Processes & Landforms Of Erosion Flashcards
Name the 4 Variables controlling rate of erosion:
- Glaciological
- Substratum
- Temporal
- Topographic
What is glaciological?
- ice processes at the bed.
Basal sliding, stress, glacial drainage, shear stress, debris entrainment.
Temporal
- Duration of Glaciation
Topographic
- Type of land
Morphology of bed.
Roughness, channel type, catchment size, gradient.
Substratum
Characteristics of the ice.
Permeability, porous, thickness, lithology.
4 types of Erosion:
Debris entrainment
Plucking and quarrying
Abrasion
Meltwater erosion
Plucking and Quarrying
Regelation, causes rocks to be plucked up into the base of the glacier.
Has to be pre existing cracks to do so.
Meltwater erosion
Water interacting with rocks
Cold water has more co2 dissolved, more acidic, can erode carbonate rocks more easily. Chemical erosion.
Debris entrainment
Meltwater at base refreezes and incorporates debris which pushes debris up into glacier through ice deformation and thrusting causing sheets pushing up through ice.
Factors of glacier that promote erosion.
Velocity
Amount of meltwater at base.
How quickly glacier can re freeze. Quickly refreezes means more plucking.
Micro scale and macroscale
Micro = less than 1m Macro = larger than 1km
Types of micro
Chattermarks (hammered in C shapes), striations, Rat-tail (rips out bits of sediment and drags them out) and fractures.
P- forms.
Types of Macro:
Cirque (start of glacier, snow accumulates and erodes deeper and deeper, steep back wall). Fjord (Milford Sound, a parabolic valley, builds or erodes river channel, glacier goes through and then melts and leaves valley).
Aerial scour - large scale sandpapering by extensive warm based ice.