomgated ridges froming on the beach waves and currents flow across loose sand which forms ripples along whole length of beach
66
What are cusps?
semi circular shaped 'depressions' with coarser material around edge and finer material in centre formed by a collection of waves reaching the same point and backswash scouring out finer material
67
What are berms?
small ridges that form near HTM deposited by swash of constructive waves
68
What is a storm beach?
a ridge found near the back of the beach composed of larger sediment picked up during a storm
69
What is thermal expansion?
when water takes up more space when it gets more warmer
70
What is isostatic change?
rising or falling of a land mass relative to the sea resulting from the release of the weight of the ice after the last ice age
71
What is eustatic change?
Variations in the sea level resulting from changes in the amount of liquid water entering oceans e.g melting ice caps
72
What is an emergent coast?
coastlines created where there has been a relative fall in sea level
73
What is an submergent coast?
coastlines created where there has been a rise in relative sea level
74
What is tectonic change?
sea-floor spreading stretches the basin making the sea level fall
75
What are examples of a sumergent landforms?
rias fjords dalmation coasts
76
What are rias?
drowned river valleys river valleys flood only showing high land e.g. Kingsbridge estuary in South Devon
77
What are fjords?
drowned glacial valleys U shaped valleys left by glaciers are submerged e.g. Western Norway
78
What are Dalmation coasts?
areas of the world where valleys (especially glacial valleys) lie parallel to each other. Appear to be a series of islands that run parallel to the coastline
79
What are examples of emergent landforms?
raised beaches relict cliffs
80
What are raised beaches?
when land has risen in comparison to sea levels - level of land is now higher than it used to be
81
What are relict cliffs?
Wherever land has risen from the sea in the past and cliffs can often be seen that are no longer reached by the sea gentle vegetated slopes are seen e.g. north-west of Scotland
82
What is an emergent coast?
a coastline exhibiting features associated with falling sea levels e.g. raised beaches and relict cliffs
83
What is a submergent coast?
a coastline exhibiting features associated with rising sea levels e.g. Rias and Fjords
84
What are fjords and a named example?
a drowned glacial valley e.g. western Norway
85
What are Dalmatian coasts and a named example?
coasts that form where especially glacial valleys lie parallel to each other and then are flooded, only tops are seen e.g. Dalmatian Coast -Croatia
86
What is a cost benefit analysis?
when costs are forecast and compared to expected benefits in order to decide what to do with a coastline
87
What is hard engineering?
physical changes to a coastline to a coastal systems to control natural processes
88
What is soft engineering?
natural systems are used to defend against natural processes
89
What is a sea wall? Pros and Cons
a recurved structure that deflects waves back to sea -provide a physical barrier and raise height of beach -need drain outlets, easily eroded if cracks are present
90
What is rock armour? Pros and Cons
large boulders placed in front of a cliff to absorb wave energy -angular to expand surface area -not secured in place, can be moved by waves
91
What are gabions? Pros and Cons
smaller boulders contained in steel wire mesh cages -absorb wave energy -can be eroded by waves
92
What are reventments? Pros and Cons
concrete/wooden structures placed across a beach -take full force of energy -wooden is easily eroded
93
What is cliff fixing? Pros and Cons
driving metal bars into cliff face -stabilises cliff and absorbs wave energy -expensive
94
What are offshore reefs? Pros and Cons
offshore reefs -force waves to break offshore -difficult to install
95
What are barrages? Pros and Cons
large structures that prevent flooding on major estuaries -act as a dam across an estuary -unappealing to tourists, alters habitat
96
What are beach nourishment? Pros and Cons
replaces material lost through longshore drift -low environmental impact -ongoing maintenance cost
97
What is dune regeneration? Pros and Cons
replanting vulnerable areas with marram grass -provide natural protection from the sea -no guarantee that the sand dunes will stay in place. They may be damaged by storms or by people walking over them.
98
What is managed retreat? Pros and Cons
abandoning current line of sea defences and exposing land to sea -act as a defence against rising sea level -infrastructure and properties lost
99
What is land use management? Pros and Cons
encouraging landowners to give up land for grazing -decreases infrastructure lost -cannot remedy damage done
100
What are the pros and cons of doing nothing?
-owners lose land -let nature take its course
101
What are the 4 DEFRA strategies?
-hold the line (MAINTAIN CURRENT POSITION OF COASTLINE) -advance the line (EXTEND COASTLINE OUT TO SEA) -managed retreat (ALLOW RETREAT IN MANAGED WAY) -do nothing
102
What is integrated coastal zone management (ICZM) ?
a holistic approach to managing coastal areas, involving various stakeholders and focusing on sustainable development, environmental protection, and risk management
103
What is background information on Odisha?
-South-east coast, bordering Bay of Bengal Straight coastline, 480km long 6 deltas ‘Hexadeltaic’ region or ‘Gift of the Six Rivers’ 1435km² mangrove forest Chilika Lake - salty lagoon renown for bird life Less salty in monsoon season Coastline of deposition, significant sediment store. Rivers important transfer of sediment to the system.
104
What are opportunities in Odisha?
Flat land for settlement. Variety of marine and coastal flora/fauna including mangroves, sea grasses, salt marshes, sand dunes, estuaries and lagoons. Large stocks of fish, mammals, turtles Potential for offshore wind, tidal and wave energy 35% of coastline has significant minerals and heavy metal deposits e.g. clay and limestone Opportunities for offshore oil and natural gas and mining Many people employed in fishing and aquaculture such as shrimps Cultural and archaeological sites along the coast attract tourists as well as beaches and wildlife sanctuaries. Chilika Lake Bird Sanctuary has over 150 species.
105
What are risks in Odisha?
Rates of erosion increased in recent decades through natural processes and human intervention Increasing concern about vulnerability to storm surges and tsunamis as well as longer term threats from rising sea levels Risk of storm surges from tropical cyclones (climate change) Attempt to halt erosion with hard engineering removes important input of sediment that is needed to form beaches, dunes and barrier beaches 50 years ago Odisha had average 5.1km of mangroves, today 1.2km
106
What are the erosion/deposition rates in Odisha?
Findings from 2011 Assessment of Shoreline Change: - 46.8% accretion, 36.8% eroding, 14.4% stable. - Most accretion is in the north near deltas - Most erosion in the south. Here hard-engineering structures protect ports - Kendrapara, Bhadrak and Baleshwar have 50% higher accretion elsewhere due to mangroves Shoreline change most significant at river mouths
107
What was the cyclone event in Odisha?
October 2013 Cyclone Phailin struck near Gopalpur. Wind speeds of 200mph – power lines torn down, trees uprooted, 1 million evacuated, 44 died, 500,000 agricultural crops destroyed, economic loss of US $700,000. Ecosystem surrounding Lake Chilika may take years to recover
108
What management has took place in Odisha?
ICZM - Integrated coastal zone management Establish sustainable economic and social activity Involve stakeholders e.g. Odisha State Disaster Management Authority and Wildlife Wing of Forest and Environmental Department and Greenpeace India
109
Wave cut platform formation
-Wave Cut Platforms form at headlands where the process of wave refraction concentrates high energy waves at the cliffs. -During high tide, erosive processes such as wave quarrying and hydraulic action erode the base of the cliff. -This is particularly powerful in neap tides where there is a lower tidal difference which concentrates wave energy at the base of the cliff for longer. -Eventually this forms a wave cut notch which leaves the cliff above unsupported. -Mass movement will occur when the cliff above collapses due to gravity into the ocean. -This leaves behind a wave cut platform which is visible from low tide.