Erosional landforms - P Flashcards

1
Q

What are erosional landforms

A

Landforms created by erosional processes

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2
Q

Define bay

A

a recessed, coastal body of water which is partially surrounded by land

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3
Q

Define headland

A

an area of usually more - resistant rock which extends into the sea, surrounded by water on 3 sides

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4
Q

define cliff

A

a steep, often m vertical or overhanging, face of rock

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5
Q

define shore platform

A

a flat or gently sloping rock surface found at the base of cliffs

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6
Q

Define geo

A

a narrow steep-sided inlet

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7
Q

Define blowhole

A

a vertical shaft between a cliff top and a cave, where spray from waves may burst out of during storm conditions

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8
Q

define cave

A

a natural opening in a cliff face, large enough for humans to explore

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9
Q

define arch

A

a wave - eroded passage through a small headland

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10
Q

define stack

A

a steep and often vertical column of rock in the sea

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11
Q

Define stump

A

a short, eroded remnant of a sea stack that juts above the sea surface

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12
Q

How to bays and headlines usually form

A

Adjacent to each other - usually due to the bands of rocks

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13
Q

What is a disconcordant coastline

A

when the rocks are perpendicular to the coastline so the weaker rocks are eroded to form bays while more resistant rocks remain as headlands

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14
Q

What is a concordant coastline

A

when rocks lie parallel to the coastline, more resistant rocks could protect softer rocks inland - usually a straight coastline.

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15
Q

What is the width and depth of bays determined by

A
  • width of band of weaker rocks
  • differential rates of erosion
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16
Q

What is wave refraction

A

is more significant where bays and headlands form

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17
Q

What is an orthogonals

A

imaginary lines, perpendicular to wave fronts, representing the transfer of energy as a wave moves towards the coast

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18
Q

Explain wave refraction

A
  • waves refract around the headland causing orthogonal to converge and wave energy too be focused on the headland
  • in bays the orthogonal diverge and the energy is dissipated leading to deposition
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19
Q

Can bays and headlands be formed on concordant coasts

A

Yes but usually they are small - e.g. Lulworth Cove, Dorset - the limestone has been eroded through the softer clays to form a cove

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20
Q

Why do cliff profiles vary

A

They depend on the geology

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21
Q

Which two types of cliffs have a near vertical profile

A
  • horizontally bedded strata
  • landward dipping strata
22
Q

Which type of cliffs has the profile following the angle of the strata

A
  • seaward dipping strata
23
Q

What causes the horizontally bedded strata to be near vertical

A

Undercutting leads to rockfall and rocks retreating inland parallel to the coast

24
Q

What causes the landward dipping strata to be near vertical

A

rocks are loosened by weathering and are difficult to dislodge so the profile is gradually lowered by weathering and mass movement

25
Q

What causes the seaward dipping strata to follow the angle of the dipping strata

A

Undercutting removes the basal support - rock layers loosened by weathering slide into the sea along the bedding plane

26
Q

Explain how a shore platform is formed

A
  • destructive waves cause undercutting between low and high tides, forming a wave cut notch
  • continued undercutting weakens support off rock above so it collapses
  • regular removal of debris means cliff retreats and is steep
  • as the process continues the cliff becomes higher
  • at the base a gently sloping shore platform is formed
27
Q

When is a shore platform exposed

A

during Low tide

28
Q

What process eroded shore platforms the most

A

abrasion as there is a lot of rock debris thats dragged across the surface by wave action

29
Q

What stops the undercutting of a cliff (shore platform)

A
  • as they become wider, friction slows approaching waves causing them to break before reaching the cliff
  • this slows down and eventually stops undercutting
30
Q

How wide does the shore platform have to be to stop undercutting of the shore platform

A

usually 500m away from the cliff

31
Q

What types of weathering are key process in the formation of a shore platform

A
  • solution, freeze thaw and salt crystallisation take place depending on rock type and climate
  • algae can accelerate weathering when exposed at low tide
  • algae makes water more acidic by releasing CO2 (chemical weathering)
32
Q

How do shore platforms usually slope

A

slope seawards between 0 and 3 degrees

33
Q

When is erosion concentrated in one location

A

during low and high tide

34
Q

What is formed due to concentrated erosion at the low water mark (LWM) and high water mark (HWM)

A
  • a ramp at the HWM
  • A small cliff at the low water mark
35
Q

When do cliffs and ramps form better

A

when the tidal range is less than 4m

36
Q

Why is a higher tidal range that 4m worse at forming ramps and cliffs

A

the erosion is spread over a larger area of the platform

37
Q

What are goes

A

narrow, steep sided inlets - occur even on coasts with resistant geology as there can be lines of weakness

38
Q

Explain how geos form

A
  • weak points are eroded more rapidly by wave action that the more resistant rock around them
  • this continues until a steep sided inlet is formed
39
Q

What is a key process in the formation of a geo

A

hydraulic action - as forcing air and water into the joins will weaken the rock strata

40
Q

What is an example of a geo

A

Huntsman’s Leap - Wales is 35m deep in Limestone

41
Q

How is a blowhole formed

A

when part of a tunnel-like cave collapses along a master joint, it may form a vertical shaft that reaches the cliff top

42
Q

what happens to a blowhole ion storm conditions

A

water may spray out of it in plumes of white aerated water

43
Q

What is unique about the size of blowholes

A

they are usually quite small but large in diameter

44
Q

What is an example of a blowhole

A

Trevone, Cornwall - 25m deep and 25m wide

45
Q

Where do a caves, arches, stacks and stumps tend to form

A
  • develop around headlands - and represent the erosional stages
46
Q

Explain how a cave is formed

A
  • due to wave refraction, energy is concentrated on the sides of headlands
  • points of weakness, such as faults or joints are then exploited by erosional processes
  • a small cave may develop one one side or even both
47
Q

Where do caves usually form

A

between high and low tide levels as wave attack is more concentrated here

48
Q

Explain how an arch is formed

A

if a cave enlarges to an extent that it extends through to the other side of the headland (possibly meeting another cave) an arch is formed

49
Q

Explain how a stack is formed

A

continued erosion widens the arch and weakens its support, weathering processes may cause the arch to collapse, leaving a stack isolated form the headland

50
Q

Explain how a stump is formed

A

further erosion at the base of the stack may eventually cause further collapse, leaving a small, flat portion of the original stack as a stump (may be only visible at low tide)

51
Q

What is an example of caves, arches, stacks and stumps

A

Old Harry Rocks, Isle of Purbeck