4.3 and 4.4 Flashcards

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1
Q

Concordant coastline rock type

A

Hard rock

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2
Q

Discordant coast rock type

A

Hard and soft rock

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3
Q

How do headlands form?

A

Headlands are formed when the sea attacks a section of coast with alternating bands of hard and soft rock.

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4
Q

Feature of a discordant coastline

A

Coastlines where the geology alternates between strata (or bands) of hard rock and soft rock are called discordant coastlines.

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5
Q

Features of a concordant coastline

A

A concordant coastline has the same type of rock along its length. Concordant coastlines tend to have fewer bays and headlands.

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6
Q

What is the difference between hard or soft rock?

A

The bands of soft rock, such as sand and clay, erode more quickly than those of more resistant rock, such as chalk.

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7
Q

What is a bay?

A

The areas where the soft rock has eroded away, next to the headland, are called bays.

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8
Q

How do wave cut platforms form?

A

Wave-cut platforms form when destructive waves hit against the cliff face, causing undercutting between the high and low water marks, mainly as a result of corrosion and hydraulic power, creating a wave-cut notch. This notch then enlarges into a cave.

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9
Q

How is an arch formed?

A

If the cave is formed in a headland, it may eventually break through to the other side forming an arch.

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10
Q

How does a cave form?

A

Caves occur when waves force their way into cracks in the cliff face. The water contains sand and other materials that grind away at the rock until the cracks become a cave. Hydraulic action is the predominant process.

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11
Q

How is a stump formed?

A

The arch will gradually become bigger until it can no longer support the top of the arch. When the arch collapses, it leaves the headland on one side and a stack (a tall column of rock) on the other.
The stack will be attacked at the base in the same way that a wave-cut notch is formed. This weakens the structure and it will eventually collapse to form a stump.

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12
Q

What three factors affect wave energy?

A

First, the wind speed must be blowing faster than the transfer of energy from wave crest to wave crest. The second factor is the amount of time the wind blows, or wind duration. The third factor is the fetch, the uninterrupted distance over the sea for which the wind blows without a change in direction.

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13
Q

What is a destructive wave?

A

A wave that has a weak swash and a strong backwash.

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14
Q

What is a constructive wave?

A

A wave that has a strong swash and a weak backwash.

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15
Q

What is abrasion?

A

the process of scraping or wearing something away.

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16
Q

What is hydraulic action?

A

When water gets pushed into cracks of rock that it splits the rock after a while.

17
Q

What is attrition?

A

Waves smash rocks and pebbles on the shore into each other, and they break and become smoother.

18
Q

What is solution?

A

Acids contained in sea water will dissolve some types of rock such as chalk or limestone.

19
Q

How do human activities have direct or indirect effect on the coast?

A

Human activities are often concentrated in coastal regions which are often least able to assimilate those activities, and where adverse effects are most apparent. Coastal zones are relatively fragile ecosystems, and disordered urbanisation and development of infrastructure, alone, or in combination with uncoordinated industrial, tourism-related, fishing and agricultural activities, can lead to rapid degradation of coastal habitats and resources. Mounting pressure on the coastal zone environment has, in several European countries, resulted in a rapid decline in open spaces and natural sites and a lack of space to accommodate coastal activities without significant harmful effects.

20
Q

Habitats

A

Humans can also affect animal habitats on coasts due to oil spills in the sea, over fishing and ocean acidification.

21
Q

What is the difference between traction, saltation, suspension and solution?

A

Solution - minerals are dissolved in the water and carried along in solution. Suspension - fine light material is carried along in the water. Saltation - small pebbles and stones are bounced along the river bed. Traction - large boulders and rocks are rolled along the river bed.

22
Q

How does longshore drift work?

A

Longshore drift. Waves that hit the beach at an angle carry sand and gravel up the beach face at an angle. When the water washes back the sediment is carried straight back down the beach face. Individual particles are moved along the beach in a zig zag pattern.

23
Q

How does a spit form?

A

Spits are also created by deposition. A spit is an extended stretch of beach material that projects out to sea and is joined to the mainland at one end. Spits are formed where the prevailing wind blows at an angle to the coastline, resulting in longshore drift.

24
Q

Characteristics of a spit

A

A spit is a stretch of sand or shingle extending from the mainland out to sea. They develop where there is a sudden change in the shape of the coastline such as at a headland. Normally, longshore drift transports beach sediment along a coastline.

25
Q

How do beaches form?

A

A beach forms when waves deposit sand and gravel along the shoreline. Some beaches are made of rocks and pebbles. Over time they are worn smooth from being rolled around by waves. The rocks usually reflect the local geology.

26
Q

Difference of spit to a bar

A

Both of these landforms are the result of longshore drift and deposition of material by the sea so there is a definite similarity in the processes of their formation and development. Spits and bars are long, narrow accumulations of sand and/or shingle. … A bar starts in a similar way, and to begin with, is a spit.