Rocks and weathering 3.2 Flashcards
What is weathering?
The decay and disintegration of rocks.
Physical weathering: freeze thaw
- Process of water getting into cracks during the day before freezing overnight, expanding by about 10%.
- The crack is widened as force of expansion is greater than the resistance of the rock.
Physical weathering: thermal fracture
- Large ranges in temperature in deserts cause rocks and minerals to expand and contract, resulting in disintegration.
Physical weathering: salt crystal growth
- When salt solutions such as sodium carbonate in the pores or joints of a rock crystallise.
- Temperatures of around 27 degrees is optimum and can produce expansion rates of up to 300%.
Physical weathering: pressure release
- Process when ground surface is lowered by erosion which reduces weight of load.
- This leads to expansion of rocks below which forms cracks.
Chemical weathering: hydrolysis
- When a mineral is broken down by reactions with water.
- This causes a change in chemical composition where the rock becomes more unstable.
- Occurs on rocks containing feldspar.
Chemical weathering: hydration
Wetting and drying of rocks adds and removes water causing expansion or contraction.
Chemical weathering: carbonation
- Process which affects carbonate minerals where rainwater containing carbonic acid attacks carbonate minerals.
- This forms chalk and limestone.
Chemical weathering: organic action
- Process of roots working their way into cracks in rocks.
- As roots become bigger, cracks widen and deepen, breaking up bedrock.
Which 5 factors affect weathering?
- Climate
- Vegetation
- Relief
- Rock structure
- Rock type
Factors affecting weathering: climate
- Determines which weathering processes occur and rate at which they occur.
Factors affecting weathering: vegetation
- Type: larger vegetation such as trees are more likely to break apart rocks with larger roots.
- Structure: high density of vegetation increases organic action
Factors affecting weathering: relief
- Steep: types of weathering caused by rain is less prevalent
- Gentle: subjected to standing water and infiltration which increases rates of weathering.
Factors affecting weathering: rock structure
- Soft/hard: softer and more permeable rocks are more susceptible to weathering
- Layers: more vulnerable to weathering.
- Joints and bedding planes: allows increase in water penetration.
Factors affecting weathering: rock type BDS
- Basalt: often highly weathered
- Dolerite: joints allow water penetration
- Slate: chemically resistant