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Mass Movements
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Weathering and Erosion
Order Weathering Erosion Deposition Weathering breaks down the rocks, erosion moves the particles, and deposition drops the sediments in another location. Badlands National Park, South Dakota
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Erosion Erosion – the process where sediments are transported by: Wind
Gravity Glaciers Running water Living Things
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Mass Movement: Creep Slow, steady, downhill flow of loose materials – 3 cm/year Oops!
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Mass Movement: Slides Rapid, downslope movement of layer of loose material Often in areas with steep topography NOT just due to water! Ex. landslide
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Mass Movement: Avalanche
Landslides of snow on steep slopes Can be very high speeds – 300 km/hr! (200mph)
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Mass Movement: mudflow
Swiftly moving mixtures of mud and water Triggered by earthquakes, heat from volcanoes, melting snow, and rainstorms
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Mass Movement: Slump Landslide along a curved surface
Common after rains along steep slopes
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Glacial Erosion Glacier: large, moving mass of ice
Cover 10% of Earth’s surface Great size, weight and density slowly moving grind out bedrock
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Glacier Formation Form near the poles and at high elevations
Accumulation of snow – increases each year Weight of top layers exerts downward pressure forcing snow below to re-crystallize into ice
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If Formed in Valley: Snow accumulation causes glacier to become heavy and to flow downhill, due to gravity Speed affected by slope, temperature, thickness of ice and valley shape – 1mm/day
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Valley Glaciers Carve out U-shaped valleys from bedrock
Change valleys from a V shape to a U shape
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Valley Glaciers Cirque - deep depression carved out at the head of a glacial valley. Moraine - rock piles deposited from melted glaciers
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Quiz You can use your rock cycle cheat sheet and this set of notes on your quiz today
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