Ice On Land Flashcards

1
Q

What is Accumulation

Ablation?

A

Inputs into the glacial budget (eg snowfall)

Outputs from the glacial budget (eg meltwater)

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2
Q

Where does accumulation/ablation respectively dominate

A
Acc = top of glacier (highest point)
Abl = snout of glacier (ie front)
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3
Q

Differences betw ice cap and ice sheet

A

Both glaciers

Ice sheet = over 50,000 km ^2 eg Antarctica and Greenland

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4
Q

What does it mean when a glacier retreats

A

When the total volume of the glacier decreases

As a result the glacier does not extend as far down the valley as previously

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4
Q

Differences betw ice cap and ice sheet

A

Both glaciers

Ice sheet = over 50,000 km ^2 eg Antarctica and Greenland

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6
Q

Facts about athabasca

A

In Canada

Nowadays only advances by 300m and is over 1750m away from max extent of 1850

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7
Q

Man made impacts on glacial budget?

A

Anthropogenic climate chance since IR (1850)
Deforestation
Greenhouse gases from burning of fossil fuels in vehicles and factory
= greenhouse effect
As a result avg global temp has increased from 9.6 to 10.8
Evidence of glacial impact = athabasca

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8
Q

Long term impacts on glacial budget

A

Milankovitch cycle - influences length of seasons and amount of solar radiation received by the earth which thus influences amount of abl / Acc

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9
Q

What is the milankovitch cycle?

What does it involve?

A

Describes how the earth orbits the sun
Includes
the eccentricity (how round the earth is)
The obliquity (angle of earths orbital axis)
The precession of the earth (direction of axis)

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10
Q

facts about the last ice age

A

Pleistocene
1.8 million - 11500 years ago
4 major ice sheets covered the planet, eg the British Isles were covered

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11
Q

What is the interglacial period we’re in called? Facts?

A

Holocene period
2 ice sheets
Antartica = 14 mil km^2
Greenland = 1.7 mil km^2 (80% Greenland)

Ice caps found in mountainous areas where temps are lower
Eg Iceland and the European Alps

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12
Q

Temp change from IR to now

A

Avg temp in Alps was 9.6, now 10.8

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13
Q

Causes of anthropogenic climate change

A

Deforestation : carbon sink
CFCs use (burnt hole in atmosphere)
Greenhouse gases emitted from oil/petrol
Oceans warming cos of global warming = ice melts which emits carbon

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14
Q

What direction does the glacier move? Why?

A

glacier flows from the zone of Acc and moves down the slope towards the zone of abl
It is under the influence of gravity and internal deformation

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15
Q

What is internal deformation

A

When the weight of the ice deforms the ice crystals
This usually happens near the glacial bed as pressure there is highest.
This enables different layers of ice to slide over each other

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16
Q

What is basal sliding

A

Meltwater at the base of a glacier acts as a lubricant and the glacier consequently slides over the land

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17
Q

Diagram of basal sliding

A

Glacier
Meltwater acting as lubricant
Bedrock

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18
Q

What do glaciers move fast with?

A

Increasing slope
Increasing snowfall
Increasing meltwater at the base of glacier

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19
Q

How does freeze thaw weathering work

A
  1. As it rains precipitation falls into the cracks of rocks
  2. Overnight the temp goes sub zero
  3. The water in the cracks expand by 9-10% as it is turning into ice
  4. As water expands the cracks expand
    (This repeats itself a lot)
  5. Eventually this weakens the rock until it breaks
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20
Q

What is left from freeze thaw weathering

A

Scree

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21
Q

What is scree

A

Small, broken down pieces of rock

They are generally jagged

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22
Q

What is ablation?

A

The wearing away of rock surfaces of the valley floor by the grinding effect of rock fragments frozen into the glacier base

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23
Q

What does ablation leave?

A

Sandpaper analogy!
Smooth surface
Striatations

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24
Q

What are Striatations?

