Physical landscapes - coasts Flashcards

(64 cards)

1
Q

how are waves formed

A

wind blows over the sea and friction with water surface causes ripples to form
these develop into waves
shallowing water and rising sea floor affects the wave’s orbital movement, becomes more elliptical
wave crest rises up and eventually breaks

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2
Q

constructive waves

A

low vs length
strong swash and weak backwash
less frequent 6-8per min
produce wide, sandy beaches with a gradual beach angled

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3
Q

destructive waves

A

tall vs length
weak swash and strong backwash
10-14 per min
break downward with great force, eroding the beach to make a steeper angle
pebble beaches often produced

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4
Q

mechanical weathering

A

is the disintegration of rocks
piles of fragments are found at the cliff foot

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5
Q

eg salt weathering

A

type of mechanical
water evaporates, leaves salt crystals which grow and expand, causing pressure on the rock

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6
Q

chemical weathering

A

caused by chemical changes
rainwater slowly dissolves rocks

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7
Q

eg carbonation

A

rainwater absorbs co2 and becomes acidic, when it comes into contact with alkaline rocks such as chalk/limestone a chemical reaction is produced
rocks slowly dissolve

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8
Q

mass movement

A

downward movement of material under the influence of gravity

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9
Q

sliding

A

large blocks of rock slide down a cliff face as a landslide, often triggered by heavy rainfall or earthquakes

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10
Q

slumping

A

involves the collapse of saturated or weak rocks e.g sand or clay, often along a curved surface

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11
Q

rock falls

A

fragments of rock break away from the cliff face to form scree

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12
Q

erosion

A

the wearing away of earth’s surface by the action of wind or water

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13
Q

hydraulic action

A

destructive waves hit the base of cliffs
water enters cracks, joints and faults at high speeds
air in these cracks is compressed with explosive force
this, repeated, causes cracks to widen and the cliff to weaken and material breaks off

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14
Q

abrasion

A

waves have the energy to carry material and at times large rocks
this material is thrown at the cliff face, scratching and scraping the surface

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15
Q

attrition

A

rock fragments carried by the sea collide and become smaller over time
jagged edges are worn away to produce small pebbles

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16
Q

traction

A

largest pieces of material are rolled along the seabed by the force of water
good when there is lots of power in the water

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17
Q

saltation

A

load is bounced along the sea bed e.g shingle
currents cannot keep heavier sediment afloat for longer periods

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18
Q

suspension

A

small particles are carried in the water

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19
Q

solution

A

materials often derived from limestone or chalk are dissolved and carried

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20
Q

longshore drift

A

process by which waves move material along the coast

waves approach the coast at an angle due to the prevailing wind direction
swash carries material toward the beach at an angle
backwash flows back to the sea down the beaches slope at 90 degrees due to gravity
process repeats itself along the coast in a zigzag movement

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21
Q

deposition

A

waves drop and leave behind the load they were carrying
takes place in areas where the flow of water slows down (low sheltered bays)
here the waves lose energy and sediment can no longer be carried
also occurs when water is trapped by landforms such as spits or engineered structures

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22
Q

headland

A

a cliff that juts out into the sea, comprised of hard rock

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23
Q

bay

A

crescent shaped indentation in the coastline, found between headlands

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24
Q

bays and headlands formation

A

form along discordant coastlines where hard and soft rocks alternate along the coast
these erode at different rates and less resistant rock such as clay is worn away
bays are sheltered by headlands and become low energy environments where deposition occurs

