glacial systems Flashcards

1
Q

over what time period did the Pleistocene last

A

1.8 million years ago until 11700 years ago

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2
Q

what was the name of the ice sheets which covered Briton in the last glacial maximum

A

Scandinavian ice sheets

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3
Q

what are the 4 types of glacial environment

A

polar - areas of permanent ice , Antarctica and Greenland

periglacial - on the edge of permanent ice . permanently frozen ground , Canada , Alaska

alpine - mountain areas- European alps

glacial - found in the edges of ice sheets and in mountainous regions , Himalayas and andes

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4
Q

what happens in the zone of accumulation

A

inputs exceed outputs

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5
Q

what are factors for the accumulation zone

A

higher altitude means increased snow fall

new snow means albedo effect which keeps it cooler reflecting the sunlight

strong winds means snow is blown into hollows and basins - accumulating

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6
Q

what is the albedo effect

A

ice and snow surfaced reflect more light keeping them cooler

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7
Q

what are the 3 factors keeping glaciers cold

A

latitude

albedo effect

altitude

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8
Q

what is the main input in the accumulation zone

A

snow.

turns to compacted ice over years

avalanches and mountain slides can be inputs

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9
Q

what happens in the ablation zone and what are its factors

A

output exceed inputs

lower altitude means less snowfall and higher temperatures

melting

sublimation

evaporation

calving

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10
Q

what are the 2 zones within a glacier

A

accumulation zone

ablation zone

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11
Q

what are the outputs in the ablation zone

A

calving

evaporation

sublimation

melting

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12
Q

what is the equilibrium line

A

the boundary where gains and loses are balanced

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13
Q

what is the glacial budget

A

considers the balance between inputs and outputs

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14
Q

what happens to the glaciers mass balance across a year

A

mass balance varies across a year

in summer ablation will be at its highest due to rapid melting of ice

in winter high snowfall and limited melting results in accumulation being higher than ablation

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15
Q

what are the characteristics of a warm based glacier

A

found at lower latitudes often in alpine environments

water present throughout the glacier which helps with movement

move much more than cold based glaciers . 20-200m per year

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16
Q

how far do cold base glaciers move a year

A

cms Per year

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17
Q

how far do warm based glaciers move per year

A

20-200 m

they erode and move large amounts of material

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18
Q

cold base glacier characteristics

A

found in polar regions in the arctic and Antartica

glacial ice remains frozen to the bedrock so limited movement

movement is cms per year

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19
Q

which glaciers can slide down mountains due to basal siding

A

warm based glaciers

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20
Q

what is basal sliding

A

siding of a glacier over bedrock due to meltwater at glaciers base

21
Q

why does basal sliding occur

A

small obstacles create pressure points

increase of pressure causes melting - pressure melting point is reached

melting allows glacier to slide over the obstacle

meltwater refreezes on the downside of the obstacle and pressure reduces

this melting and freezing is called REGELATION

22
Q

what is regelation

A

the melting and freezing which occurs in basal sliding

23
Q

how do cold based glaciers move

A

internal deformation

24
Q

which glaciers does internal deformation take place

A

warm and cold based glaciers

25
how big it the rate of movement by internal deformation
1-2 cm per day
26
what is intergranular movement
individual ice crystals slipping and sliding over one another ice crystals within a glacier tend to orientate themselves in a direction of ice movements - means they can slide past each other
27
what is intragranular movement
individual ice crystals becoming deformed or fractured because of the stress from the glaciers mass from gravity . ice deforms and moves downhill due to poverty
28
3 characteristics of extensional flow
slope steepens velocity increases ice thins
29
3 characteristics of compressional flow
slope decreases velocity decreases ice thickens - erosion
30
what are the different factors affecting ice movement
temperature of ice - in some places the temperature is so cold the ice freezes to the bedrock which causes slower movement gravity - downhill force causing the ice to move . steeper gradient means greater pull meltwater - lubricants the base of the ice enabling it to slide downhill friction - mass of ice - heavier the ice the more potential energy needed . more force needed
31
what are geomorphological processes
natural process which shape the earths landscape
32
what is weathering
breakdown or disintegration of rock in its original position or just below the ground surface
33
what is the process of frost shattering
water seeps into cracks and freezes when reaches bellow 0 C - it expands by 9% in volume this enlarges cracks and pores overtime cracks enlarge and chunks of rocks break away and pile up as scree
34
what is nivation and where does it take place
nivation makes hollows deeper by freezing and thawing snow gets into hollows and increases the size of the hollows every time ice freezes it expands and breaks bits of rocks when the snow melts the meltwater carries broken rock and debris away eventually the rock becomes deeper and wider
35
what are the 3 glacial processes
transportation erosion deposition
36
what are the 2 main forms of erosional processes
abrasion plucking
37
what is abrasion
the sandpapering affect of ice as it grinds over the landscape
38
where do the scratches in the bedrock come from and why are they useful what are they called ?
come from large rocks carried beneath the ice which scrape on the rocks they are called striations useful for studying the direction of ice flow in the post glacial environments
39
what is plucking
meltwater freezes the bedrock to the base of the glacier. any loose rocks will be plucked away by the glacier.
40
what landform is caused by plucking and abrasion and basal sliding
roche moutonnée
41
how is abrasion shown in a Roche moutonnee
steep sided edge formed by abrasion with evidence of striations on the surface
42
roche moutonnée and basal sliding
ice slides over obstacle due to pressure melting point and melting at the base (basal sliding )
43
where is plucking in a Roche moutonnee
jagged downvalley ice would refreeze on the down valley of the obstacle then move, plucking away the rock
44
what are the 3 types of glacial transportation
supraglacial englacial subglacial
45
what supraglacial
weathered material carried on top of the ice
46
englacial
once supraglacial material , now buried by snowfall and carried in the ice
47
subglacial
material carried beneath the ice , dragged by the overlying glacier
48