P1: Coastal Landscapes Flashcards

1
Q

erosion

A

when soil and rock is worn down

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2
Q

Abrasion

A

sandpapering effect of pebbles grinding over a rocky platform causing it to become smooth

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3
Q

corrasion

A

fragments of rock are picked up and hurled by the sea at the cliff acting like tools.

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4
Q

Hydraulic power

A

waves smash into cliffs. trapped air is forced into holes and cracks the rock

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5
Q

attrition

A

rock fragments carried by the sea knock against one another causing them to become smaller and more rounded

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6
Q

suspension

A

floating on the water

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7
Q

solution

A

dissolved in the water

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8
Q

traction

A

rolling over sea bed

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9
Q

saltation

A

bounce over sea bed

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10
Q

Long Shore Drift

A

prevailing wind send waves. The swash comes up at an angle and backwash perpendicular to the coast. It is then carried to groynes

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11
Q

Destructive waves

A

Destroy beaches, tall and not wide, strong swash and weak backwash

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12
Q

Constructive wave

A

Create beaches, Small and wide, strong backwash and weak swash

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13
Q

Wave formation

A

fetch - the distance the waves travel to coast
Wave speed and duration

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14
Q

Breaking waves

A
  1. winds make waves circular
  2. Friction with seabed stops circular motion
  3. Increasingly elliptical orbit top moves faster
  4. Waves break
  5. Water rushes up the beach
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15
Q

Mass movement

A

the downslope movement or rock and soul under the influence of gravity

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16
Q

Landslide

A

blocks of rock sliding down a slide plane

17
Q

rockfall

A

rock fragment breaking away down a screeslope

18
Q

slumping

A

saturated soil slumping along a curved surface

19
Q

mudslide

A

saturated soil flows down a slope

20
Q

Weathering

A

the breakdown of rock in situ

21
Q

Mechanical weathering

A

water freezes in gaps and expands in size by 9% over time more and more freezes making it bigger.

22
Q

Biological weathering

A

plants grow into gaps and loosen rocks breaking them down .animals also dig holes in rocks and open up gaps

23
Q

Chemical weathering

A

also called honeycomb weathering is when salts erodes rocks

24
Q

Deposition

A

happens when a wave loses energy and drops its sediment load to the seabed

25
Four conditions for Deposition
constructive waves, shallow beaches, short fetch, low energy
26
Concordant coastline
bands of resistant and less resistant rock running parallel to the coastline
27
Discordant coastline
bands or resistant and less resistant rock running perpendicular to the coastline
28
Bays and Headland formation explanation
. Discordant Coastline . differential erosion occurs and less resistive material gets erodes very quickly. . The water becomes deeper at bays and shallower at areas of headlands. .Wave refraction occurs and the energy is spread out and concentrated at headlands.
29
Headlands erosion
The wave refraction causes a crack in the cliff. Expands into a cave. An arch is formed- holes on both sides after erosion. The weathering gets too much and it can not bare the weight and collapses. At low tide, you can see a slump. Coast retreats
30
Spits formation
prevailing winds send waves towards the shore causing long shore drift. This causes deposition which creates a spit at a point where land changes direction. When half the entrance to the river is covered then the spit cannot increase and waves are refracted to form a hook. Water gets stuck in the hook creating a salt marsh. Pioneer species then grow in this area. e.g. Spurn heads North Yorkshire.
31
Dunes formation
Onshore winds pick up sand from the beach and transport it inland. Sand accumulates behind an obstacle such as grass or litter. As the dunes grow vegetation is used to bind the sands together and stop the dunes from crumbling. Only form on wide beaches with plenty of sand. Dunes are blown backwards over time a process known as dune migration
32
Types of dunes
embryo - <1m tall. exposed and loose sand foredune - slightly large with more vegetation yellow dunes - same as above but vegetation is more Mature dunes - can support shrubs and small trees
33
Holderness coast
erodes due to bands of less resistive and more resistive parrallel to the sea. Shoreline management plan in place to slow down erosion
34
Coastal management strategies
Sea walls Beach reprofiling Revetment Gabions Beach nourishment Rock armour Managed retreat Offshore breakwater Groynes
35
CS : Mappleton
North east England, Yorkshire Why? Cliff made of boulder clay - very weak. Large fetch, narrow beaches Schemes Used : Grannite revetments two rock groynes Vegetation Impacts : - no further erosion - new infrastructure to promote tourism - erosion doubled further south - Spurn head eroded and become a tidal island.