Weathering Processes and Types

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This set of vocabulary flashcards covers the definitions, agents, examples, and climatic conditions associated with physical, chemical, and biological weathering as described in the lecture notes.

Last updated 8:45 AM on 7/19/26
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15 Terms

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Physical Weathering

The disintegration of rock without any change in its chemical composition, often occurring in cold and arid climates.

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Chemical Weathering

The process by which chemicals in rainwater react with minerals in rocks, causing them to decompose or change their mineral composition.

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Biological Weathering

The breakdown of rocks caused by the growth and activities of living organisms such as plants, animals, and microbes.

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Wind Weathering

Weathering caused by the blowing of grains of sand against a rock surface.

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Rain and Wave Weathering

Weathering that occurs by slowly wearing rock away over long periods of time.

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Acidic Rainwater

Rainwater that has dissolved CO2CO_2 from the air, making it slightly acidic and capable of reacting with minerals in rock.

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Root Weathering

A biological process where plant roots grow into rocks causing cracks and produce acidic juices that break down rock material.

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Burrowing Animals

Animals such as rabbits and rats that contribute to biological weathering by loosening and breaking rocks through their activities.

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Physical Weathering Agents

The main forces involved in disintegration, including temperature, frost, and pressure.

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Chemical Weathering Agents

The main substances involved in decomposition, including water, oxygen, CO2CO_2, and acids.

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Physical Weathering Examples

Common processes such as frost action and exfoliation.

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Chemical Weathering Examples

Specific chemical reactions including carbonation, oxidation, and hydrolysis.

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Biological Weathering Examples

Specific instances of life-driven breakdown such as root wedging and the production of organic acids.

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Cold and Arid Climate

The typical climate environment where physical weathering is most common.

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Hot and Humid Tropical Climate

The typical climate environment where chemical weathering is most prevalent.