Coastal Landscapes and Processes Flashcards

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1
Q

What are the three types of weathering?

A

Mechanical, chemical and biological weathering.

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2
Q

What is mechanical weathering?

A

Freeze-thaw weathering, a type of mechanical weathering, occurs when water gets into cracks in rocks. When the temperature falls below freezing, the water will expand as it turns into ice. The expansion puts pressure on the rock around it and fragments of the rock may break off. This type of weathering is common in highland areas where the temperature is below freezing in the night.

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3
Q

What is chemical weathering?

A

Rainwater contains weak acids that can react with certain rocks. Carbonates in limestone are dissolved by these weak acids and this causes the rock to break up or disintegrate. This can be seen on limestone statues and pavements.

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4
Q

What is biological weathering?

A

This is the action of plants and animals on the land.

Seeds that fall into cracks in rocks will grow in the presence of moisture, and breaking up the rocks as they grow.

Burrowing animals like rabbits can further break up rocks by making tunnels.

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5
Q

What is mass movement?

A

When material moves down a slope due to the pull of gravity.

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6
Q

Where is mass movement common in coasts?

A

Clay cliffs - in dry weather the clay contracts and forms cracks and when it rains water gets into these cracks, weakening the rock until, due to the pull of gravity, they fall off.

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7
Q

What are the four processes of coastal erosion?

A

Abrasion, hydraulic action, solution and attrition.

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8
Q

What is abrasion?

A

Where sand and pebbles carried within waves are thrown against the cliff face with force, and particles break off of the rock face as a result, which are in turn used to repeat the process.

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9
Q

What is hydraulic action?

A

This is the pressure of the water being thrown against the cliff by the wave. It also includes the compression of air in the cracks, as water gets into the cracks, it puts a large amount of pressure on the rock, causing pieces of rock to break off under the pressure.

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10
Q

What is solution?

A

This is a chemical reaction between rocks and the salt and other acids in the water. This is evident on limestone cliffs, where the water is milky blue due to the dissolved lime.

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11
Q

What is attrition?

A

This process involves wearing away rocks that are at sea. As the boulders in the sea continually roll around, they chip away at each other until smooth pebbles or sand are formed.

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12
Q

What are the four ways that the sea transports materials?

A

Traction, saltation, suspension and solution.

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13
Q

What is traction?

A

This is where large sediment such as pebbles roll long the sea bed.

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14
Q

What is saltation?

A

Where small pieces of shingle or large grains of sand are bounced along the sea bed.

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15
Q

What is suspension?

A

Where small particles like sand and clay are carried in the water; this can make the water cloudy, especially during storms or when the sea has a lot of energy.

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16
Q

What is solution? (In the context of transport)

A

Where minerals are dissolved in sea water and carried by the sea water.

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17
Q

What is the process of longshore drift?

A

The movement of sand and pebbles down a coastline. The direction of the waves hitting the coastline is determined by the prevailing wind. If the wind is blowing at an angle, the swash will approach at this angle, transporting the pebbles and sand with them. As the backwash is being pulled by gravity, it will find the shortest route down the beach. It always returns at 90 degrees relative to the coast.

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18
Q

What is deposition?

A

Deposition is laying down materials like sand and pebbles, which are being transported by the sea. The sea will deposit materials when it slows down and loses energy.

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19
Q

How does a rock’s structure affect erosion rates?

A

Rocks that are well jointed or have many faults, such as limestone, will erode rapidly since the waves exploit these lines of weakness. Rocks that have fewer joints will be harder to erode, rocks like chalk have lines of weakness that allow the sea to erode them easily.

20
Q

What is a concordant coastline?

A

Concordant coastlines have rocks that lie parallel to the coastline. These have alternate layers of hard rock and soft rock, the hard rock will act as a barrier to the erosive power of the sea. If the sea erodes the hard rock, the soft rock behind it will quickly erode afterwards.

21
Q

What is a discordant coastline?

A

Discordant coastlines have bands of rock that lie at right angles to the coastline. If there are alternate layers of hard and soft rock, the soft rock will erode faster, forming bays, with the resistive rocks forming headlands.

22
Q

What is a destructive wave?

