Unfinished
Weathering
The process by which exposed rocks are broken down
Scree
Angular sediment that collects at the foot of a mountain range or cliff
Freeze-thaw
Physical weathering- Caused by expansion of water as it freezes, exerting pressure on the rock as the process repeats
Salt crystallisation
Breakdown of rock by expansion and contraction of salt crystals due to fluctuating temperatures above and below 26 degress
Heating and cooling
Expansion and contraction of rock in deserts due to repeated heating and cooling between night and day
Solution
Some minerals in rock require no chemical reaction to be soluble eg rock salt
Chelation
Humus releases organic acids which attack certain minerals
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
Carbonation
Dissolving of rock by acid rain
Oxidation
Oxygen is dissolved in water, the dissolved oxygen forms oxides or hydroxides on contact with rocks and minerals, causing rust
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
Exfoliation
Pelling off of the top layer of rock
Wetting and drying
Expansion and contraction of rock due to addition and removal of rock
Denudation
Weathering and erosion working together causing landscapes to be worn down
Regolith
Weathering breaks down a rock surface to produce a pile of loose debris
Physical biological
Plant roots seeking out joints and bedding planes. Animals digging holes in rocks
Chemical biological
Humic acids, Bird droppings can be acidic
Aspect
Direction of a slope impacts temperature, south facing slopes are warmer in winter and will experience more freeze-thaw action
Relief
Gradient of slopes, steeper slopes with more exposure will weather faster
Desertification
The process of fertile land becoming desert