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Weathering and Soils

AB
Angle of ReposeThe greatest angle that a material can remain stable.
Chemical WeatheringChanges in the rocks chemistry to break it down.
CreepDownward movement of material.
Debris FlowRapid movement of soil and Regolith containing large amounts of water.
Differential WeatheringThe idea that different surfaces weather at different rates.
EarthflowMovement of soils and Regolith from a saturated soil in a tear drop form.
EluviationThe washing out of fine soil components.
ErosionMovement of materials though wind, water, or ice.
Exfoliation DomeThe unloading of rocks off massive plumes.
External ProcessWeathering, mass wasting, and erosion are part of this process.
FallWhen large pieces of whole rock are released.
FlowMaterials move as a fluid down a surface.
Frost WedgingThrough the expansion of water in a closed system.
HorizonDifferent soil zones that can be observed.
HumusDecayed remains of plants and animals.
LaharMovement like a debris flow for volcanoes.
LateriteHot and wet tropical weathered soils.
LeachingDepletion of soluble materials within a soil.
Mass WastingTransfer of rock down a side because of gravity.
Mechanical WeatheringThe physical breaking of down of rock.
Parent MaterialThe mineral matter that is the base for the other soils.
PedalferCollection of iron oxides within the soil.
PedocalCalcium carbonate soils.
PermafrostGround that is permanently frozen
RegolithWeathered rock layer around the Earth.
RockslideSudden movement of rock materials as they move down a surface.
Secondary EnrichmentConcentration of metallic ores as a result of weathering.
SheetingWhere large slabs of rock are unloaded.
SlideWhere materials remain similar and move along a surface.
SlumpMovement of material along a curved surface.
SoilCombination of mineral and organic material
Soil ProfileA collection of soil horizons.
Soil TextureThe different sized particles inside of the soils.
SolifluctionA specific type of creep in areas of permafrost.
SolumTrue soil, layers O,A,E, and B.
Spherodial WeatheringThe changing of blocking rock to a more spherical shape.
Talus SlopeThe remains rocks from frost wedges weathering.
WeatheringDisintegration and decomposition of rock materials at the Earth’s surface.


Agricultural Education Instructor and FFA Advisor
Audubon Community Schools
Audubon, IA

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