4.1 Glaciated Landscapes And The Glacial System Flashcards

Landscapes and systems

1
Q

What is a glaciated landscape?

A

A landscape which is distinctive in that its characteristics are exclusively linked to glaciation

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2
Q

What is in the foreground?

A

An active glacier

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3
Q

Example of an active glacier?

A

Mer de glace, France.

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4
Q

Is there vegetation in the foreground?

A
  • trees

- some traces of vegetation beginning to take hold of side valleys

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5
Q

What is a glacial system?

A

This is where several components integrate to function as a system.

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6
Q

Inputs in a glacial system

A
  • snow

- avalanches

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7
Q

Outputs

A
  • liquid water - melting of ice close to snout
  • calving
  • sublimation
  • evaporation
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8
Q

What is calving?

A

Huge chunks of ice break off to form icebergs.

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9
Q

When a glaciers mass is combined with the force of gravity what energy is generated?

A

Potential energy

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10
Q

What is the potential energy converted into to carry the glacier?

A

Kinetic energy

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11
Q

What processes are carries out as a result of movement from kinetic energy?

A
  • erosion
  • transportation
  • deposition
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12
Q

What is the main store in a glacial system?

A
  • snow

- ice

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13
Q

How often does variation in magnitude occur?

A

Seasonally

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14
Q

Which regions are seasonal variations in magnitude most common in?

A

Temperate regions

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15
Q

Over how many years have the stores of many world glaciers shown a decline in mass?

A

30

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16
Q

why has there been a decrease in glacier mass?

A
  • recent trends in climate change

- and global warming

17
Q

what do flows/transfers include?

A
  • evaporation
  • sublimation
  • melt water flow
  • processes of glacial movement: internal deformation and basal sliding
18
Q

where are flows and transfers more active?

A

warmer environments where there are significant seasonal variations in temperature.

19
Q

where are flows and transfer less active?

A
  • coldest environments

- e.g. Greenland

20
Q

dynamic equilibrium

A

found in a glacial system - an equilibrium line can be drawn on the boundary line of the accumulation zone (input zone) and the ablation zone (output zone).

21
Q

how is the equilibrium line balanced?

A

as the balance shifts, the equilibrium line will move up or down the glacier, hence the term ‘dynamic’ equilibrium.