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Erosion, Deposition AND SOIL FORMATION
Actions That Change Earth’s Surface
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Weathering: a review… Physical or Chemical processes that break down rocks. Mechanical weathering: ice wedging, root pry, exfoliation, etc. Chemical weathering: oxidation (iron + oxygen + water = rust), acid precipitation (from burning fossil fuels: sulfur, carbon dioxide, and nitrogen), plant acids (lichens)
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What affects the rate of weathering?
The type of rock: mineral composition Surface area: smaller rocks have a greater surface area and weather faster Climate (temperature and precipitation): hot/warm and wet/humid weather fastest
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What is erosion? Erosion is the transport (movement) of weathered rocks and sediment from one place to another. Erosion is usually gradual… Humans can speed it up.
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What are the agents of erosion?
Wind Water Waves Glaciers (ice) Gravity (mass movement, mass wasting)
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What is deposition? What goes up must come down.
What is carried must be… dropped. Deposition occurs when agents of erosion deposit (lay down, drop) sediment.
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How does gravity change Earth’s surface?
Rapid Mass Wasting… Landslide Mudflow
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Erosion and Deposition
Gravity- pulls materials downhill Running Water- water has great power Rill erosion- water running in small channels down a slope Gulley- When a channel becomes deep and wide
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How does slow mass wasting erode rocks?
Creep Slump
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How does water change Earth's surface?
Running water Load deposits
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How is a river's load deposited?
Delta Alluvial fan
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How do waves change Earth's surface?
Sand bars Longshore drift
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Coastal Deposition & Erosion
Much of what is weathered is carried to a coast When a river hits the oceans, it slows down, dropping its load of sediment Ocean waves, currents, and tide continue erosion
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How do glaciers change Earth's surface?
Large mass of moving ice and snow Abrasion
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Glacial Erosion Currently Cover <10% of Earth
Very Powerful, polish grind, scratch surfaces Form valleys, waterfalls, lakes
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How does wind change Earth's surface?
Sand dunes
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Wind Erosion Major forces where low precipitation, high temperature and no plant cover = sandblasting
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Plants, Animals and People
Move soil around Buildings, highways, etc.
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Formation of Soil Soil- loose covering of broken rock, decaying organic matter (humus) covering Earth’s surface Soil Formation- Beginning: weathering breaks solid bedrock into smaller pieces Organic (living) matter added; organisms die, decay (decomposers)
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Soil Composition Parent Material- bedrock “gives birth to soil”
Residual Soil- just above parent material Transported Soil- soil moved to a location far away from parent bedrock Think Running Water, Wind, Glaciers
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Soil Profiles- a vertical sequence of layers
Horizons- distinct layers of soil O- All leaf litter, top layer A- organic mixed with rock fragments B- Sub Soil, rich in clay C- between B and bedrock, mostly broken pieces of rock Topography affects thickness of soil, hillsides loose soil to erosion
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Soil Textures Clay- smallest particles Silt- slightly larger
Sand- larger Loam- combination of the three
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Soil Fertility How well a soil can support plant growth Factors
Mineral/nutrients, microorganisms, precipitation, topography and acidity Fertilizer adds nitrates, potassium, phosphorus Legumes (peas and beans) add microorganisms and nitrates to soil as they grow
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What caused the Dust Bowl in the 1930s?
Poor soil conservation…
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