Glaciation Flashcards

(45 cards)

1
Q

what is an example of a cold based glacier?

A

Meserve Glacier, Antarctica

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2
Q

how do cold based glaciers move?

A

Internal deformation
- intergranular flow
- laminar flow

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3
Q

how do warm based glaciers move?

A

Basal slippage
- regelation slip
- creep
- glacial surge

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4
Q

what are the details of the cold based glacier?

A
  • 7km long
  • basal temp is -17C
  • silt rich basal layer
  • slow movement
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5
Q

what is an example of a warm based glacier?

A

Athabasca Glacier, Canada

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6
Q

what are the details of the warm based glacier

A
  • move 2-3m a year
  • 6km long
  • 90-300m thick
  • basal temp at PMP
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7
Q

what is intergranular flow

A

when individual ice crystals re-orientate and move in relation to each other

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8
Q

what is laminar flow

A

movement of individual ice layers within the glacier

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9
Q

what is regelation slip?

A

Glacier melts to go over obstacle, then refreezes on other side due to pressure

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10
Q

what is creep?

A

if ice encounters obsctale, its put under strain so deforms plastically and flows or creeps around the obstacle

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11
Q

what is the case study of a landscape associated with the action of ice sheets?

A

Minnesota and the Laurentide ice sheet

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12
Q

what is Minessota’s geology

A
  • rocks lie in alternating belts of volcanic and sedimentary rock
  • between these belts is granitic rock
  • gneisses have been faulted to form some mountains
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13
Q

how did the ice move across Minessota

A
  • there were 4 lobes
  • lobes advanced and retreated based on climate
  • wadena lobe
  • rainy and superior lobe
  • des moines lobe
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14
Q

how did the ice affect the geology of Minnesota

A
  • origins of lobes resulted in till
  • it transported and deposited this till as it advanced and retreated
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15
Q

what was the erosional impact on the relief in Minnesota?

A
  • as ice was sometimes 1km thick is wore down mountains
  • now the highest peaks only 500-700km
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16
Q

creating of lakes in minnesota?

A
  • earlier tectonic tilting revealed weaker shales which are less resistant
  • caused ellipsoidal basins
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17
Q

what is the wadena lobe

A
  • deposited drumlins and glacial drift
  • till left the ground moraines with a reddish colour
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18
Q

rainy and superior lobe

A

left behind coarse textured till with basalts, gabbro and red sandstone

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19
Q

des moines lobe

A

till which is tan to buff coloured and clay rich

20
Q

what is minessotas pro glacial lake

A
  • Lake Agassiz
  • maximum covered 440,000km2 and in place it was 400m deep
21
Q

case study of a landscape shaped by the action of valley glaciers

22
Q

when was Snowdonias glaciation at its extent

A

20,000 years ago

23
Q

U-Shaped valey in snowdonia

A
  • Nant Ffrancon
  • carved by an outlet valley
24
Q

what are snowdonias erosional features

A
  • corrie
  • aretes and pyramidal peaks
  • truncated spurs
  • hanging valleys
  • roche moutonnee
  • u shaped valley
25
what are snowdonias depositional features
- tills and moraines - eskers - drumlins - kames
26
what is the study of human activity in periglacial environments
trans Alaskan Pipeline
27
details of the trans alaskan pipeline
- pump 1.4 million barrels - 1300km long with over 600m built on stilts
28
what is the need for oil in alaska
- Alaska has 3 billion known barrels - they have no energy security
29
what is area 1002
- contains over 16 billion barrels of oil so need to drill it to meet demands - 6070km in NW part of Arctic Refuge
30
what are the support drilling into area 1002?
- oil industry supports - many alaskans get money from industry - $3000 per person - provide energy security
31
reasosn against drilling area 1002
- some alaskans rely on Carabou and this would impact their migration - only 50% chance of actually finding oil
32
solving problems with alaskan pipeline
- pipe is raised so no heat on permafrost - animals move below pipeline so migration routes not blocked - pipe is above river bed
33
what is the impact of alaskan pipeline on glacial material flows
- permenant settlements alter thermal temp of ground - lead to thaw of permafrost - buildings are raised to remove heat
34
what is the impact of alaskan pipeline on glacial energy flows
- release gas during drilling - release CO2 and methane which impact global warming
35
effect of buildings in alaska on the permafrost
- have heating effect - lead to mobility of active layers and solifluction
36
what is the methane problem in alaska
- organic matter frozen in permafrost is major source of methane - thawing leads to decomposition and released CO2 and methane
37
what is the impact of alaskan pipeline on plants
- as more water is available there is rapid growth of plants - as permafrost melts, no impermeable layer to prevent drainage - after few motnhs, there is no water left.
38
what is the cases study of human activity in glacial areas
Grande Dizence Scheme in Switzerland
39
what are the details for Grande Dixence Scheme
- built in 1960s to provide hydroelectric power - cost of building was 1600million - hgihest gravity dam - 285m high
40
what are the water details for grande dixence scheme
- stores of 400million m3 of water - water from area of 35km2 and meltwater from 35 glaciers - four pumping stations
41
energy production for grande dixence scheme
- glacial meltwater is stored in summer and used for high demand power in winter - powers 400,000 homes
42
what is the impact of the grande dixence scheme on the environment
- pumping stations are mianly underground - tourism has increased for helicopter rides - higher pollution from domestic sources
43
impact of grande dixence scheme on glacial system
- 85% of water used for generation - 15% used for sediment problems - lack of water flow leads to deposition behind dam
44
impact of grand dixence scheme of river channel
- increased channel erosion - contraction in channel size - risk of sudden flooding
45