GLACIERS - FULL TOPIC

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Last updated 7:31 AM on 1/29/26
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1
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Biggest conflcit in Lake District

Farmers vs tourists

2
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Other groups that could conflict

Locals vs tourists

Conservation vs hunting/quarrying/forestry etc

Forestry vs farming

3
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Solution to tourists not abiding by the Outdoor Code

Signs and educating tourists

4
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Solutions for traffic congestion

Public transport, parking payment, one way systems

5
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Solutions for footpath erosion

Volunteers maintain paths with local materials (fix the fells)

6
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Solutions for overflowing bins

Taking away bins to encourage people to take litter home

7
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Solution for noise and air pollution

Public transport to reduce car numbers

8
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Solutions for closed services due to second home owners not being permanent residents

Mobile services and second home tax

9
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Glenriddig zip wire conflict between who?

Tourism industry vs locals

10
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Glenriddig zip wire conflict: how many people for / against

13 people for, 324 people against

11
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Glenriddig zip wire conflict: % of people against

96%

12
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Why were people against the Glenriddig zip wire

Could drive away tourists seeking peace and quiet

Building could damage ecosystems

13
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Why were people for the Glenriddig zip wire

Economic opportunity

14
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Where were the first 3 wind turbines in the Lake District built

Summit between Ambleside, Troutbeck and Ullswater

15
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Name of the pub benefitted by the Lake District wind turbines

Kirkstone Pass

16
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How much did the wind turbines in the Lake District cost

£135,000

17
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Why were people against the Lake District wind turbines

They would be alien and ugly

18
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National Trust opinions on the Lake District wind turbines

had concerns, but were in favour for the upkeep of the pub

19
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Why were people for the Lake District wind turbines

Reduces the cost of the Kirkstone Pass getting heating and light, allowing it to stay open

20
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When did the Lake District gain National Park status?

1951

21
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Where is the Lake District located?

North West England

22
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What is the Lake District famous for (summary)

Lakes, mountains, activities, monuments, authors, villages

23
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What are the famous lakes in the Lake District?

Windermere, Ullswater

24
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What are the famous peaks in the Lake District?

Helvellyn, Scafell Pike

25
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What are the famous scenic villages in the Lake District?

Ambleside, Grasmere

26
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What are the famous authors in the Lake District?

Beatrix Potter, William Wordsworth

27
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What are the famous monuments in the Lake District?

Ravenglass, Muncaster Castle

28
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What are the famous activities in the Lake District?

fishing, watersports, hiking, rock climbing

29
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Social impacts of tourism in the Lake District

Impacts 40,000 locals

Over 89% of visitors arrive by car = traffic congestion

High house pricing - 20% = holiday rental or second homes

Tourism jobs are seasonal, unreliable and poorly paid

30
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Economic impacts of tourism in the Lake District

Tourists spent nearly £1000 million

Provides jobs for thousands

Traffic congestion slows down business communication

31
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Environmental impacts of tourism in the Lake District

Traffic congestion = CO2 fumes

Overcrowding, litter and footpath erosion

Verge damage by cars

32
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Traffic congestion management in the Lake District

Public transport is sustainable

Dual carriageways

Transport hubs eg. Ambleside

Speed bumps in villages

33
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Footpath erosion management in the Lake District

Fix the Fells - scheme to clear footpaths

Local resources are used

However not sustainable as paths need constant attention

34
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Economic development vs conservation in the Lake District

Conservation should be more important but both are managed simultaneously

35
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How many tourists visited the Lake District in 2014?

14.8 million

36
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Freeze-thaw weathering

Water expands into ice in cracks, making cracks bigger

37
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Freeze-thaw weathering summary

Water seeps into cracks

Water = freeze = ice

Water—> ice = expands

Cycle repeats and cracks get bigger

38
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Plucking

Meltwater freezes around rocks and ice pulls the rock away

39
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Abrasion

Sandpaper friction effect of rock on rock at the base, causing erosion

40
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Percentage of water to ice expansion

10%

41
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Corries (upland)

Bowl shaped hollows with a steep back wall

42
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Corrie formation

Glacier, downslope, erosion =- steep back wall

Glacier hits a rock lip = rotational slip = basin

Ice may melt = tarn (lake)

43
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Arête (upland)

Two corries back to back, creating a sharp ridge that separates two valleys

44
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Pyramidal peak (upland)

Three or more corries back to back creating a sharp edged mountain peak

45
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Glacial trough / U-shaped valley (lowland)

