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20 Terms
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Weathering
The process by which exposed rocks are broken down
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Scree
Angular sediment that collects at the foot of a mountain range or cliff
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Freeze-thaw
Physical weathering- Caused by expansion of water as it freezes, exerting pressure on the rock as the process repeats
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Salt crystallisation
Breakdown of rock by expansion and contraction of salt crystals due to fluctuating temperatures above and below 26 degress
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Heating and cooling
Expansion and contraction of rock in deserts due to repeated heating and cooling between night and day
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Solution
Some minerals in rock require no chemical reaction to be soluble eg rock salt
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Chelation
Humus releases organic acids which attack certain minerals
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Hydration
Water is absorbed into the crystal structure of the mineral within a rock. The water absorption allows the minerals to swell and creates stresses, water within the crystal structure causes chemical changes
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Carbonation
Dissolving of rock by acid rain
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Oxidation
Oxygen is dissolved in water, the dissolved oxygen forms oxides or hydroxides on contact with rocks and minerals, causing rust
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Hydrolysis
Carbonic acids release H+ ions from water, which combine with some minerals in rock (feldspar) which releases Na, K, Mg. Minerals within the rock now disintegrate
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Exfoliation
Pelling off of the top layer of rock
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Wetting and drying
Expansion and contraction of rock due to addition and removal of rock
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Denudation
Weathering and erosion working together causing landscapes to be worn down
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Regolith
Weathering breaks down a rock surface to produce a pile of loose debris
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Physical biological
Plant roots seeking out joints and bedding planes. Animals digging holes in rocks
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Chemical biological
Humic acids, Bird droppings can be acidic
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Aspect
Direction of a slope impacts temperature, south facing slopes are warmer in winter and will experience more freeze-thaw action
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Relief
Gradient of slopes, steeper slopes with more exposure will weather faster