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Guided Notes about Weathering
Section 7.1
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Weathering Weathering is the process by which rocks on or near Earth’s surface break down and change.
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Erosion Erosion is the removal and transport of weathered material from one location to another.
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There are two types of weathering:
Mechanical Chemical
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Mechanical Weathering
Mechanical weathering is the process by which rocks break down into smaller pieces. It is also called physical weathering and doesn’t involve any change in the rock’s composition.
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Water Water is the most important agent of mechanical weathering, but wind also plays a role.
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Two factors influence the amount of mechanical weathering that will occur:
Temperature Pressure
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Chemical Weathering Chemical weathering is the process by which rocks and minerals undergo changes in their composition as a result of chemical reactions.
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There are four agents of chemical weathering:
Water Oxygen Carbon dioxide Acid precipitation
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Four factors affect the rate of weathering:
Climate Rock type Surface area Topography
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Climate Climate plays a role in weathering because certain climates encourage different types of weathering. Chemical weathering occurs most readily in warm, humid climates. Physical weathering occurs most readily in cool, dry climates.
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Sedimentary Rocks Sedimentary rock types are more easily weathered than any other type of rock.
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Surface area As the surface area of a rock increases due to weathering, the rate of weathering also increases.
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Topography Rocks that are located on a slope are more likely to be weathered because gravity can cause them to move more readily.
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