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Prentice Hall Interactive Science: Earth Science - Chapter 6 Weathering and Soil

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UniformitarianismGeological principle that the same geological process that operated in the past to change earth’s surface is the same one working now
ErosionProcess by which water ice and wind and gravity move particles of rock and soil
WeatheringChemical and physical process that breaks down rock and other substances
Mechanical weatheringRock is physically broken into smaller pieces
Chemical weatheringProcess that breaks down rock through chemical changes
AbrasionGrinding away of rock by other rock particles carried in water, ice or wind
Frost wedgingSplits rock, water seeps into cracks freezes and expands
OxidationSubstance combines with oxygen, as when iron oxidized, forming rust
PermeableCharacteristic of a material that contains connected arir spaces or pores that water can seep through
SoilLoose weathered material on Earth’s surface in which plants grow
BedrockRock that makes up Earth’s crust; also the solid rock layer beneath the soil
HumusDark-colored organic material in soil
LoamRich, fertile soil made up of about equal parts of clay, sand, and silt
TopsoilCrumbly, topmost layer of solid made of clay and other minerals
SubsoilLayer of soil below topsoil w/ less plant and animal, contains mostly clay and other minerals
DecomposerOrganism that gets energy by breaking down biotic wastes and dead organisms and returns raw materials to soil and water
Soil conservationThe management of soil to limit its destruction
Crop rotationPlanting of different crops in a field of each year to maintain soil’s fertility
Contour plowingPlowing fields along curves of a slope to prevent soil loss
Conservation plowingSoil conservation method in which weeds and dead stalks from the previous year’s crop are plowed into ground


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