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25
headland features formation
large crack is enlarged by the on/off pressure of hydraulic action crack grows into a notch and then a cave as destructive waves converge on the headland and continue to erode it over time the cave becomes larger; water refraction draws waves to all sides of the headland so caves may form back to back sea breaks through the back of the caves, cutting through the headland to form an arch - base is widened as notches form weathering weakers the top of the arch which eventually collapses, leaving a pillar of detached rock called a stack notches form at the base of the stack and it becomes unstable eventally topples leaving only its base, the stump
26
wave cut platform formation
sea attacks cliff base between high and low tide mark dent or wave cut notch is formed by erosional processes e.g abrasion and hydraulic action notch increases in size, cliff becomes unstable as it is undercut; materials fall off into the sea as the cliff begins to collapse platform is left - the very base of the cliff below the sea the process repeats and the cliff continues to retreat
27
wave cut platform
area of bedrock at the base of some cliffs, seen at low tide has deep cracks in some places, rock pools, bare rock, may be smoothed by attrition, slopes gently to the sea
28
beaches
deposits of sand and shingle at the coast formed by constructive waves depositing material to build up the beach sand beaches are flat and wide, backwash moves small particles back down to form a gentle slope, mainly found in sheltered bays pebble beaches are steep and narrow; finer sand washed away
29
sand dunes
form on the dry backshore of a sandy beach need a large sand supply, onshore wind, a flat beach and an obstacle embryo dunes form around deposited objects like rocks and wood these develop and become stabilised by vegetation e.g marram grass, form fore dunes and yellow dunes rotting vegetation adds organic matter to the sand increasing fertility - more plants found on back dunes wind can form depressions in the sand - dune slacks - where ponds can form
30
spit
a long, narrow finger of sand/shingle jutting out into the sea from the land form on the coast where there is significant lsd if the coastline changes orientation and bends sharply, sediment is deposited out to sea, building up as an extension from the land strong winds can cause the end of the spit to be curved into a hook mud flats and salt marshes can form in the sheltered land behind
31
bar
spit stretching across a bay by lsd, trapping a freshwater lake or lagoon
32
tombolo
spit stretching out from the mainland to connect an island
33
jurassic coast
located in sw england, coast of channel stretches from bridport to bournemouth, discordant old harrys rock - chalk stump swanage bay - chalk, clay, limestone durdle door - limestone arch
34
hard engineering management strategies
built to alter or defend the environment; include anything designed to prevent cliff erosion along the shore or at the cliff foot
35
sea wall
built along cliff front or beach back, often recurved to relfect waves back on themselves and impede the next
36
sea wall benefits
can last up to 50 years sense of security promenade on top and seating at base doesn't impede the movement of sediement downdrift so no disadvantage to other areas
37
sea wall costs
restrict people's access to the beach unsightly can destroy habitats expensive to build + repair at £5000 per metre
38
rock armour
large boulders of hard rock placed on the cliff base, absorb wave energy
39
rock armour pros
cheap and easy to build long lasting versatile - can lengthen the lifespan of a seawall or stabilise dunes
40
rock armour cons
ugly imported rocks are preferred causing tension need regular maintenance potentially hazardous
41
gabions
rocks and boulders encased in wired mesh, placed at the beach back to absorb and dissipate wave energy
42
gabions pros
cheap and easy to build often constructed on site quick fix and good value blend in well
43
gabions cons
easily destroyed, repairs dangerous to birds and people when damaged unsightly if damaged use is restricted to sandy beaches
44
groynes
wood or stone barriers constructed at right angles to the beach trap material and stop transportation by longshore drift; wide beach is encouraged helping to absorb wave energy and reduce erosion
45
groynes pros
cheap and long lasting larger beach attracts tourists can be used to walk along, or as wind breaks
46
groynes cons
unattractive problem is merely passed on, not halted can be dangerous to kids and surfers restrict walking along the beach
47
soft management strategies
adapt and encourage natural processes to take place
48
beach nourishment
replacement of sediment lost through lsd shingle is dredged from the seabed and pumped
49
beach nourishment pros
natural, blends in, makes a wider beach may attract tourists protects people living along the seafront and expensive properties
50
beach nourisment cons
hiring a dredger is expenive so high overheads access to the beach is restricted for several weeks
51
beach reprofiling
artificial reshaping using existing material bulldozers move shingle up the beach wave energy is absorbed and dissipated by the beach, reducing erosion
52
beach reprofiling pros
residents feel safer ecosystems behind the beach are protected looks natural
53
beach reprofiling cons
can be expensive machines restrict beach access may look uninviting to tourists if the beach is steep and high crested
54
sand dune regeneration
artificial creation of new dunes or restoration of existing ones results in a physical barrier between sea and land, absorbing wave energy
55
sand dune regeneration pros
maintains a habitat often uses volunteer labour and local grass so is cheap protects the land behind popular as a walking or picnic area
56
sand dune regeneration cons
no guarantee it will last - dynamic environment has to be checked often systems must be put in place to prevent areas being trampled fenced off whilst being established - off putting
57
managed retreat
a deliberate policy allowing the sea to erode or flood an area allows sea to indundate land and create new intertidal habitats more sustainable longterm
58
medmerry sussex
on the stretch of the se coast most affected by flooding new embankment created with a channel behind rock armour built up intertidal area created finished in 2014, first such scheme in the UK
59
managed retreat pros
cheaper than having to maintain hard engineering methods may take pressure off areas further down the coast and reduce the risk of flooding designed to conserve or enhance natural environment - new habitats created
60
managed retreat cons
people are moved out and buildings are demolished - disruption and distress as communities are split up relocation makes short term costs high large areas of agricultural land are lost bird habitats affected eg cranes, bittern
61
coastal management scheme lyme regis - why
cliffs are unstable and prone to landslides and erosion harbour is used for fishing and cliffs are important for fossil studies is a large tourist destination on the south coast
62
lyme regis management strategy
phase 1 - 90s (60m) sea wall and promenade, cliff nailing to emergency stabilise cliffs phase 2 - 2005-7 (22m) new sea walls/promenade, wide shingle and sand beach created, extension of rock armour at the cobb phase 3 - scrapped phase 4 - 2013-5 (19.5m) 390m sea wall in front of old one lots of nailing, piling and drainage to stablilise the cliff and protect homes
63
lyme regis outcomes pros
defences have stood up to recent stormy winters, fewer landslides harbour is better protected, benefitting boat owners and fishermen new beaches increase visitor numbers so seafront businesses can thrive
64
lyme regis outcomes cons
more visitors so more traffic and litter have new defences spoilt the natural landscape new sea wall will interfere with coastal processes and affect neighbouring stretches of coastline - conflict elsewhere stabilisng cliffs will prevent landslips exposing important fossils