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Biological weathering
Breakdown of rock due to living organisms such as plant roots, burrowing animals, or humans.
Chemical weathering
The decomposition of rocks by chemical processes
Carbonation
Rainwater reacts with carbonate rocks
Oxidation
Reaction of iron-rich rocks with oxygen, leading to rust and weakening.
Solution
Dissolving of minerals in rock by water.
Exfoliation
A type of physical weathering in hot climates where rocks expand during the day and contract at night, causing layers to peel off
Mass movement
The downslope movement of rock and soil under gravity
Creep
Slow movement of soil down gentle slopes.
Flow
Movement of saturated soil down moderate slopes.
Slide
Rapid movement of material along a plane.
Slump
Rotational movement of saturated material on a curved surface.
Fall
Sudden dropping of rock fragments from steep slopes
Salt crystallisation
A weathering process where salt crystals expand in rock pores, exerting pressure and causing the rock to break apart.
Wetting and drying
Physical weathering process where rock expands when wet and contracts when dry, causing cracks to form.