Rocks and weathering 3.2 Flashcards

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1
Q

What is weathering?

A

The decay and disintegration of rocks.

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2
Q

Physical weathering: freeze thaw

A
  • 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.
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3
Q

Physical weathering: thermal fracture

A
  • Large ranges in temperature in deserts cause rocks and minerals to expand and contract, resulting in disintegration.
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4
Q

Physical weathering: salt crystal growth

A
  • 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%.
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5
Q

Physical weathering: pressure release

A
  • Process when ground surface is lowered by erosion which reduces weight of load.
  • This leads to expansion of rocks below which forms cracks.
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6
Q

Chemical weathering: hydrolysis

A
  • 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.
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7
Q

Chemical weathering: hydration

A

Wetting and drying of rocks adds and removes water causing expansion or contraction.

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8
Q

Chemical weathering: carbonation

A
  • Process which affects carbonate minerals where rainwater containing carbonic acid attacks carbonate minerals.
  • This forms chalk and limestone.
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9
Q

Chemical weathering: organic action

A
  • Process of roots working their way into cracks in rocks.

- As roots become bigger, cracks widen and deepen, breaking up bedrock.

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10
Q

Which 5 factors affect weathering?

A
  • Climate
  • Vegetation
  • Relief
  • Rock structure
  • Rock type
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11
Q

Factors affecting weathering: climate

A
  • Determines which weathering processes occur and rate at which they occur.
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12
Q

Factors affecting weathering: vegetation

A
  • Type: larger vegetation such as trees are more likely to break apart rocks with larger roots.
  • Structure: high density of vegetation increases organic action
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13
Q

Factors affecting weathering: relief

A
  • Steep: types of weathering caused by rain is less prevalent
  • Gentle: subjected to standing water and infiltration which increases rates of weathering.
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14
Q

Factors affecting weathering: rock structure

A
  • 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.
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15
Q

Factors affecting weathering: rock type BDS

A
  • Basalt: often highly weathered
  • Dolerite: joints allow water penetration
  • Slate: chemically resistant
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