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Weathering
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What is Weathering?
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The process by which rocks and minerals at the Earth's surface are physically and chemically broken down.
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Types of Weathering
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Mechanical Weathering Disintegration
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Breaks rock into smaller pieces.
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Abrasion Physical wearing and grinding of a surface through friction.
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Mushroom Park
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Animal & Plant Lichen works very slowly to break down granite boulders.
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Exfoliation The peeling away of large sheets of loosened materials at the surface of a rock.
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Frost Wedging
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Mt Brewer in the Sierra Nevada
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The east ridge of Mt. Brewer
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Lab: Frost Wedging
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Chemical Weathering Decomposition
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Rocks are changed into different materials.
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Usual Suspects
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Oxygen
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Oxidation
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Acid Rain
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Lab: Acid Rain
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Water Weathering
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Lab: Effects of Weathering on Various Minerals
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Lab: Observe the Chemical Weathering of Feldspar
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Mechanical vs. Chemical Mechanical Weathering Changes the size of the rock. Chemical Weathering Changes the composition of the rock.
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Factors That Control Weathering Surface Area
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Surface Area
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Lab: Surface Area vs. Size & Shape
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Lab: Chemical Weathering vs. Surface Area
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Factors That Control Weathering Composition of Rock
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Climate
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Lab: Temperature vs. Chemical Weathering
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Erosion & Mass Movements
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Erosion Removal and transport of materials by wind & running water.
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Mass Movement Downward transportation of weathered materials by gravity.
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Soil Earth’s Life Supporting Material.
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Soil Profile
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Soil Profile vs. Time
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Soil Age
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Soil Composition Refers to the proportions of different particle sizes in the soil.
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Sand (less than 2 mm) Silt (less than 1/16 mm) Clay (less than 1/256 mm)
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Sandy soils are light and typically very free draining, usually holding water very poorly due to very low organic content. Clay soils tend to be heavy and difficult to work when dry. Clay soils tend to allow virtually all water to run-off.
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Soil Texture Triangle
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30% clay 20% silt 50% sand 10% clay 70% silt 20% sand 50% clay 20% silt 30% sand Sample A Sample B Sample C Sand Clay Loam Silty Loam Clay
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Lab: Are You My Type?
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Lab: Soil Texture Feel Test
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Soil Texture Feel Test 1 Place about 2 teaspoons of soil in your palm. Add water drop by drop and knead soil until it is moldable and feels like moist putty.
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Does the soil remain in a ball when squeezed?
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Soil Texture Feel Test 1 SAND No Yes Move to Soil Texture Feel Test 2!
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Soil Texture Feel Test 2 Place the ball of soil between your thumb & forefinger. Gently push the soil with thumb, squeezing it upward into a ribbon. Allow the ribbon to emerge and extend over your forefinger until it breaks from its own weight.
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Does the soil form a ribbon?
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LOAMY SAND No Yes Move to Soil Texture Feel Test 3!
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Soil Texture Feel Test 3A Does the soil make a weak ribbon (<1inch long) and feels gritty?
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LOAM or SILT LOAM No Yes SANDY LOAM
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Soil Texture Feel Test 3B Does the soil make a medium ribbon (1-2 inch long) and feels gritty?
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CLAY LOAM or SILT CLAY LOAM No Yes SANDY CLAY LOAM
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Soil Texture Feel Test 3C Does the soil make a strong ribbon (>2 inch long) and feels gritty?
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CLAY No Yes SANDY CLAY
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Porosity Porosity is the percentage of void space in a rock.
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Soil Porosity
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Lab: Soil Porosity
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Lab: Soil Permeability
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Soil Erosion
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Causes of Soil Erosion
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Contour Farming
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Strip-Cropping
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Windbreaks
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Terraces
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