Glacial Environments Flashcards

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1
Q

What are glaciers?

A
  • One of the most important agents shaping landscapes we inhabit
  • A key indicator of recent and ongoing climate change
  • Direct cause of potential future environmental catastrophe
  • Main water source for many of worlds major rivers
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2
Q

How are glaciers formed?

A

Glaciers begin to form when snow remains in the same area year-round, where enough snow accumulates to transform into ice. Each year, new layers of snow bury and compress the previous layers

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3
Q

What is basal motion?

A

Basal motion erodes, entrains, transports and emplaces sediment and in process creates sediments and landforms

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4
Q

What is a glacier thermal regime?

A

The thermal regime of a glacier is a function of ice temperature (which again is a function of air and ground temperatures, with some glaciers being heated from below by geothermal heating) and the pressure of the ice

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5
Q

What are the tree types of thermal regime?

A

1) Temp - warm ice except seasonality warmed and cooled surface layer
2) Cold - entirely cold ice
3) Polythermal - both warm and cold ice

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6
Q

Why is the temperature of the glacier bed critical?

A
  • Glacier bed is warmed by friction of movement and geothermal heat
  • It controls whether there is water at the glacier bed, which determines whether it moves through basal motion
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7
Q

Outline glacial landscapes

A
  • Glaciers are orderly systems

- The landscapes they generate are closely associated with their climate, thermal regime and flow dynamics

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8
Q

What are the different types of glacial landforms?

A
  • In a ‘typical’ mid-latitude temperate glacier, clear relationships in the development:
    1) erosional landforms
    2) subglacial bedforms
    3) ice-marginal landforms
    4) meltwater landforms
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9
Q

What are sub glacial bedforms?

A
  • Continuum of streamlined features (both erosional and depositional) formed at the bed of a glacier moving through basal motion
  • Highly controversial features with alternative process-form models:
  • Highly elongate bedforms (MSGLs) suggested to reflect unstable, fast ice in ice-streams and surging glaciers
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10
Q

What are ice-marginal landforms?

A
  • Glacier margins are complex in detail, but broadly comprise formation of moraines and moraine systems:
  • Moraine ridges: terminal, lateral, medial
  • Ice-marginal aprons:
  • Suite of landforms that mark the lateral edge/margin of a glacier
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11
Q

What are proglacial landforms?

A
  • Means by which glaciers extend their influence well-beyond the glacial margin
  • Extreme annual and diurnal variation in melter release
  • Very high sediment load
  • Risk of catastrophic floods – Jokullhlaups
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