coasts - seneca Flashcards

1
Q

what is the littoral zone

A

series of sub zones from the sea to land. we consider it a closed system

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2
Q

what are the four sub-zones in the littoral zones

A

offshore (open sea)
foreshore (land where most wave processes occur
backshore (area above high tide level that is only affected during exceptionally high tides.)

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3
Q

how does a system reach dynamic equilibrium

A

input=output

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4
Q

inputs of the littoral zone

A

sediment brought by waves, current and wind

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5
Q

outputs of the littoral zone

A

sediment washed out to sea by erosion

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6
Q

what are high energy coasts

A

destructive waves, long fetches, high erosion rates, caves, arches, stacks and stumps, cliffs and wave cut platforms

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7
Q

what are low energy coasts

A

constructive waves, shorter fetches, high deposition rates, spits and bars, beaches, sand dunes and salt marshes

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8
Q

how ma sediment ells are there in england & wales?

A

11

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9
Q

what are the sources of sediment cells

A

where sediment comes from (cliffs, offshore bars)

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10
Q

what are the flows in a sediment cells

A

movement of sediment in LSD

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11
Q

what are the sinks in sediment cells

A

where sediment is deposited (spits, beaches)

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12
Q

what is a positive feedback loop

A

takes system away from dynamic equilibrium

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13
Q

what is a negative feedback loop

A

returning a system back to equilibrium

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14
Q

negative feedback loop - a storm increases input of sediment to beach

A
  • When the destructive waves from the storm lose their energy excess sediment is deposited
    as an offshore bar.
  • The bar dissipates the waves energy which protects the beach from further erosion.
  • Over time the bar gets eroded instead of the beach.
  • Once the bar has gone normal conditions ensue and the system goes back to dynamic
    equilibrium.
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15
Q

positive feedback loop - a storm increases input of sediment to beach

A

People walking over sand dunes destroys vegetation growing there and causes erosion.
- As the roots from the vegetation have been holding the sand dunes together, damaging the vegetation makes the sand dunes more susceptible to erosion. This increases the rate of
erosion.
- Eventually the sand dunes will be completely eroded leaving more of the beach open to
erosion taking the beach further away from dynamic equilibrium.

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16
Q

Valentine’s Classification

A

describes the range of coastlines that can occur
An advancing coastline may be due to the land emerging or deposition being the prominent
process. Alternatively, a coastline may be retreating due to the land submerging or erosion
becoming the prominent process.
Emergent or submergent coastlines may be due to post-glacial adjustment (the land ‘wobbles’ as
the glacier above it melts, causing isostatic sea level change), as well as other causes (discussed
later).

17
Q

concordant coast

A

parallel bands to coast