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mass wasting
the transfer of rock and soil downslope under the influence of gravity
erosion
the physical removal of material by mobile agents such as water, wind, ice, or gravity
types of mechanical weathering
frost wedging, unloading, thermal expansion, biological activity
frost wedging
alternate freezing and thawing of water in fractures and cracks promotes the disintegration of rocks
unloading
exfoliation of igneous and metamorphic rocks at the Earth’s surface due to a reduction in confining pressure
Thermal expansion
alternate expansion and contraction due to heating and cooling
biological activity
disintegration resulting from plants and animals
most important agent involved in chemical weathering
water
chemical weathering processes
dissolution, hydrolysis, oxidation
factors affecting weathering
climate, surface area, rock characteristics
what part of soil supports plant growth
regolith
solum (soil levels)
O, A, E, B, C