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Where Does the “Stuff” Go?
Erosion & Deposition Where Does the “Stuff” Go?
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Definitions Erosion: Deposition:
Removal and transport of weathered material from one location to another. Deposition: Materials are left behind in another location (final stage)
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5 Agents Gravity Running Water (most overall erosion)
Glaciers (most powerful) Wind (least powerful) Plants/Animals
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Gravity Pulls materials down slope
Forces sediment to settle during deposition Examples: glaciers, streams, landslides, mudflows, avalanches
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Gravity Get image of mass wasting
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Water Faster flow = More erosion
Rill Erosion- small channels on the side of a slope Gully Erosion- channel becomes deep and wide (3m deep)
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The Grand Canyon
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Rill & Gully Erosion Gully Rill
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Stream Erosion
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Stream Erosion Erosion occurs upstream (towards the headwaters)
Diagram of a stream system
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Stream Deposition Deposition occurs downstream (towards the mouth)
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Coastal Erosion/Deposition
Currents, waves and tides carve out cliffs, arches, etc. Constant water movement causes constant erosion especially at shorelines
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Water Image of a calm stream
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Water Image of turbulent river
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Water
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Water
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Stream Deposition Delta: build up of stream sediments at the mouth
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Glaciers Can scratch, grind, polish, gouge out large sections
Glaciers currently cover less than 10% of Earth’s surface, but have a huge effect
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Glacier
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Glaciers Image of alpine glacier
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Yosemite Valley
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Yosemite Valley
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Wind Erosion Erosion by abrasion
Hot dry areas w/ little vegetation to hold soil Wind barriers (breaks): trees planted perpendicular to wind, trap snow, conserve moisture
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Wind
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Wind Erosion – Arches Nat’l Park
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Plants, Animals & Humans
Animals burrow Humans excavate (garden, build athletic fields, build highways)
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