Coasts, 10 Flashcards

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1
Q

Destructive waves

A
  • they are created in storm conditions.
  • they are also created from big , strong waves when the wind is powerful.
  • they occurs when wave energy is high and the wave has travelled over a long fetch
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1
Q

Swash of the wave

A

Swash goes up at the angle of the wind ( on the direction of the wind ).

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2
Q

Wave

A

A wave is a body of water moving towards a coastline at higher than average level.

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3
Q

Backwash of the wave

A

The backwash is always at right angles to the sea.

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4
Q

Constructive waves

A
  • they are created in calm weather and are less powerful than destructive waves.
  • they break on the share and deposit material, building up reaches.
  • they have a Swash that is stronger than the backwash.
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5
Q

Formation of wave cut platform

A
  1. Erosion occurs at high water / high tide.
  2. The processes of erosion must be mentioned ie. Corrasion, solution and hydraulic action.
  3. Undercutting occurs.
  4. A wave cut notch is formed at the base of the cliff.
  5. The resulting overhang collapses and the cliff.
  6. A large area of flat rock is left at the base of the new cliff line. This is the wave-cut platform.
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6
Q

Caves, Arches and stacks

A
  1. CRACK
    a large crack is enlarged by the pressure on / off effect of hydraulic action.
  2. NOTCH
    the crack grows into a notch and then a cave as destructive waves coverage on the headland and continue to erode it.
  3. CAVE
    over time, the cave becomes larger. Wave refraction draws waves to all sides of the headland so caves may form back-to-back.
  4. ARCH
    the sea breaks through the back of the cave forming a natural arch is widened as notches form.
  5. HEAVY TOP OF THE ARCH
    weathering such as freeze-throw continues to weaken the top of the arch, making it
    less stable.
  6. ROCKS FELL
    top of the arch eventually collapses.
  7. STACK
    this leaves a pillar of detached rock called a stock.
  8. STACK STARTS TO FALL
    notches from at the base of the stack, which eventually makes it unstable.
  9. STUMP
    the stack will eventually topple into the sea, leaving only its base. This stump is normally only visible at low tide.
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7
Q

Transportation and LSD( long shore drift ),
Solution

A

Solution = dissolved chemicals ( often derived from chalk or limestone) in sea water and carried in solution. The load is not visible.

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8
Q

Transportation and LSD( long shore drift), suspension

A

Suspension = small particles are carried (suspended) in water, eg slits and clays, which can make the water look cloudy.

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9
Q

Transportation and LSD( long shore drift ), saltation

A

Saltation = load is bouncing or hopping along the sea bed, eg small pieces of shingle or large sand grains. Particles which are too heavy to be suspended.

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10
Q

Transportation and LSD( long shore drift ), traction

A

Traction = pebbles and larger sediment are rolled along the sea bed.

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11
Q

Long shore drift

A

Long shore drift = transport of sediment along a stretch of coastline caused by waves approaching the beach at an angle.

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12
Q

The land forms, types (3)

A
  1. Beaches
  2. Splits
  3. Bars
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13
Q

Coastal deposition.
Deposition is likely to occur when:

A
  • waves enter an area of shallow water.
  • waves enter a shelter area, eg a cove or bay, where low energy means constructive waves are dominant.
  • there is little wind.
  • wide expanse of flat beach, so swash spreads out, weaking the wave, so backwash is weak.
  • there is a good supply of material from up drift erosion.
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14
Q

Beach

A

A beach is the gently sloping area of land between the right and low water marks.

Beaches ARE NOT permanent features as their shapes are alternated by waves.

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15
Q

Split

A

A split is a narrow coastal land formation that is tied to the coast at one end

16
Q

Formation of Bar

A

Because of wind creates long shore drift and sand bank is carrying on the beach. At the end of it, it starts deposition and split forms. Split joins with headlands and creating the bar behaving and it creates lagoon.

