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Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

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Strike-Slip Fault- These form at transform boundaries. ... Strike-slip faults are associated with crustal shear. * Title: Earth s Crust Author: Preferred Customer – PowerPoint PPT presentation

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Title: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.


1
Plate TectonicsLearning GoalComprehend plate
tectonics and apply in lab.
2
Convection currents
3
  • Continental drift idea that continents have
    moved slowly to their current positions due to
    convection currents in the mantle.
  • Pangea the idea that the all land masses on
    earth were once a single large land mass.

4
  • Ocean floor spreading theory that hot less
    dense material below Earths crust rises toward
    the surface at the mid-ocean ridges. Then, it
    flows sideways, carrying the seafloor away from
    the ridge in both directions. http//geology.com/n
    sta/divergent-boundary-oceanic.gif
  • Convection current unequal distribution of heat
    in the mantel causes a net movement in a circular
    motion.

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  • The Earths CRUST is the outer most part of the
    Earths surface.
  • Average 32 km thick (19.84 miles)
  • Thickest point 70 km (in mountains)
  • Thinnest point 8 km (under ocean)

7
  • Plate tectonic theory that Earths crust and
    part of the upper mantle are broken into sections
    called plates.
  • Lithosphere all of the earths crust and part
    of the upper mantle.
  • http//www.allaboutspace.com/subjects/astronomy/pl
    anets/earth/Inside.shtml
  • Asthenosphere plastic like layer below the
    lithosphere. The ridged plates of the lithosphere
    float on the more plastic layer called the
    asthenosphere.

8
  • l

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  • Deformation The breaking, tilting, and folding
    of crustal rock due to crustal movement. (three
    types of forces)
  • Compression squeezing of earths crust that
    compacts the rock. Convergent boundary
  • 2. Tension is the pulling apart of the earths
    crust. Divergent boundary.
  • 3. Shearing pushes rocks side by side in
    opposite directions. Transform boundary.

11
Convergent boundary
Divergent boundary
Transformation boundary
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Rift valley
subduction
14
  • FAULTS
  • Normal Fault (Divergent Boundary) fault caused
    by tension stress that moves the hanging wall
    down relative to the foot wall.

15
  • Fault block mountain is a mountain created by
    blocks of rock uplifted by normal faults.

16
Divergent boundary in Iceland
17
  • Reverse Fault (Convergent Boundary) fault
    caused by compression forces where the hanging
    wall will move up relative to the foot wall.

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In Lateral (strike-slip) faulting (Transform
Boundary), the two blocks move either to the left
or to the right relative to one another.
Strike-slip faults are associated with crustal
shear.
20
San Andreas Fault, CA
21
  • Facts about folds/faults.
  • increased temp. s fold
  • decreased temp s fault
  • increased pressure s fold
  • decreased pressure s fault
  • rock type brittle s fault
  • rock type ductile s fold
  • time greater the time s fold
  • time less time s fault

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  • Earthquakes
  • Earthquake is the shaking and trembling that
    results from the sudden movement of part of the
    Earths crust.
  • Tsunamis A giant sea wave produced by an
    earthquake.

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  • Seismic Waves
  • Focus The point beneath the Earths surface
    where the rocks break and move, the underground
    origin of the earthquake.
  • Epicenter The point directly above the focus,
    on the earths surface where the origin of an
    earthquake is above ground.

29
Faults- Once the elastic limit of rocks is
passed, they break and move along surfaces.
  • 3 types of faults are
  • Normal Fault- These form at divergent boundaries.
  • Reverse Fault- These form at convergent
    boundaries.
  • Strike-Slip Fault- These form at transform
    boundaries.

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  • Seismic waves earthquake waves. Three types.
  • 1. Primary waves (P-waves) - arrive at a given
    point before any other type of seismic wave. Will
    pass through solid, liquid and gas.(fastest of
    the three)
  • 2. Secondary Waves (S-waves) arrive at a
    given point after the P wave. (second fastest)
    Will only travel thru solids. Will NOT pass
    through liquids and gases thus creating a shadow
    zone.

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  • 3. Surface waves (L-waves) slowest
    moving seismic waves. Arrives last.

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  • Volcanoes
  • Volcano A mountain that forms when layers of
    lava and volcanic ash erupt and build up.
  • Magma rock that exists as a hot liquid deep
    within the earth.
  • Lava is magma that reaches the Earths surface.

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  • Composite Volcanoes Violent eruptions due to
    high amount of silica (D.A.N, quartz, mica,
    feldspar) which is light in color and is
    explosive because of large amounts of gas, ash
    and lava.

38
  • Domes is the uprising area caused by magma

39
  • Shield volcano Volcanoes composed of quiet lava
    flows. The lava has a low amount of silicia
    (D.A.N, quartz, mica feldspar) and is dark in
    color. These volcanoes are nice with gently
    sloping sides with very wide base.
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