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Weathering Topic 9 Regents Earth Science
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Weathering The break down of rock material as a result of chemical and/or physical action
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Physical weathering aka mechanical weathering The breakdown of rock into smaller pieces without chemical change
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1. Frost action Weathering of rock by the alternate freezing and thawing of water in the pores or cracks in the rock
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Frost Wedging
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2. Plant action Occurs when cracks in rock are widened by the forces exerted by growing plants
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Plant Action
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3. Pressure unloading Occurs when rocks split along the planes of weakness when the pressure of overlying material is removed Usually occurs as the result of natural processes such as landslides, erosion, and earthquakes But humans also cause this through quarrying and mining
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4. Abrasion The physical action of scraping, rubbing, grinding, or wearing away of rock surfaces due to the movement of solid sediment in an erosional system such as stream or wind
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*As time increases, particles become more rounded.*
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5. Exfoliation The scaling or peeling of successive shells from the surface of rocks Generally occurs in coarse-grained rocks that contain feldspar (like granite)
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Pressure Unloading and Exfoliation
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Chemical weathering aka decoposition The breakdown of rock by chemical action, during which there is a change in chemical composition of the minerals in the rock
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The agents of chemical weathering include
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1. oxygen The chemical reaction of oxygen with another element is called oxidation
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2. water Speeds up chemical reactions Dissolves many materials Reacts directly with many mineral substances (hydrolysis)
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Caves form
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3. Carbon dioxide Easily dissolves in water to form carbonic acid Calcite, limestone, and marble react with carbonic acid Reaction of carbonic acid with other substances is known as carbonation
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Sinkhole
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4. acids Produced in the atmosphere by lightning and on the surface by decay of organic wastes Also gases released by people and industry combine with water to form acids
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