2.4 - Erosion And Waves Flashcards

1
Q

Factors affecting the size of waves

A
  • Strength of the wind
  • Duration the wind is blowing
  • Water depth
  • Fetch
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2
Q

How do waves form and break

A
  • Waves start out at sea and have a circular orbit
  • As waves approach the shore friction slows the base of the wave
  • Causing the orbit to become elliptical
  • Until the top of the wave breaks over
  • Waves break in shallow water because the crest of the wave begins to move forward much faster than the wave trough
  • The trough experiences friction with the sea floor causing it to slow
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3
Q

Constructive waves

A
  • Low energy
  • Low flat wave height (under 1m)
  • Long wave length (up to 100m)
  • Low wave frequency
  • Strong swash that pushes sediment up the beach, but a weaker backwash that is unable to transport all particles back down so they are deposited as a berm at the top of the beach
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4
Q

Destructive waves

A
  • High energy
  • Large wave height
  • Short wave length
  • High wave frequency
  • Strong backwash and weak swash due to steep angle of impact
  • Strong backwash erodes material from the top of the beach carrying it down the beach to the offshore zone
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5
Q

How do waves influence beach morphology

A
  • Destructive, high-energy waves dominate in the winter, lowering angle of beach profile and spreading shingle over the whole beach. Offshore ridges/bars formed by destructive wave erosion and subsequent deposition of sand and shingle offshore.
  • In summer, constructive, low-energy waves dominate, steepening beach angle and sorting particles by size, with larger shingle particles towards back of beach. In summer, constructive waves build berm ridges, typically of gravel/shingle at high tide mark
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6
Q

What is erosion

A

Erosion refers to the wearing away of the land surface and removal of materials by river and seawater, ice and wind.

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7
Q

Hydraulic action

A
  • this is the shear force of the waves forcing air at high pressure into cracks in the cliff over time this weakens the rock and causes the joint to widen
  • High energy waves with a large wave height are the most effective at erosion through hydraulic action.
  • It is also accentuated when there is no debris at the cliff foot to absorb some of the wave energy and protect the cliff base.
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8
Q

Abrasion

A
  • Abrasion is where a wave picks up sediment and throws these load items against a rock
  • The repeated impact chips away at the rock face until small fragments break away
  • High-energy destructive waves with a large wave height are most effective as they hurl load items with greater force, resulting in faster rates of erosion by abrasion
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9
Q

Attrition

A

as rocks are moved around by the water, they knock into each other gradually becoming smaller and rounder

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10
Q

Solution/corrosion

A
  • weak acids in seawater dissolve the rock particles
  • Minerals are immediately carried away by the wave in solution
  • They are also vulnerable to erosion by rainwater and sea spray
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11
Q

Factors affecting the rate of erosion

A
  • Wave type: The size and type of waves affects the amount of hydraulic action and abrasion
  • Wave size: Erosion tends to happen more during the winter due to a greater number of destructive waves
  • Lithology: Weaknesses in rocks erode more quickly, more resistant rocks erode more slowly
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12
Q

Wave cut notch

A
  • A wave cut notch is a curved indentation of about 1-2 m high extending along the base of a cliff.
  • It forms between the high and low tide marks, where destructive waves impact against the cliff.
  • It’s eroded by hydraulic action and abrasion, and in some cases corrosion.
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13
Q

Wave cut platform

A
  • a flat rock surface exposed at low tide, extending out to sea from the base of a cliff.
  • Powerful destructive waves attack the base of the cliff at high tide
  • The hydraulic action and abrasion create a wave-cut notch which over time increases in size
  • This is called undercutting
  • Eventually, the overhang created by the undercutting collapses due to weathering and gravity
  • The cliff retreats, leaving a wave cut platform that is exposed at low tide
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14
Q

Crack, cave, arch, stack , stump

A
  • Wave refraction concentrates wave energy onto the headland and can contribute to the formation of caves, arches, stack and stumps
  • Cracks/joints in the headland are susceptible to erosion by hydraulic action
  • Over time the joints widen forming a cave that is enlarged by hydraulic action and abrasion
  • Eventually, erosion cuts through the headland forming an arch
  • The roof of the cave will eventually collapse due to gravity and the lack of support
  • This leaves a stack that will over time be eroded by weathering, abrasion, and hydraulic action to form a stump
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