Yeet Flashcards

1
Q

Where are the uk’s main upland areas

A

North and West of the country

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2
Q

Where are the uk’s main lowland areas

A

South and East of the country

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3
Q

What are the three types of rock

A

Igneous
Sedimentary
Metamorphic

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4
Q

Igneous rocks formation

A

Formed when molten rock from the mantle cools and hardens
The rock forms crystals as it cools.
Usually hard (e.g granite)

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5
Q

Sedimentary rocks formation

A

Formed when layers of sediment are compacted together until they become solid rock

Two main types:

Carboniferous limestone and chalk
Clays and shales

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6
Q

How are Limestone and chalk formed

A

Tiny shells and dead skeletons of dead sea creatures.
Limestone is hard
Chalk is soft

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7
Q

How are clays and shales formed

A

Made from mud and clay minerals

Very soft

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8
Q

How are Metamorphic rocks formed

A

Formed when other rocks are changed by heat and pressure. The new rocks become harder and more compact

e.g shale becomes slate, then slate becomes schist

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9
Q

Characteristics of granite

A

Very resistant
Forms upland landscapes
Lots of joints (cracks)
Impermeable - doesn’t let water through

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10
Q

Characteristics of Slate and Schist

A

Forms in layers creating weak planes
Very hard and resistant
Schist has bigger crystals than slate
Form rugged, upland landscapes

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11
Q

Characteristics of chalk and clay

A

Chalk is harder than clay
Forms hills in the lowlands and cliffs at the coast
Chalk is usually permeable
Clay is very soft and easily eroded
Clay forms wide, flat valleys in lowlands
Clay is permeable

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12
Q

Characteristics of limestone

A

Rainwater weathers the limestone through carbonation weathering
Limestone is permeable

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13
Q

What physical processes alter the landscape

A

Weathering
Erosion
Post-glacial river processes
Slope processes

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14
Q

What is weathering

A

Breakdown of rock into smaller pieces

Mechanical
Biological
Chemical

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15
Q

What is erosion

A

Erosion wears away rock

Rivers and sea constantly erode landscapes

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16
Q

What are post-glacial river processes

A

Melting ice at the end of glacial periods made rivers much larger with more power to erode the landscape

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17
Q

What are slope processes

A

Includes mass movement -

Shifting of rocks and loose material down a slope

Three types of mass movement:
Slides - shifts in a straight line
Slumps - shifts with a rotation
Rockfalls - material breaks up and falls

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18
Q

Three ways humans have changed the landscape

A

Agriculture
Forestry
Settlement

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19
Q

How have humans changed the landscape through agriculture

A

Clearing land for farming

Walls mark out fields

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20
Q

How have humans changed the landscape through forestry

A

Management of areas of woodland
Very little natural woodland left
Trees planted in straight lines, not natural

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21
Q

How have humans changed the landscape through settlement

A

Land concreted
Rivers diverted
Rivers straightened

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22
Q

What is mechanical weathering

A

Breakdown of rocks without changing its chemical composition

Salt weathering:

1) seawater gets into cracks
2) water evaporates, forming salt crystals which expand, putting pressure on rock
3) causes rock to break up

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23
Q

What is chemical weathering

A

Breakdown of rock by changing its chemical composition

Carbonation weathering:

1) seawater and rainwater have carbon dioxide (weak carbonic acids)
2) They react with rock that contains calcium carbonate.
3) rocks are dissolved