17
Q

Formation of Tombolo

A

Tombolos are formed where a split continues to grow outwards joining land to an offshore island to be located in the path of the land of the long shore drift for the split to latch onto as it grows.
Tombolos, like all deposition features can be removed during large storm but are often permanent and used.

18
Q

Location of Dune

A

Essential conditions, large flat beach, large supply of sand, onshore wind, large tidal range and an obstacle such as drift wood.

18
Q

Similarities and differences between the bars and splits.

A

Similarities: they creating in the same way( long shore drift)
Differences: bars going to lagoon, split goes to the sea.

19
Q

Sand dunes

A

Sand dunes are often found at the back of a beach. However, they need very specific contact to form and are therefore not uniformly seen

20
Q

Sand movement

A

Sand movement = the sand used to create dunes is transported to the back of the beach by the wind in 3 main ways, creep, saltation, suspension

21
Q

Formation of dune

A
  1. At the back of the beach is an obstacle such as drift wood.
  2. Heaviest grains settle against the obstacle, lighter ones settle on other side of obstacle.
  3. Side facing the wind begins to form a crest.
  4. This is because the pile of sand become too steep to build ups and falls under its own weight .
  5. Sand stops slipping when slope reaches a gradient of 30-34 degrees.
  6. Repeated movement of material up windward side and down leeward side causes dunes to migrate inland.
  7. Sand dune its self becomes and obstacle and other dunes from in front of it.
22
Q

Concordant

A

Concordant = where bands of different rock type run parallel to the coastline.

23
Q

Discordant

A

Discordant = layers of rock at right angles to the coast.

24
Q

Hard engineering

A

Hard engineering = building artificial structures aimed at controlling natural process.

25
Q

Hard engineering, gabions

A

What is it?
A wall of wire cages filled with rocks, usually built at the foot of cliffs.

Benefits
Gabions absorb wave energy and so reduce erosion. They’re cheap and easy to build.

Costs
They’re ugly to look at and the wire cages can corrode over time.

25
Q

Hard engineering, sea wall

A

What is it?
A wall made out of a hard material like concrete that reflects waves back to sea.

Benefits
It prevents erosion of the coast. It also acts as a barrier to prevent flooding.

Costs
It creates a strong backwash that erodes under the wall. Expensive to build and maintain

25
Q

Soft engineering

A

Soft engineering = a sustainable approach to managing the coast without using artificial structures.

25
Q

Hard engineering, groynes

A

What is it?
Wooden or stone fences that are built at right angles to the coast. They trap material transported by long shore drift.

Benefits
They create winder beaches which slow the waves. This gives greater protection from flooding and erosion. They’re a fairly cheap defence.

Costs
They starve beaches further down the coast of sand, making them narrower. Narrow beaches don’t protect the coast as well, leading to greater erosion.

25
Q

Soft engineering, beach nourishment and reprofiling

A

What is it?
Sand and shingle from elsewhere (e.g. from the seabed) or from lower down the beach that’s added to the upper part of beaches.

Benefits
It creates wider beaches which slow the waves. This gives greater protection from flooding and erosion.

Costs
Taking material from the seabed can kill organisms like sponges and corals. It’s a very expensive defence. It has to be repeated.

25
Q

Hard engineering, rock armour

A

What is it?
Boulders that are piled up along the coast

Benefits
It absorb wave energy, reducing erosion and flooding. It’s a fairy cheap defence.

Costs
Boulders can be moved around by strong waves, so they need to be replaced.

26
Q

Soft engineering, dune regeneration

A

What is it?
Creating or restoring sand dunes by nourishment, or by planting vegetation to stabilise the sand

Benefits
Dunes create a barrier between land and sea and absorb wave energy, preventing flooding and erosion. Stabilisation is cheap.

Costs
The protection is limited to small area. Nourishment is very expensive.

27
Q

Mass movement

A

Mass movement = is the shifting of rock sand loose material down a slope, eg a cliff. It happens when force of gravity acting on a slope is greater then the force supporting it.

28
Q
A
29
Q
A