Weathering and Erosion

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Presentation transcript:

Weathering and Erosion

Objective: 2.1.3 I can explain how natural actions such as weathering, erosion (wind, water and gravity), and soil formation affect Earth’s surface.

What is Weathering? Is the breaking down and changing of rocks near Earth’s surface Two Types Mechanical Chemical

What is Mechanical Weathering? When physical forces break rock into smaller pieces Does not change the rock’s composition Three Ways Frost Wedging Unloading Biological Activity

Mechanical Weathering: Frost Wedging Water enters cracks and crevices in rocks Water freezes expanding the cracks Eventually breaking rocks into pieces

Mechanical Weathering: Unloading The uplift and weathering of rocks overlying igneous rocks Why? Pressure on igneous rocks is reduced causing uplift Exfoliation: slabs of outer rock separate and break loose

Mechanical Weathering: Biological Activity Activities of living organisms Example: Plant roots wedge into rocks, breaking them apart

What is Chemical Weathering? Is the transfer of rock into one or more new compounds

Agents of Chemical Weathering Water Most important agent Picks up gases from the atmosphere Oxygen Causes oxidation of metal minerals Ex: rusting

Chemical Weathering in Action Carbon Dioxide Combines with water in the atmosphere Causes acids to form like in acid rain Spheroidal Weathering Causes the corners and edges of rock to be rounded

Rate of Weathering What affects it? Rock Characteristics Mineral composition Mineral solubility Climate Temperature and moisture Favors high temperatures and abundant moisture

What is Erosion? Removal and transport of weathered material from one location to another

Agents of Erosion

Agents of Erosion Running Water Wind Glaciers Ocean currents and Waves Biological Organisms

What happens to the Material? Deposition Materials are dropped in another location Final stage of erosion

How does Wind Erode Soil? Picks up and carry sediment Sand Dunes Mounds or ridges of sand Wind also can cause them to move

How can humans control erosion? Planting rows of trees called windbreakers Terracing hillsides Plowing along the contours of hills Rotating crops

What is Soil? Part of the regolith that supports the growth of plants Layer of rock and mineral fragments that cover most of Earth’s land surface

How is Soil Formed? Weathering of rocks that is carried away Factors Parent Material Time Climate Organisms Slope

Soil Formation Factors Time Important in all geologic processes The longer a soil has been forming, the thicker it will become Parent Material Source of the mineral matter in the soil

Organisms Climate Slope Furnish organic matter in soil Steep slopes often have poorly developed soils Climate Greatest effect on soil formation Influences of temperature and precipitation affect rate, depth and type of weathering

Characteristic of Soil: Soil Composition 45% mineral matter 25% air 25% water 5% humus Decayed remains of organisms

Characteristic of Soil: Soil Texture Refers to the proportions of different particle sizes Sand (large size) Silt (feels like flour) Clay (small size) Loam (mix of all three; best for plants)

What is Mass Movement? The transfer of rock and soil down-slope due to gravity

How to Classify Mass Movement? Classified by Kind of material the move How it Moves Speed of movement

Mass Movement Types Landslides Mudslides Tsunamis Earthquakes Slumps

Why mass movements are more frequent? Decreased soil stability Droughts Less vegetation Increased storms

Human Preventions of Mass Movements Increasing soil stability: Increasing vegetation Contouring (maintaining) the landscape Effective irrigation

Word Sort Activity Using your vocabulary cards, arrange them into groups of 3 (there should be at least 3 groups, Max 5) based on their meaning and relatedness. On the back of your question sheet, write your three groups (include the vocabulary words for each group) and write 2-4 sentences discussing how they are related (BE SPECIFIC)