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24
Q

What is biological weathering

A

Breakdown of rock by living things

e.g plant roots grow into cracks, pushing rock apart

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25
3 ways waves wear away the coast
Hydraulic action Abrasion Attrition
26
What is hydraulic action
Waves crash against rock and compress air in the cracks, putting pressure on the rock. This widens the cracks and makes bits break off
27
What is abrasion
Eroded particles in the water scrape and rub against rock, removing small pieces
28
What is attrition
Eroded particles in the water smash into each other and break into smaller fragments and get rounder
29
Concordant coastline
Alternating bands of hard and soft rock are parallel to the coastline Moving this way ------------>
30
Discordant coastline
Alternating bands of rock are perpendicular to the coast Moving upwards
31
What coastline are headlands and bays formed at
More common discordant coastlines because the bands of rock are being eroded at different rates
32
How is a headland and bay formed
Less resistant rock (e,g clay) is eroded quickly forming a bay More resistant rock (e,g chalk) is eroded more slowly and its left poking out, forming a headland
33
How are wave-cut platforms formed
Waves erode the foot of the cliff the most, forming a wave cut notch. The rock above becomes unstable and collapses The collapsed material is washed away and the new wave-cut notch forms Repeated, this forms a wave cut platform
34
How are headlands eroded to form caves, arches and stacks
Cracks are enlarged due to hydraulic action and abrasion. Enlargement causes the formation of a CAVE Continued erosion deepens the cave until it breaks through the headland, forming an ARCH Erosion continues to wear away the rock supporting the arch and it collapses forming a STACK
35
What is transportation
Transportation is the movement of material that has been eroded and deposited by waves
36
How is material transported around the coast
Waves follow the direction of the prevailing wind They usually hit the coast at an oblique angle The swash carries material up the beach in the same direction as the waves The back wash then carries material down the beach at right angles back towards the sea This repeats and the material travels along the coast
37
How do you constructive waves deposit material
Constructive waves are long, low, and have low frequency This watch is powerful and it carries material up the coast The backwash is weaker and doesn't take a lot of material back down the coast Constructive waves deposit materials such as sand and shingle along the coast to form beaches
38
How are spits formed
Spits form at sharp bends in the coastline Longshore drift transport sand and shingle past the bend and deposits at the sea Strong winds and waves can curve the end of the spit The sheltered area behind the spirit is protected from waves The sheltered area can become a mud flat or salt marsh
39
How are bars formed
A bar is formed when a split joins to headlands together The bar cuts off the bay between the headlines from the sea This means a lagoon can form behind the bar
40
What human activities have direct and indirect effects on the coast
Agriculture Development Industry Coastal management
41
What are direct effects
They are an immediate result of human activities for example building coastal defences will prevent erosion
42
What are indirect effects
Effects that happen as a result of the direct effects, for example building coastal defences will prevent erosion In one place but it can increase erosion further along the coast
43
How does agriculture affect the coast
Agricultural land has a low economic value which means it is often left and protected, leading to the sea eroding the cliffs and the land Changing the way farmland is used to can affect the stability of cliffs, for example vegetation helps bind the soil together Land such as marshland is sometimes reclaimed and drained for agricultural use, reducing the natural flood barrier that marshland provides
44
How does development affect of the coast
Coastal areas are popular places to live and work so there is lots of development Coast with lots of settlements have more coastal defences which is positive for the coastline There is a change in transportation and deposition along the coast because building On coast land restricts sediment supplier to beaches making them narrower and vunerable
45
How does industry affect the coast
Coastal quarry is expose large areas of rock making them vulnerable to chemical weathering and erosion Gravel has been extracted from some beaches for use in construction, increasing the risk of erosion Industrial growth at ports has led to increased pressure to build on saltmarshes restricting the natural flood barriers and leaving the land more vulnerable
46
How does coastal management have an affect on the coast
Coastal management such as sediment movement reduces the protection on the beach increasing erosion Coastal defences can reduce erosion, preventing the landscape from changing
47
How do you groins cause problems further along the coast
They cause narrow beaches the form further down the coast, increasing erosion down the coast
48
How is rising sea level increasing coastal flooding
Rising sea levels would cause higher tides that would flood coastal areas more frequently, removing larger amounts of material from beaches and erosion of cliffs
49
How is storm frequency increasing coastal flooding
Climate change is causing storms to be more frequent Storms give the sea more erosion of power, therefore areas of soft rock erode more quickly The sea will have more energy to transport material, leaving some areas being staffed and vulnerable to erosion Storm surges could become more frequent and sealevel rise could cause surges to reach areas further inland
50
Examples of hard engineering
Sea wall | Groynes
51
Examples of soft engineering