A valley with a flat bottom and steep sides

46
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Glacial trough / U-shaped valley formation

A glacier moves through a young V-shaped valley, eroding it and forming a wide U-shaped valley

47
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Interlocking spurs

Projecting ridges extending from alternate sides of a valley

48
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Truncated spurs

When interlocking spurs have been cut off due to erosion

49
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Hanging valley

A smaller valley on the side of a main valley with a sharp fall between them

50
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Hanging valley characteristics

Tributary river flowing through and a waterfall flowing into the main valley

51
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Hanging valley formation

V-shaped valley with main river and tributary

Large glacier in large valley and smaller one in smaller valley

Main valley = more ice and erosion = Large valley

Small valley = less ice and erosion = Small joined valley

52
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Drumlins

Smooth hills with a blunt end and a tapered end

53
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Drumlins and ice flow

Ice flowed in the direction of the tapered end

54
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Drumlins formation

Ice flows down but there is an obstacle

Ice flows around obstacle

Moraine piles up behind obstacle and is overloaded (blunt end)

Flows over the obstacle and tapers out

55
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Erratics

Large boulders differing from bedrock they were found in

56
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Ground moraine

Underneath the glacier via plucking

57
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Terminal moriane

At the end of the glacier, bulldozed by the snout

58
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Lateral moraine

Ridge of material round the edges of the glacial trough via freeze-thaw weathering

59
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Medial moraine

Two lateral moraines joining to make a ridge of material down the middle of where two glaciers join

60
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Upland soil (farming)

Thin and acidic so bad for crops

61
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Upland farming

Extensive grazing (sheep and deer)

62
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Valley soils (farming)

Thick due to deposition

63
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Valley farming

Flat valleys are easy for machinery, crop farming

64
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Crop examples in valleys

Cereals, potatoes, grass for winter

65
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Lowland soils (farming)

Fertile due to till coverage

66
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Lowland farming

Flat/rolling landscape and warmer climate is good for extensive crop farming

67
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Forestry

Conifers are adapted for acidic soils so are planted on steep upland slopes

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Forestry outcomes

Conifers are used for paper and soft wood

69
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Lowland quarrying

Sand and gravel deposits for construction industry

70
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Lowland quarring outcomes

sand makes cement

gravel makes concrete

71
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Upland quarrying opportunities

Hard and resistant rock

72
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Upland quarrying outcomes

Construction and road building

73
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Upland quarrying example

Pennine hills, UK

74
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Why do tourists like glaciated areas

unique scenery, activities, cultural heritage

75
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Tourism outcomes

Creates jobs

76
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Tourism example

Aviermore: Scotland, Lake District etc

77
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Moraine

Any material carried by a glacier

78
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How can moraine be carried?

On the surface, inside the glacier, beneath the glacier

79
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Glacial outwash

Moraine carried by water

80
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How is glacial outwash obtained?

Meltwater rivers carry large amounts of sediment

81
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Characteristics of glacial outwash

Fine, round, smooth, small as it has been eroded by water

82
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Glacial till

Moriane carried by ice

83
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How is glacial till obtained?

The glacier acts as a conveyor belt and material trapped inside makes its way to the snout where the ice melts and it is deposited

84
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Glacial till characteristics

Angular and unsorted, can be large. No erosion

85
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Glaciers move due to:

gravity, weight of the ice, meltwater

86
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Basal sliding summary

Weight = more pressure

Pressure = warmth

Warmth = meltwater

Meltwater = lubrication and sliding

Gravity = slides downhill

87
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Basal sliding

Weight and pressure cause warmth and meltwater which makes the glacier slide downhill

88
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Rotational slip

Ice moves in circular motions if it can’t go downhill

89
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Rotational slip summary

Snowflakes in hollow = ice

Ice = trapped and can’t move down

Circular motion = crevasses

90
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Bulldozing

Weight of the ice and gravity makes it push material forwards via snout

91
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% of land covered in ice (global present)

10%

92
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How many countries are glaciers found in?

47

93
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% of fresh water supplies stored by glaciers

80%

94
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Age of antarctic ice sheet

40 million years

95
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90% of modern ice is located where?

Antarctica and the Arctic

96
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Most recent ice age

2.6 million years ago

97
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Ice age definition

A period of long term cooling of the atmosphere

98
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2.6 million years ago —> present

Quaternary period

99
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11,000 years ago —> present

Holocene epoch

100
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What makes it an ice age

If there is ice on earth

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