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Factors Affecting Movement

Glaciers move by a range of different processes and at different rates. A range of factors influence rates of glacial movement.

Altitude

Altitude

  • The potential energy gained from height can increase glacier movement.
  • But, high-altitude glaciers are more likely to be cold-based for longer time periods in a year so won't move as much.
Slope and lithology

Slope and lithology

  • Steeper sloped valley glaciers have higher rates of flow.
  • Lithology influences bed topography. Easily eroded rocks (e.g. sandstone) are more likely to eroded, creating deformations which may slow movement down.
Mass balance

Mass balance

  • Areas of accumulation have slower rates of movement than areas of ablation.

Types of Glacial Movement

Glaciers move by a range of different processes and at different rates.

Basal slip

Basal slip

  • Basal slip is linked to the pressure melting of ice that takes place along its base.
  • Ice normally forms from water at a temperature of 0oC, but the temperature at which water freezes is reduced under pressure.
  • As a glacier moves it will exert pressure and so some melting may take place at its base.
  • A thin film of water then exists between the glacier and the bedrock.
  • This film reduces friction, acts as a lubricant, and allows the glacier to slide.
Regelation creep

Regelation creep

  • Regelation is the re-freezing of water under a glacier when pressure reduces after meeting an obstruction.
  • Pressure melting takes place on the upstream side, creating a film of water, and regelation takes place on the downstream side.
  • The combination of both processes allows a temperate glacier to slide downhill.
Internal deformation

Internal deformation

  • Internal deformation is small in scale and takes place in all glaciers, but it is the most common form of movement in cold-based glaciers.
  • It takes place where the ice crystals set themselves in line with the movement of the glacier and slide past each other.
  • Movement can occur along lines of weakness called cleavage planes . This is sometimes called laminar flow.
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