Geology And The Coast Flashcards

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1
Q

What is coastal morphology?

A

The shape and form of coastal landscapes and their features.

Relates to the underlying geology, rock type and the geological structure.

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2
Q

What is lithology?

A

The physical characteristics of particular rocks.

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3
Q

What are the characteristics in lithology?

A
Strata 
Bedding planes 
Joints 
Folds 
Faults 
Dip
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4
Q

What are strata?

A

Layers of rock

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5
Q

What are bedding planes?

A

Horizontal cracks - natural breaks in the strata, caused by gaps in time during periods of rock formation.

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6
Q

What are joints?

A

Vertical cracks - these are fractures, caused either by contraction as sediments dry out, or by earth movements during uplift.

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7
Q

What are folds?

A

Formed by pressure during tectonic activity, which makes rocks buckle and crumple (e.g. Lulworth Crumple)

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8
Q

What are faults?

A

Formed when the stress or pressure to which a rock is subjected, exceeds its internal strength (causing it to fracture).

The faults then slip or move along fault planes.

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9
Q

What does dip mean?

A

Refers to the angle at which rock strata lie (horizontally, vertically, dipping towards the sea, or inland).

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10
Q

What does the relief mean?

A

Height and slope of land - also affected by geology and geological structure

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11
Q

What does geology and lithology affect?

A

The speed at which a coast erodes/recedes.

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12
Q

What are different types of rock?

A

Igneous
Sedimentary
Metamorphic
Unconsolidated

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13
Q

What are igneous rocks?

A

Granite - crystalline, resistant and impermeable

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14
Q

What are sedimentary rocks?

A

Limestone, chalk, sandstone and shale.

Formed in strata.
Jointed sedimentary rocks (sandstone and limestone) are permeable.
Other sedimentary rocks (chalk) have air spaces between the particles - making them porous.
Shale is fine grained and compacted - making it impermeable

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15
Q

What are metamorphic rocks?

A

Marble - very hard, impermeable and resistant

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16
Q

What are unconsolidated materials?

A

Loose, such as the boulder clay of Holderness.

They are not cemented together in any way and are easily eroded.

17
Q

What affects the rate of erosion or recession?

A

Geology
Lithology
Weathering
Mass movement

18
Q

What are concordant coasts?

A

This is where bands of more-resistant and less-resistant rock run parallel to the coast

19
Q

What are Dalmatian coasts?

A

A type of concordant coastline.

They have formed as a result of a rise in sea level. Valleys and ridges run parallel to each other.
When the valleys flooded because of sea level rise, the tops of the ridges remained above the surface of the sea - as a series of offshore islands that run parallel to the coast.

20
Q

What are haff coasts?

A

Also consist of concordant features - long spits of sand and lagoons - aligned parallel to the coast.

21
Q

What are disconcordant coasts?

A

The geology alternates between bands of more-resistant and less-resistant rock, which run at right angles to the coast.

22
Q

What are headlands and bays?

A

Headlands jut out into the sea, and bays lye between them

23
Q

How do headlands and bays form?

A

When rocks of different strengths are exposed at the coast.

More resistant rocks, such as chalk and limestone tend to form headlands, whilst weaker rocks, such as shale and clays, are eroded to form bays.

24
Q

How do headlands and bays affect incoming waves?

A

Headlands - force the incoming waves to refract or bend - concentrating their energy at the headlands.
This increases the waves erosive power, which leads to a steepening of the cliffs and their eventual erosion into arches and stacks

When waves enter a bay, their energy is dissipated (spread out) and reduced. This leads to the deposition of sediment (sand or shingle) - forming a beach

25
Q

What increases a waves erosive power at headlands?

A

The depth of the water decreases…
This causes the waves to get higher and steeper.
Their velocity also reduces
They become closer together

26
Q

What decreases a waves erosive power at bays?

A

Water is deeper.
So they don’t lose their velocity as rapidly.
Lower and less steep than those off the headland.
This allows for deposition rather than erosion