Deck 16- Impact of geology on the coastline Flashcards

1
Q

What are igneous rocks?

A

Igneous rocks form from magma that cools and crystalises as it rises towards the surface, for example during volcanic eruptions

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2
Q

What are sedimentary rocks?

A

Sedimentary rocks are formed when other rocks are broken down into pieces and are deposited into layers. Over time the layers become compacted and cemented forming a solid rock

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3
Q

What are metamorphic rocks?

A

Metamorphic rocks form when rocks are buried at high pressures and temperatures which causes them to recrystalise

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4
Q

Which two types of rocks are generally more resistant to erosion?

A

Igneous and metamorphic rocks are more resistant to erosion due to their crystalline structure.

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5
Q

Why are sedimentary rocks less resistant to erosion?

A

They are tiny lines of weaknesses due how they form in layers, which make a focal point for erosional processes

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6
Q

State three examples of igneous rocks.

A

Granite, basalt, pumice

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7
Q

State three examples of metamorphic rocks.

A

Slate, schist, quartzite

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8
Q

State three examples of sedimentary rocks.

A

Sandstone, limestone, chalk

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9
Q

What is a discordant coastline?

A

A discordant coastline is where the type of rock runs perpendicular (at a right angle) to the coastline.

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10
Q

What is a concordant coastline?

A

A concordant coastline is where the type of rock runs parallel to the coast. The limestone at forms a concordant coastline on the south Dorset coastline.

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11
Q

What is an example of an area that has both discordant and concordant coastlines?

A

Swanage, Dorset

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12
Q

What sort of landforms form along a discordant coastline?

A

The series of headland and bays made by alternating bands of rocks is characteristic of a discordant coastline.

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13
Q

How do headlands and bays form at discordant coastlines?

Stretch: Include the specific names of locations and rock types at Swanage Bay

A

The less resistant bands of rocks (e.g. mudstones in Swanage Bay) erode at a faster rate than the more resistant rocks on either side (e.g. chalk at Ballard Point and limestone Durlston Head) leading to the formation of headlands and bays.

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14
Q

What is wave refraction and how does it influence the formation of headlands and bays?

A

Wave refraction is the bending of waves as they approach an uneven coastline, causing the wave energy to concentrate on protruding headlands and disperse in the recessed bays, leading to increased erosion at headlands and deposition in bays, thus shaping the coastline into a pattern of headlands and bays.

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15
Q

What landforms are characteristic of a concordant coastline?

A

Concordant coastlines are usually rocky coastlines that become a focus for erosion and form features such as wave cut platforms, caves, arches, stacks and stumps.

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16
Q

How can a headland and bay form at a concordant coastline?

Stretch: Include an example of where this has happened and the rock types present here.

A

At Lulworth Cove the sea has broken through the limestone due to a pre-existing weakness in the rock.

Once the sea had eroded past the limestone it was much easier to erode the poorly consolidated mudstone so this eroded much faster than the remaining limestone forming a wide cove with a narrow breach.

When the sea reached the consolidated chalk the rate of erosion slowed as the chalk is more resistant than the mudstone. The cove is becoming wider as the sea continues to erode the mudstone at the fastest rate.

17
Q

What is a Dalmatian coastline?

A

Dalmatian coastlines are a specific type of concordant coastline that form when some parts of landscapes are flooded due to sea level rise. Prior to the sea level rising there would have been a series of ridges and valleys running parallel to each other. As the sea level rose the valleys were flooded leaving the ridges remaining above the water.

18
Q

State an example where a Dalmatian coastline has formed.

A

Croatia

19
Q

What is a Haff coastline?

A

Haff type coastlines are a type of concordant coastline. They are a depositional concordant coastline where unconsolidated sediment e.g. sand and shingle have been deposited in structures parallel to the coastline. The sediment has been reworked by waves since it was deposited by meltwaters at the end of the Last Glacial Maximum,.

20
Q

State an example of a Haff coastline.

A

Frisian Islands in the North Sea, Netherlands/Germany and Vistula Lagoon in the Baltic Sea, Poland