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Weathering and Erosion
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Weathering The breakdown of the materials of the Earth’s crust into smaller pieces, due to exposure to the atmosphere
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Mechanical (Physical) Weathering
The process by which rocks are broken down into smaller pieces, without changing its composition. Types of mechanical weathering: Frost (ice) heaving and frost (ice) wedging Plant roots Wetting and drying (swelling/shrinking) Friction and impact Burrowing of animals
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Frost (Ice) Wedging
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Frost (Ice) Heaving
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Plant Roots
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Friction and Repeated Impact
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Burrowing of Animals
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Chemical Weathering The process that breaks down rock through chemical changes. The agents of chemical weathering Water Oxygen Carbon dioxide Living organisms Acid rain
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Water Water weathers rock by dissolving it
Water combines with some minerals (eg. Feldspar) to produce clay Chemical reaction of water with other substances is called hydrolysis
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Oxygen Iron combines with oxygen in the presence of water in a processes called oxidation The product of oxidation is rust
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Carbon Dioxide CO2 dissolves in rain water and creates carbonic acid
Carbonic acid easily weathers limestone and marble
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Living Organisms Lichens that grow on rocks produce weak acids that chemically weather rock Acids are formed when plants and animals decay
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Acid Rain Compounds from burning coal, oil and gas react chemically with water forming acids. Acid rain causes very rapid chemical weathering
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Rate of Weathering Several factors determine the rate at which rock weathers: Wet vs. dry climates The composition of the rock (what minerals it contains) The amount of surface area exposed
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Bryce Canyon (Utah) -rocks of different resistance weather at different rates.
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Erosion The process by which water, ice, wind or gravity moves fragments of rock and soil.
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Water Erosion Rivers, streams, and runoff
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Ice Erosion Glaciers
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Wind Erosion
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Mass Movements Landslides, mudslides, slump and creep
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