A

Often left by abrasion

Scratches in the floor caused by large rocks beneath the ice

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25
What is till?
Boulder clay found within the glacier
26
What is plucking? Analogy?
When meltwater freezes it bonds glacier to rocky surface below, therefore when the glacier lives it plucks away any loose rocks leaving a jagged landscape Rock fragments are dragged along the base of the glacier Extracting loose teeth analogy
27
What processes do all glaciers do
Erode Transport Deposit material
28
What happens when a glacier goes down a valley
It'll begin to melt due to rise in temp
29
What happens as a glacier melts? | Key terminology answer as wel
It can't carry as much material so it deposits it | The load has exceeded the glaciers carrying capacity
30
What are morraines
Ridges of sediment
31
Terminal morraine?
Sediment found at the max advance of glacier Deposited as ice melts Most of the material will have been plucked and carried at the base of glacier
32
What is lateral morraine?
Sediment (normally frost shattered material) found At the valley sides (It had been carried on the side of the glacier)
33
Medial morraines
When two valley glaciers meet and merge the two lateral morraines form one big morraine which runs down the centre of the largest glacier
34
Recessional morraine?
Before the terminal morraine | When the glacier stops for a sufficient time to produce morraine yet the glacier has not reached its furthest extent yet
35
What is bulldozing
Pushing of deposited sediment at the snout of the glacier as it advances
36
What is a corrie
Arm chair shaped hollow high up on a hillside often containing a tarn. Has a steep back wall and a raised lip
37
How do corries form
Snow collects in a hollow high up on a mountain This snow compacts into ice, forming a corrie glacier The ice moves under gravity due to basal sliding Ice rotates to the rock lip (flows uphill) and this rotational slip gouges out a deeper hollow Abrasion deepens the hollow Plucking steepens the back meal A tarn may fill a hollow when ice has melted because of raised lip which forms due to reduced erosion at front of corrie because it's thinner ice
38
What is an arête?
A knife edged ridge, often formed betw two corries
39
How do aretes form?
Occur when two neighbouring corries run back to back | As each erode each side of the ridge, the ridge becomes steeper and narrower
40
What is a pyramidal peak?
Sharp edged mountain peak eg Mount Everest
41
How do pyramidal peaks form?
If 3 or more corries hVe formed on a mountain all back to back erosion may cause it to become a single peak rather than a ridge
42
Example of arête and pyramidal peak?
Arête - striding edge in Lake District | Pyramidal peak - Matterhorn, Mount Everest
43
How are truncated Spurs formed?
When a glacier erodes through a valley where there used to be interlocking Spurs The glacier can't flow through the interlocking Spurs so it cuts through them This leads steep edge Spurs at the sides of a glacial trough
44
What are truncated Spurs
Steep edged Spurs at the side of a glacial trough
45
What is a glacial trough
U shaped valley (used to be v shaped)
46
What does it mean when a glacier advances
When the total volume of the glacier increases | As a result it will extend down the valley further than previously
47
Formation of glacial trough?
There is a vshape valley with a main river running down it In a period of glaciation the river freezes into main glacier As the glacier lives down the valley it plucks and abrades the base and side of the valley The material it gathers under the glacier (subglacial morraine) aids the process of abrasion This widens and deepens the valley floor leaving a flat floor with v steep valley walks A misfit stream will form and sometimes a hanging valley waterfall will
48
How do hanging valleys form?
Large glacier is joined by a tributary glacier (because main lake was joined by a smaller lake) The large glacier moves down v shaped valley and via erosion leaves a u shaped valley (a glacial trough) The small glacier simultaneously erodes but erodes slower/less powerfully Therefore it doesn't erode to the same depth As a result it looks like it's hanging Waterfalls sometimes form
49
Learn glacial trough formation diagram
Okay
50
What is a ribbon lake?
Long and thin lakes in the floor of a glaciated valley
51
How do ribbon lakes form?
Glacier moves down hard rock, finding it hard to erode as rock is more resistant When glacier reaches soft rock it can easily erode This leaves a rock basin (hard rock steep compared to soft rock eroded in depth) A band of hard rock follows the soft rock (glacier can't erode this as much so it's higher up than the soft rock) A ribbon lake will form on the soft rock but be dammed by the rock bar / any morraine built up
52
Egs of landforms of erosion
``` Corrie Pyramidal peak arête Truncated spur Glacial trough (u shaped valley) Hanging valley Ribbon lake ```
53
What is a drumlin
A smooth elongated mound of Boulder clay which has been streamlined by ice