Beach replenishment Slope stabilisation Strategic realignment
52
What does hard engineering mean
Man-made structures built to control the flow of sea and reduce flooding and erosion
53
What does soft engineering mean
Schemes set up using knowledge of the sea and its processes to reduce the effects of flooding and erosion
54
Sea wall benefits and costs
Benefits include: It prevents erosion of the coasts and acts as a barrier to prevent flooding Costs include: It creates a strong backwash which arose under the wall. Seawalls are very expensive to build and to maintain
55
Groynes benefits and costs
Benefits include: They create wider beaches which slows the waves, giving greater protection from flooding and erosion Fairly cheap Costs include: they starve beaches further down the coast making them narrower Narrow beaches don't protect the coast as well leading to greater Rosian and floods
56
Beach replenishment benefits and costs
Benefits include: It creates wider beaches which slow the waves, giving greater protection from flooding and erosion Costs include: Taking material from the seabed can kill organisms It's a very expensive defence and has to be repeated
57
Slope stabilisation benefits and costs
Benefits include: It prevents mass movement by increasing the strength of the slope Cost include: very expensive and difficult to install
58
Strategic realignment benefits and costs
Overtime the land will become marshland-creating new habitats Flooding and erosion are reduced behind the marshland Costs include- People may disagree over what land is allowed to flood such as flooding farmland
59
Upper course of river
The gradient is steep V shaped Valley, steep sides, Narrow, shallow channel
60
Middle course of river
Medium gradient Gently sloping valley sides Wider deeper channel
61
Lower course of river
Gentle gradient Very wide, almost flat valley Very wide, deep channel
62
What is vertical erosion
Verticle erosion deepens the river valley making it the shaped. It is dominant in the upper course High turbulence causes the rough, angular particles to be scraped along the river bed causing more erosion
63
What is lateral erosion
This widens the river valley during the formation of meanders Dominant in the middle and lower courses
64
How does freeze thaw weathering help shape river valleys
Water gets into the rock that has cracks When the water freezes it expands, putting pressure on the rock When the waterfalls and contracts, it releases the pressure on the rock Repeated freezing and thawing widens the cracks and causes the rock to break up
65
What is traction
Large particles like boulders are pushed along the river bed by the force of the water
66
What is suspension
Small particles like silt and clay are carried along
67
What is saltation
Pebble sized particles are bounced along the river bed by the force of the water
68
What is solution
Soluble materials dissolve in the water and the carried along
69
What is deposition in the river
When a river drops the eroded material it's transporting It happens when a river slows down, this is because: The volume in the river falls The amount of eroded material in the water increases The water is shallow The river reaches its mouth
70
How are waterfall is formed
Softer rock Is eroded more than hard rock creating a step in the river As water goes over the step into roads more and more of the softer rock A steep drop is eventually created
71
How is a gorge formed
The hard rock from the waterfall is undercut by erosion and collapses The collapsed rocks or swelled around at the foot of the waterfall where they erode the softer rock This creates a plunge pool More undercutting causes more collapses, the waterfall will retreat leaving behind a steep sided gorge
72
How are meanders formed
The current is faster on the outside of the bend of a river because the river channel is deeper More erosion takes place on the outside of the bend The current is slower on the inside of the bend because the river channel is shallow Eroded material is deposited on the inside of the bend
73
How are ox bow lakes formed
Erosion causes the outside bends to get closer Only a small bit of land is left between the bands (called a neck) The river breaks through this land during a flood The river flows along the shortest course Deposition eventually cuts off the meander, forming an ox-bow lake
74
What are floodplains
Floodplains our flat areas of land that flood
75
How are levees formed
During a flood eroded material is deposited over the whole floodplain Heavy deposited material builds up creating levees along the edges of the channel
76
How are deltas formed
Rivers deposit material that they are carrying when they slowdown If the sea doesn't wash away the material built-up, the channel gets blocked Eventually the material builds up so much that low-lying areas of land called deltas are formed
77
Two main factors increasing floodrisk in the UK
Increased Frequency of storms | Land Use Change
78
How has increased frequency of storms in the UK
Frequency of storms is increasing due to climate change. Storms are becoming more extreme - more intense rainfall is increasing the scale of flood events More rainfall means the ground is saturated, making flooding more likely.
79
How has Land use increased the risk of flooding in the UK
Growing population leads to pressure to expand urban areas Increase of impermeable surfaces - rapid surface runoff Building on floodplains increases risk of developed areas as they are naturally prone to flooding. More people at risk if flood defences fail
80
Threats of flooding to people
People can be killed or injured Roads, railways, bridges damaged/destroyed Floodwater is contaminated with sewage Businesses may be forced to shut down
81
Threats of flooding on environment
Floodwater contaminated with sewage - pollutes rivers, damaging habitats Farmland ruined by sediment being deposited after a flood River banks are eroded Force of floodwater uproots trees