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Erosional Forces

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Erosional Forces Erosion Wearing away of surface materials by gravity, water, wind, or glaciers. Deposition- process where sediments are dropped by erosion agents as ... – PowerPoint PPT presentation

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Title: Erosional Forces


1
Erosional Forces
2
  • Erosion
  • Wearing away of surface materials by gravity,
    water, wind, or glaciers.
  • Deposition- process where sediments are dropped
    by erosion agents as they lose energy.

3
  • Mass movement occurs as gravity moves materials
    down a slope as one large mass.
  • Examples Slumping, Creeping, Rock
    Falls/Slides, Mudflows
  • Steep slopes can be made safer with vegetation,
    drainage pipes, and walls of concrete or railroad
    ties.

4
  • Glaciers
  • Large masses of ice and snow that slowly move on
    land causing erosion.
  • Plucking- erosion process caused by moving
    glaciers picking up boulders, gravel, sand.
  • Scour scrape the soil and bedrock.
  • Grooves striations indicate the direction a
    glacier moved.

5
  • Glaciers deposit a mixture of different sized
    sediments (till) when they retreat.
  • Moraine- a ridge, or pile, of deposit left at the
    end of a glacier.
  • Outwash- material deposited in layers by the
    meltwater of a glacier, with largest
    pieces closer to the glacier..
  • Eskers outwash deposit formed as
    meltwater rivers within the ice deposit sand
    gravel within their channels.

6
Zone of Accumulation
Snowline
Crevasses
Zone of Wastage
7
  • Types of Glaciers
  • Continental Glaciers-huge masses of ice and snow
    that cover large areas of land.
  • Covers 10 of Earth near the poles. (Antarctica
    Greenland)
  • Ice Ages - periods of widespread glaciation over
    the last 2 to 3 million yrs.
  • Thicker than some mountain ranges.

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  • Valley Glaciers- exist in mountain ranges.
  • Cirques- bowl-shaped basins in the sides
    of mountains.
  • Arête- a long ridge that forms when two
    valley glaciers erode a mountain side-by-side.
  • Peaks- form when valley glaciers erode a
    mountain from several directions.
  • Valleys formed by glaciers are U shaped

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11
  • Wind
  • Scatters dust or volcanic ash over thousands of
    kilometers.
  • Deflation- wind removes small particles of
    loose sediment, leaving behind heavier materials.
  • Abrasion- wind behaves like a sandblaster
    blowing sand grains against rocks wearing them
    down.

The
12
  • Windbreaks rows of trees planted to slow down
    wind in order to reduce erosion.
  • Dunes mounds of sediment drifted by wind.

13
Water Erosion
14
  • Surface Water
  • Runoff
  • Rainwater that doesnt soak in to the ground or
    evaporate.
  • Affected by
  • Amount of rainfall
  • Length of time it falls
  • Steepness, or slope, of the land
  • Amount of vegetation

15
  • Rivers Streams
  • River system network of groundwater
    streams that come together to form a system.
  • Drainage Basin- area of land from which a stream
    or river collects runoff.
  • The Mississippi River drainage basin is the
    largest in the United States

16
  • Young River
  • Flows swiftly through a narrow valley.
  • May have rapids waterfalls.
  • Erodes the bottom faster than the sides.
  • V shaped valleys

17
  • Mature Stream
  • Flows smoothly through the valley.
  • Erodes more on the sides.
  • Forms meanders oxbow lakes.
  • Carves a flat, broad valley floor called a
    floodplain.

18
  • Old Stream
  • Flows smoothly through a floodplain it has
    carved.

19
flood plain
meanders
oxbow lake
valley wall
20
  • Delta fan shaped area formed by sediments that
    are deposited as water empties into an ocean or
    lake.
  • Alluvial Fan fan shaped area formed by
    sediments that are deposited as water empties
    from a mountain valley onto a flat open plain.

21
  • Groundwater
  • Groundwater is water that soaks into the ground
    and collects in the pores of the underlying soil.
  • Soil and rock are permeable if water can pass
    through the pore spaces. (Sandstone)
  • Soil and rock are impermeable if water can not
    pass through the pore spaces. (Granite)
  • Aquifer a layer of permeable rock that
    lets water move freely.
  • Zone of Saturation area where all the pores are
    filled with water.
  • Water Table upper surface of the zone of
    saturation.

22
Aquifer
Zone of Saturation
Zone of Aeration
Water Table
23
  • Wells are used to pump groundwater from an
    aquifer to the surface.
  • Artesian wells wells that dont require a pump
    because the water is under pressure.
  • Spring free flowing water because the water
    table is so close to the surface.
  • Geyser hot spring that erupts peroidically,
    shooting water steam into the air.

The the
24
  • Caverns are formed by Carbonic acid dissolving
    limestone rock, thereby enlarging cracks to form
    chambers.
  • Stalactites Calcium carbonate deposits that hang
    from a caves ceiling.
  • Stalagmites Calcium carbonate deposits that
    form on a caves floor.

25
Other Features
Soda Straws
Columns
Cave Popcorn
Draperies
Cave Pearls
26
  • Ocean Shoreline
  • Shoreline Forces
  • Waves pound against pound against shores.
  • Currents move sediments along the shoreline.
  • Tides carry sediment out to sea bring in new
    sediment.

27
  • Rocky Shorelines
  • Rocks cliffs
  • C. Sandy Beaches
  • Beaches deposits of sediments parallel to the
    shore.
  • Barrier Islands fragile sand deposits that
    parallel the shore but are separated from the
    mainland.
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