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
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
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
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
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
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.
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.
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
9
Q
Attrition
A
as rocks are moved around by the water, they knock into each other gradually becoming smaller and rounder
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
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
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.
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
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