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Changing Earth's Surface

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Deposition changes the shape of the land Wearing Down and Building Up Weathering, erosion, and deposition act together in a cycle that wears down and builds up Earth ... – PowerPoint PPT presentation

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Title: Changing Earth's Surface


1
Changing Earth's Surface
2
Wearing Down and Building Up
  • Erosion is the process where natural forces move
    weathered rock and soil from one place to
    another.
  • A landslide is a very rapid type of erosion.
  • Other types of erosion move soil and rock more
    slowly.
  • Gravity, running water, glaciers, waves, and wind
    can all cause erosion.

3
Wearing Down and Building Up
  • The material moved by erosion is sediment.
  • Both weathering and erosion produce sediment.
  • Deposition occurs where the agents of erosion lay
    down sediment.
  • Deposition changes the shape of the land

4
Wearing Down and Building Up
  • Weathering, erosion, and deposition act together
    in a cycle that wears down and builds up Earth's
    surface.
  • Where does erosion and deposition occur?
  • Erosion and deposition are at work everywhere on
    Earth.
  • Sometimes they work slowly.
  • At other times, they work quickly.
  • Erosion and deposition are never-ending.

5
Mass Movement
  • Gravity is the force that moves rock and other
    materials downhill.
  • Gravity causes mass movement.
  • Mass movement can be rapid or slow.
  • The different types of mass movement include
  • Landslides
  • Mudslides
  • Slump
  • Creep

6
Landslides
  • The most destructive kind of mass movement is a
    landslide, which occurs when rock and soil slide
    quickly down a steep slope
  • Landslides can be dangerous

7
Mudflows
  • A mudflow is the rapid downhill movement of a
    mixture of water, rock, and soil.
  • The amount of water in a mudflow can be as high
    as 60 percent.
  • Mudflows often occur after heavy rains in a
    normally dry area
  • Mudflows can be very dangerous.

8
Slump
  • Slump is when a mass of rock and soil suddenly
    slips down a slope.
  • Unlike a landslide, the material in slump moves
    down in one large mass
  • Slump often occurs when water soaks the base of a
    mass of soil that is rich in clay.

9
Creep
  • Creep is the very slow downhill movement of rock
    and soil. You can barely notice it.
  • Creep often results from the freezing and thawing
    of water in cracked layers of rock beneath the
    soil.
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