A

They are the most important agent in erosion and take sediment away from coastlines. The backwash is stronger than the swash and therefore it is able to carry sand and pebbles away from the shore. They break frequently and are normally found on steep beaches.

23
Q

What is a constructive wave?

A

They are responsible for deposition in coastal areas and landforms. The swash is more powerful than the backwash and therefore it deposits material. They break infrequently and are generally found on gently sloping beaches.

24
Q

What landforms do destructive waves create?

A

Headlands, bays, caves, arches, cliffs, stacks and wave-cut platforms.

25
Q

What is seasonality?

A

A pattern of change in the UK’s weather between spring, summer, autumn and winter.

26
Q

What is fetch?

A

The distance over which the wind blows over open water.

27
Q

What is the prevailing wind affecting the UK?

A

The prevailing wind comes from the South-West and from the gulf stream from across the Atlantic Ocean.

28
Q

What are dynamic landforms?

A

Landforms that are actively changing.

29
Q

How is a wave-cut platform formed?

A

The sea erodes and undercuts the cliff, forming a small cave, with time this overhang falls down and another cave forms, further in this time and the overhang falls off again, forming a platform just under the water level.

30
Q

How is a stump formed?

A

Firstly, the sea attacks the side of the headland, eroding it until cracks form. Over time these cracks widen to form a cave, and eventually it keeps eroding until an arch is formed. Eventually, due to the force of gravity, the overhang falls down leaving a stack on the other side of the headland. This also collapses under the force of gravity given time and then forms a stump, disconnected from the rest of the headland.

31
Q

What is a spit?

A

A long, narrow stretch of pebbles and sand that is attached to the shore at one end. It forms when longshore drift occurs on a coastline and a large amount of material is deposited in one area for a long period of time.

32
Q

What is a bar?

A

If a spit develops in a bay, it may build across it, linking two headlands to form a bar. This is only possible if there is a gently sloping beach and no powerful river entering the sea. Hence special salt concentration conditions may form in a lagoon behind the bar.

33
Q

What is hard engineering?

A

A method of coastal management involving major construction work, like sea walls which work against the landscape.

34
Q

What is soft engineering?

A

A method of coastal management attempting to work with the landscape, this typically tends to be visually unobtrusive and does not involve major construction work.

35
Q

What are the advantages of sea walls?

A

-They are effective for many years.
-They are very visible and make residents feel safe.
-They reflect and absorb wave energy.

36
Q

What are the disadvantages of sea walls?

A

-They are very costly to build and maintain.
-They can be ugly and put off tourists.
-They can stop the natural processes occuring.
-They can cause wave scouring if not positioned correctly.

37
Q

What are the advantages of groynes?

A

-They are effective for many years.
-They keep the beach in place for tourists.

38
Q

What are the disadvantages of groynes?

A

-They are ugly, perhaps not encouraging tourism.
-It makes walking along beaches difficult.
-They prevent natural processes from occuring, building up certain areas with sand.
-They cost a lot - Β£400 for 1 metre of 1 metre high groyne.

39
Q

What are the advantages of rip-rap?

A

-They can be effective for many years.
-They dissipate wave energy.
-They can be cheap depending on rock type used.

40
Q

What are the disadvantages of rip-rap?

A

They can make a beach inaccessible for tourists.
-They aren’t effective during storms.
-They are not visually appealing.

41
Q

What are the advantages of beach nourishment?

A

-It is cheap - Β£6500 per 100 metres.
-It provides the beach in the same conditions - tourism.
-The beach’s natural processes aren’t interrupted.
-It can be a good use of sand.

42
Q

What are the disadvantages of beach nourishment?

A

-Lorries depositing sand disrupt home owners.
-Requires constant maintenance.
-May affect plant and animal life in the area.

43
Q

What are the advantages of offshore reefs?

A

-The waves break further offshore, reducing erosive power.
-They allow the build up of sand due to reduction in wave energy.

44
Q

What are the disadvantages of offshore reefs?

A

-They are expensive - Β£1950 per metre.
-They are difficult to install.
-They may be removed by heavy storms.
-They are less visually appealing.
-They may disrupt natural processes.

45
Q
A