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Earth Science

Chapter 3 Weathering, Soil, and Mass Wasting

AB
WeatheringThe physical breakdown and chemical alteration of rocks at or near Earth's surface
Mass Wastingthe transfer of rock and soil dowslope under the infunence of gravity
Erosionthe physical removal of material by mobile agents as water, wind, or ice
Mechanical Weatheringthe physical forces that break rock into smaller and smaller pieces without changing the rock's mineral transformation
Chemical Weatheringthe chemical transformation of rock into one or more new compounds
Frost Wedgingthe process of many freeze-thaw cycles the rock is broken into pieces
Talus slopesThe sections of rock are wedged looses and may tumble into large piles
Sheetinga process when large masses of igneous rock most granite, are exposed by erosion, slabs begin to break loose like the layers of an onion
Exfoliation domesthe outer layers expand more than the rock below and thus separate from the rock body and the continued weatherubg eventually causes the slabs to separate and spall off
Biological activitythe activites of organisms, including plants, burrowing animals, and humans.
Regoliththe layer of rock and mineral fragments produced by weathering
Soilthe combination of mineral and organic matter, water,and air
Soil Textureproportions of different particle sizes which influences the soil's ablilty to retain and transit water, air
Horizonssoil into zones or layes
Eluviationthe washing out of the fine soil components
Leachingthe depletion of soluble materials from the upper soil
Lateritesoils in hot, wet tropical climates

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