54
Shape of drumlin
They have a broad and upstream stoss end and a gentle tapering lower downstream end (lee end)
55
How do drumlins form
Melting glacier meets a small obstacle which is enough to encourage the deposition of till from the ice as the glacier had a low competence On first meeting the obstacle the most deposition occurs (this forms the blunt stoss end) The glacier mounds the till into shape around the obstacle which forms a tapered lee end Overtime material is reshape by further i e movements
56
Typical measurements of a drumlin
Up to 40 m high | 400m long
57
Flow diagram of ice
Ice erodes Transports Deposits Landform is reshaped
58
What is a fragile environment? Ecample?
A area which is easily damaged and would take a long time to recover
59
Winter attractions at chamonix
Paragliding over glaciated landscape Iceskating at chamonix ice rink Winter mountaineering
60
Summer attractions at chamonix
Sightseeing eg Aigulle du Midi Hiking (350km trail) Mountain biking (5 mile trail)
61
How can human activity damage glacial environment?
Air pollution from vehicles / heat from hotels = increase local temp = melting of snow (loss of habitats) Less snow on slopes = concentration of people further up mountains = more erosion at top of mountain Less snow on slopes = snow machine = uses lots of water = affects hydrological system Summer activities eg mountain biking = erosion, environment can't recover Deforestation/ removal of vegetation = increases risk of erosion, loss of habitat, decreases slope stability
62
Positive impacts of tourism in chamonix
Brings in money which supports local services Provides jobs Experience of different cultures
63
Negative impacts of tourism in chamonix
10000 people population swells to 100,000 in summer a day Noise pollution due to tourism/congested roads Footpaths eroded Trees cut down to make way for skiing paths Sking close to tress can damage them Shops are tourist orientated Inflation in some shops
64
The three management strategies in chamonix
Tomorrows valley Espace Mont Blanc Respect the mountain
65
What does tomorrow's valley do/ who does it involve
Mix of locals and tourists : finds a balance Maintains footpaths Renovates historical monuments Plants trees
66
Whag does Espace Mont Blanc do/ who does it involve?
International issues betw France Italy and Switzerland reduces pollution and congestion Nature conservation
67
How tourism can damage a glacial area ?
Air pollution from vehicle emissions / heat from hotels = increase local temp = melting of snow = habitats lost and erosion Less snow on low slopes = people move up the mountain = more erosion up the mountain Less snow on low slopes = snow machine = lots of water used up = effects hydrological system Summer activities = eg mountain biking = leads to erosion, fragile environment can't recover Deforestation for skiing = habitats lost, slope instability, risk of erosion
68
What does respect the mountain do?
Tells tourists why mountains are so important Tells them to recycle and be respectful Sell £2 wristband where profits go to tree planting to conserve environment
68
How tourism can damage a glacial area ?
Air pollution from vehicle emissions / heat from hotels = increase local temp = melting of snow = habitats lost and erosion Less snow on low slopes = people move up the mountain = more erosion up the mountain Less snow on low slopes = snow machine = lots of water used up = effects hydrological system Summer activities = eg mountain biking = leads to erosion, fragile environment can't recover Deforestation for skiing = habitats lost, slope instability, risk of erosion
69
Types of avalanches
``` Powder Soft slab Hard Slab Climax Wet ```
70
Powder avalanches?
Windy but dry conditions | freshly layer of fallen cold snow is blown off
71
Slab avalanches
Two types : soft (new powdery snow) and hard (old, more dense, chunkier snow) Big range of mountain Hard = more dangerous A layer of rigid snow on top of a layer of softer, more mobile snow Often set off by explosives to reduce impacts
72
Climax avalanches?
Aka delayed action avalanches | weight of fresh snow causes rest of snow to succumb
73
Evidence of human impacts on avalanches
100 or so natural avalanches at chamonix 10 set off by skiers off piste at chamonix 90% people who die in avalanches set them off themselves
76
what is an avalanche
A mass on snow sliding down a valley under the influence of gravity
77
Management of avalanches
Warnings sent out They blow it up with dynamite Afforestation (trees set up like a wall) Snow fences/ barriers to trap snow eg Paravalanche de Tacconaz at chamonix Avalanche proof tunnels
78
What can make avalanches likely?
Heavy accumulation (snowfall on unstable area puts pressure on snowpack) Steeper slope Human activity (eg vibrations from mountain bikes) Warm temp Layers of snow turning to ice (fresh snow easily slides down)
79
Wet avalanches?
Common in spring Made up of wet snow Either due to warmth/rainfall causing snow to melt off