OCR A Level GL - 6 OCR A Level GL 2.2a Geomorphic and Glacial Processes Flashcards
What is weathering?
the in situ breakdown of rocks exposed at, or near, the land surface by physical, chemical and biological processes.
What is physical weathering (Mechanical)?
the in situ breakdown of rock in which there is no chemical alteration. In glacial environments, these include “Freeze-thaw”, “Frost-shattering” and “Pressure Release”.
What is freeze-thaw weathering?
a form of physical weathering in which water enters cracks/joints in rocks then freezes, expanding by 10% in the process, and causing the rock to split or for pieces to break off. Particularly prevalent in areas where temperatures fluctuate around zero (i.e. areas of high altitude with diurnal changes in temperature).
What is frost shattering?
a form of physical weathering in which water trapped in rock pores freezes at extremely low temperatures, exerting stress and disintegrating the rock into small particles.
What is pressure release (dilatation)?
a form of physical weathering whereby rock underlying a glacier expands and fractures parallel to the surface when the weight of a glacier is removed when it melts.
What is chemical weathering?
the in situ breakdown of rock in which there is a chemical reaction between elements of the weather and some minerals within rocks. These type of weathering includes oxidation, carbonation, solution, hydrolysis and hydration.
What is oxidation?
a form of chemical weathering in which minerals in rocks react with the oxygen found in the air. This process particularly happens in rocks with high iron content (such as sandstone).
What is carbonation?
a form of chemical weathering in which carbonic acid (formed when rainwater combines with dissolved carbon dioxide) reacts with calcium carbonate, in particular found in limestone.
What is solution?
a form of chemical weathering whereby a mineral dissolves in water.
What is hydrolysis?
a form of chemical weathering in which water chemically reacts with rock minerals. Examples include: Silicate + Water = clay Feldspar (found in granite) + hydrogen (found in water) = kaolin (china clay)
What is hydration?
a form of chemical weathering in which water and rock minerals form new minerals of a larger volume. This process can cause surface flaking of rocks.
What is biological weathering?
the in situ breakdown of rock that is caused by the physical actions of plants and/or animals or by organic acids (chelation)
What is mass movement?
the movement of material down a slope when the forces acting on the slope (mainly gravity) exceed the forces keeping the material on the slope (friction).
What is rock fall?
when rocks dislodge from a steep slope (40 degrees or more) and fall to the foot of the slope under gravity. This mainly occurs in areas where bare rocks are exposed to physical weathering processes.
What are rock slides?
When a section of rock or soil moves downhill. This can be Linear - in which movement is along a straight line slip plane. This often occurs between bedding planes. Rotational - movement is along a curved slip plane (also known as slumps). This is a key process in the formation of corries.
What is glacial erosion?
The action of removing rock by a glacier
What is plucking (quarrying)?
a form of glacial erosion in which meltwater seeps into joints in rock on the valley floor or sides. This then refreezes and becomes reattached to the glacier. As the glacier advances, it pulls pieces of rock away. This mainly takes place at the base of a glacier where pressure melting can take place. If the bedrock is highly jointed then this process will be particularly effective.
What is abrasion?
a form of glacial erosion in which as a glacier moves across a surface, the debris that is embedded withing it scours the rock and wears them away. Larger or more coarse material will scrape, scratch and groove the rock - forming striations. Smaller and more fine material will smooth and polish the rock.
What factors affect the rate of abrasion?
- Presence of basal debris
- Debris size and shape
- Relative hardness of particles and bedrock
- Ice thickness.
- Basal water pressure
- . Basal sliding
- . Movement of debris to the base of the glacier
- . Removal of fine debris