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Weathering and Erosion
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Weathering The gradual breakdown of the materials of Earth’s crust into smaller pieces through chemical or mechanical processes.
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Physical Weathering Process by which rocks are broken down into smaller pieces by external conditions. Types of Physical weathering Frost heaving and Frost wedging Plant roots Friction and impact Burrowing of animals Temperature changes
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Frost Wedging
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Frost Heaving
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Plant Roots
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Friction and Repeated Impact
Breaks off pieces of rock, and gradually forms smooth round rocks found in stream beds or along lake shores.
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Burrowing of Animals
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Temperature Changes
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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 the minerals
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Oxygen Iron contained in rock 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
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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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Karst Topography A type of landscape in rainy regions where there is limestone near the surface, characterized by caves, sinkholes, and disappearing streams. Created by chemical weathering of limestone
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Features of Karst: Sinkholes
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Features of Karst: Caves
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Features of Karst: Disappearing Streams
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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
Delta-a fanlike deposit of sediment where a river enters an ocean/sea.
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Ice Erosion Glaciers-large long lasting mass of ice that moves due to gravity and plucks rocks and boulders and scourers valleys smooth.
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Glaciers Creates U-Shaped valleys
Moraine-piles of rocks that form hills or ridges that are left behind/deposited once a glacier has melted or receded. Kettles- small glacial depressions that fill with water to form small lakes
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Wind Erosion Winds must be 11 mph to move sediment. Dust storms can move 6,000 tons per cubic mile of air. Loess: windblown silt and clay that produces very fertile soil (Mississippi, N. China, Argentina)
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Mass Movements Landslides, mudslides, slump and creep
landslide clip.mpeg
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Building Soil Soil: A loose mixture of weathered rock, organic matter, air, and water that supports plant growth. Humus: organic material in soil Soil quality determines the types of vegetation that can grow.
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Soil Factors Parent Material: chemical composition of the original rock Relief: steep slopes erodes faster Organisms: decomposers help loosen soil Climate: wet/dry, hot/cold = different soils Time: 2.5 cubic cm per 100 years
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