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G2: Weathering and Soil Formation/definitions

AB
weatheringthe process by which rock materials are broken down by physical and chemical processes
mechanical weatheringthe breakdown of rock by physical means such as abrasion, wind, water, and gravity
frost actionthe alternate freezing and thawing of soil and rock
ice wedginga type of frost action where water seeps into rocks, freezes, then expands
abrasionthe grinding and wearing away of rock surfaces through mechanical weathering
chemical weatheringthe process by whick rocks break down as a result of a chemical process like exposure to water, acids, or air
acid precipitationrain, sleet or snow that contains a high concerntration of acids
karst featurea limestone cavern
oxidationthe chemical reaction in which an element is exposed to moisture and air
differential weatheringsofter, less weather resistant rock is worn away, and leaves harder rock behind
soilloose mixture of small mineral fragments, organic material, water, and air that can support the growth of vegetation
parent rockrock that is the source of soil
bedrocklayer of rock beneath the soil
residual soilsoil that remains above its parent rock
transported soilsoil that is blown or washed away from parent rock
soil texturethe soil quality that is based on porportions:% of soil types that make up the soil
soil structurethe arrangement of the particles that make up the soil
infiltrationthe ability of water to flow through a soil
humusdark, organic material in soil
soil horizonslayers of soil that are formed
leachingthe removal and transport of substances that can be dissolved by the passing of water
soil conservationa method to maintain the fertility of soil: keeps soil safe from erosion and nutrient loss
erosionthe process by which wind, water, ice, and gravity move soil and sediment from one place to another
land degredationwhen soil becomes infertile from overuse
desertificationwhen a fertile area becomes a desert
contour plowingwhen a farmer plows rows across the slope of the hills
terracingplowing land so that one steep hill becomes a series of smaller hills
no-till farmingleaving old stalks in the fields
cover cropscrops that are planted between harvests to replace nutrients and prevent erosion
crop rotationplanting diffent crops in the same field from year to year.


St. James Catholic School
Millstadt, IL

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