Enquiry Question 2 Flashcards

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1
Q

How are waves created?

A

Friction between the wind and surface of the water generates circular movements of energy

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2
Q

What happens when the wave approaches the shore?

A

The bottom of the wave experiences friction with the sea bed, causing the bottom of the wave to slow down faster than the wave crest. Therefore the movement becomes eliptical. This causes the wave to break, creating breakers.

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3
Q

What impacts the strength of a wave?

A
  • Wind speed/ strength
  • The fetch
  • The duration of the wind
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4
Q

Fetch

A

Distance the wave travels in open water

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5
Q

Swell waves

A

Waves continue after wind stops, they have a long time to lose energy.

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6
Q

Characteristics of constructive waves

A
  • Have a long wavelength
  • Low frequency of waves: Every 6-8 mins
  • The swash is stronger than the backwash (surging waves)
  • Very little erosion caused by backwash
  • Causes a gradual build-up of sediment creating a flatter beach
  • Very low wave height
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7
Q

Surging waves

A

The swash is stronger than the backwash

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8
Q

Characteristics of destructive waves

A
  • Shorter wavelength
  • More frequent waves: 10-15 mins
  • Backwash stronger than swash
  • Very little deposition; more erosion
  • Much steeper beach profile
  • Sand removed from the beach is deposited offshore creating an offshore bar
  • High wave height
  • High energy environment
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9
Q

Sediment profile:

A

The pattern of distribution of different sized or shaped deposited material

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10
Q

Formation of an Offshore bar:

A

Destructive waves, backwash removes sediment off the beach.
As the backwash loses energy, deposition occurs in the offshore/nearshore region
Once the ridge exists, it creates more friction with backwash, leading to more deposition and therefore larger offshore bars.

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11
Q

Swash aligned beach

A

When beaches/ coastlines are sheltered means waves run parallel to the beach and are swash aligned

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12
Q

Ridges

A

Areas of the foreshore that are raised

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13
Q

Runnels

A

A shallow trough in the foreshore

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14
Q

Berms

A

Shingle ridges formed beneath the storm beach

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15
Q

Storm Beach

A

Very coarse sediment deposited here during severe storms

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16
Q

Long-shore Bars

A

A shore parallel bar separated from the beach by a deep trough

17
Q

Cusp

A

Crescent shaped indentations that form on beaches of mixed sand and shingle

18
Q

Drift-aligned beaches

A

Beaches affected by longshore drift. Swash is aligned to the direction of prevailing wind

19
Q

Features of Drift-aligned beaches

A
  • Narrower beaches
  • More susceptible to erosion
  • Zig-zag shape - especially with human intervention (i.e groynes)
  • Sediment is deposited at an angle