2B.1 Flashcards

1
Q

Define littoral zone

A

An area of coastline which has all sediment processes occurring sources, transport and sinks. A littoral cell is not a closed system

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2
Q

What does the littoral zone consist of

A

backshore, nearshore, offshore zones and includes a wide variety of coastal types - it is a dynamic zone of rapid change
OKAY NOW FRY BACON (SEA - OFFSHORE, NEARSHORE, FORESHORE BACKSHORE)

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3
Q

What is the backshore

A
  • The upper beach closest to the land, including any cliffs or sand dunes.
  • essentially from the mean high tide water mark up to a change in physiography (sand dune or cliff)
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4
Q

What is the foreshore

A

The lower part of the beach covered twice a day at high tide (the part of the beach that receives the most regular wave action).
- it includes the swash zone

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5
Q

What is the nearshore

A
  • area from the mean low tide mark to beyond where waves break (hence called the breaker zone)
  • this part of the sea is not exposed unless there is low tide unlike the foreshore which is exposed at both high and low tide
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6
Q

What is the offshore zone

A
  • open sea
  • further seaward than nearshore
  • The area of deeper water beyond the point at which waves begin to break. Friction between the waves and the sea bed may cause some distortion of the wave shape.
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7
Q

What is wave breaking

A

Waves break, but vary between high and low tide points

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8
Q

What is a wave

A
  • Initially in open water, as energy transferred from air to water
  • Shelving increases friction and wave breaks
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9
Q

What do rocky coasts result from and why?

A

Rocky coasts (high and low relief) result from resistant geology
WHY …
withstands erosive forces of sea, rain and wind, often in a
high-energy environment

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10
Q

What is resistance of a rock dependent on?

A

1) is rock clastic or crystalline?
2) how many cracks, fractures and fissures?
3) lithology of a rock

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11
Q

Why does clastic/crystalline factors matter to rock resistance

A
  • sedimentary rocks like sandstone are clastic as they
    are made up of cemented sediment particles, therefore are vulnerable to erosion,
  • igneous and metamorphic rocks are made up of interlocking crystals, making them more
    resistant to erosion
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12
Q

why does the amount of fissures, cracks and fractures affect resistance of geology?

A

the more weaknesses there are in the rock
the more open it is to erosional processes, especially Hydraulic Action

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13
Q

Igneous; State examples, rate of erosion

A

examples: granite, basalt
ROE: v slow, less than 0.1 cm a year

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14
Q

SEDI; State examples, rate of erosion

A

example is limestone
ROE = very fast, 0.5-10 cm year

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15
Q

metamorphic ; State examples, rate of erosion

A

examples: slate, schist, marble
ROE = slow, 0.1-0.3 cm a year

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16
Q

Why does age of rock affect its resistance to erosion

A
  • Ancient limestones have been compressed and compacted over millions of years = more resistant
  • Recently erupted volcanic lava flows and tephra deposits tend to be weaker and easily eroded = less resistant
17
Q

How does permeability affect resistance to erosion

A
  • Permeability is important as groundwater flow can weaken rocks by exploit joint structures and binding materials.
  • It can also create high pore water pressures within cliffs reducing stability
18
Q

State examples of permeable and impermeable rock

A

Permeable rocks include sandstones and limestones
Impermeable rocks includes clays, mudstones and most igneous and metamorphic rocks

19
Q

Describe unconsolidated material and how it is affected by erosion

A
  • unconsolidated coastal material is the weakest and most easily eroded (due to lack of strength and subsequent exploitation by water).
  • They tend to slump when saturated.
  • consider if there are reactive Minerals in the rock (e.g. Calcite) – solution.
20
Q

Define differential erosion

A

The selective erosion of areas of weaknesses