Deck 17a- Factors that impact on coastal recession Flashcards

1
Q

What 4 physical factors impact on rates of coastal recession?

A

Waves, lithology, geological microstructures and vegetation

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2
Q

How do microstructures impact on coastal morphology?

A

Microstructures form a weakness in the bedrock that erosional processes focus on meaning erosional features such as caves and cave cut are more likely to form

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3
Q

What are 5 geological microstructures?

A

Bedding planes, faults, folds, joints and angle of dip

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4
Q

What is a bedding plane?

A

Beds are the layers of sedimentary rocks that are distinctly different from overlying and underlying subsequent beds of different sedimentary rocks. The line between the different beds is a bedding plane.

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5
Q

How do bedding planes impact on coastal morphology?

A

Bedding planes are a line of weakness for erosional processes

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6
Q

What is a joint?

A

A joint is a fracture dividing rock into two sections that moved away from each other either during tectonic uplift or the contraction of sediments as they dry up.

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7
Q

Which processes are joints particularly susceptible to?

A

Weathering processes such as freeze thaw weathering as the elements can impact the joints from above the waves.

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8
Q

What is a fault?

A

A fault is a fracture between two blocks of rock where there has been displacement. Fault occur when rocks are subjected to high levels of stress and pressure, for example during tectonic activity.

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9
Q

How do faults impact on morphology and rates of recession?

A

Faults are a line of weakness in a rock. If the rocks along a coastline are heavily faulted rates of coastal recession will be higher.

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10
Q

What is a fold?

A

A fold is where the rock has bent or curved during tectonic activity.

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11
Q

How do folds impact on coastal morphology and rates of recession?

A

Folds lead to a irregular occurrence of rocks and bedding planes at the surface which can lead to a variation in the amount of erosion taking place.

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12
Q

What does the angle of dip refer to?

A

Dip is the angle that layers of rocks lie e.g. horizontal, vertical or dipping towards or away from the sea.

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13
Q

How does the angle of dip impact on coastal morphology?

A

Depending on the dip direction and angle different layers of rock will be exposed to the sea and will lead to different rates of erosion. It is an important control on the shape of cliff profiles.

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14
Q

What is a cliff profile?

A

A cliff profile is the height and angle of a cliff plus any features it includes.

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15
Q

What 3 factors influence the shape of a cliff profile?

A

-The resistance to erosion of the rock (lithology)

-Weaknesses in the bedrock through geological structures

-The dip of rock strata in relation to the coastline

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16
Q

What characteristics does a cliff profile with a horizontal dip have?

A

-Cliffs have a vertical or near vertical profiles

-Wave cut notches form in the weaker layers of rock as they are less resistant to erosion, particularly if they are located near the base of the cliff where the wave action is more concentrated

17
Q

What characteristics does a cliff profile with a steep sea-ward dip have?

A

-Cliff is sloped with a gentler angle

-Susceptible to land slides as the layers of rock dip towards the sea

-Layer facing the sea is vulnerable to land slides particularly if the layer beneath is weaker or along a bedding plane

-At the base of the cliffs there is often a pile of weathered material

18
Q

What characteristics does a cliff profile with a gentle sea-ward dip have?

A

-Profiles may exceed 90° producing areas of overhanging rock

-Very vulnerable to rock falls as overhangs are likely to form

-If an overhang forms then the weight of the overlying rocks will eventually lead to a collapse of the cliff

-There is often a large pile of rock debris at the base of the cliff

19
Q

What characteristics does a cliff profile with a landward dip have?

A

-Steep profiles often at angles of 70-80°

-Produce very stable cliff profiles with a smaller chance of rock falls

-It is harder to produce an overhang due to the layers dipping back towards the land

20
Q

What does lithology mean?

A

The type of rock present in an area.

21
Q

What is does mineral composition refer to?

A

The minerals which make up the rock

22
Q

What does hardness refer to? How can it be measured?

A

Hardness refer to how hard the rock is on the Mohs scale. This can be measured through the scratch test.

23
Q

Which types of rocks score highest on the Mohs scale?

A

Igneous and metamorphic rocks with a crystalline structure generally score higher, particularly those with a high concentration of quartz e.g. grantie

24
Q

What does solubility refer to?

A

Whether the rock is likely to dissolve in slightly acidic rainwater.

25
Q

Which type of rocks are more soluble?

A

Carbonate rocks that contain lots of fossils e.g. chalk/limestone

26
Q

What does permeability mean?

A

The ability of rocks to allow water to pass through them

27
Q

Which types of rocks are more permeable?

A

Sedimentary rocks such as sandstone

28
Q

How are waves created?

A

Waves are caused by the friction between wind and water, where energy is transferred from the wind to the water.

29
Q

What 3 factors impact on the strength of waves?

A

-Fetch (distance travelled over water)

-Wind speed

-Wind duration

30
Q

Why do waves break?

A

Waves are brought on shore by the wind. As the waves approach the shore friction slows the base of the wave causing the wave to steepen. This continues to happen until the wave topples over itself and surges up the beach as swash. Water from previous waves then return to the sea as backwash.

31
Q

What are the characteristics of a constructive wave?

A

Strong swash, weak backwash, low frequency (8-10 per minute), low amplitude (less that 1 metre). Associated with calmer conditions that allow for higher levels of deposition.

32
Q

What are the characteristics of a destructive wave?

A

Weak swash, strong backwash, high frequency (10-14 per minute), high amplitude (over 1 metre). Associated with stormier conditions resulting in higher levels of erosion.