2.A6 The glacier landform system Flashcards
Glaciers alter landscapes from many different processes -
Erosion, entrainment, transport and deposition
Glacier erosion in altering glacier landscapes -
Erosion - removal of rock material by ice and meltwater main ones are abrasion, plucking and meltwater erosion.
Abrasion -
Abrasion used individual stones which erode the bedrock of the glacier which leads to micro features such as striations it is known to polish the underlying rocks in a kind of ‘sandpaper’ action.
Plucking -
Often referred to as glacier quarrying. Can have two initial stages where it begins of widening the joints in the rock and then subsequent entrainment of loose material. The idea of plucking is the process is very dependant on pre-existing joints and the rock types. Where ice masses pull away masses of rock.
Meltwater erosion -
Can be mechanical (similar to fluvial erosion but the water is under hydrostatic pressure. Whereby the meltwater can dissolve away minerals and solutes of little debris and can be carried away especially in limestone rocks (prime GCSE rivers knowledge)
Entrainment inolvement in and out of the glacier -
Entrainment is the inclusion of of debris in, above or below the glacier.
Supraglacial -
Debris is transported on the surface of the glacier (above). Can be material falling from hillsides picked up on the top or even volcanic ash (common on Icelandic glaciers)
Englacial -
Debris is transported inside the glacier. Where material has moved or made its way down vertically through the ice sheet or glacier.
Subglacial -
Debris transported below the glacier. This includes material that has been eroded from the glacier bed and valley walls and frozen to the base from the subglacial streams.
Transportation can be of the three process within or out of the glacier -
Subglacial, Englacial or Supraglacial.
Deposition -
When material is released from the ice at the margin or base of the glacier. This may occur directly on the ground or may be released into the meltwater. Can occur from melting or sublimation of the ice. Can occur by friction at the bedrock.
Landform scales can either be -
Meso-scale, Macro-scale, Micro-scale.
Examples of Meso-scale landforms -
Crag and tail, roches moutennees, drumlins, kames, eskers kettleholes.
Examples of Micro-scale landforms -
Features such as striations, glacial grooves, chatter marks, erratics.
Examples of Macro-scale landforms -
Ice sheet, eroded Knock and Lochan, Cirques, Aretes, pyramidal peaks, glacial troughs ribbon lakes. Terminal moraines.