What%20is%20the%20Elastic%20Rebound%20Theory? - PowerPoint PPT Presentation

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What%20is%20the%20Elastic%20Rebound%20Theory?

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What is the Elastic Rebound Theory? Explains how energy is stored in rocks Rocks bend until the strength of the rock is exceeded Rupture occurs and the rocks quickly ... – PowerPoint PPT presentation

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Title: What%20is%20the%20Elastic%20Rebound%20Theory?


1
What is the Elastic Rebound Theory?
  • Explains how energy is stored in rocks
  • Rocks bend until the strength of the rock is
    exceeded
  • Rupture occurs and the rocks quickly rebound to
    an undeformed shape
  • Energy is released in waves that radiate outward
    from the fault

2
  • The Focus and Epicenter of an Earthquake
  • The point within Earth where faulting begins is
    the focus, or hypocenter
  • The point directly above the focus on the surface
    is the epicenter

3
Where Do Earthquakes Occur and How Often?
  • 80 of all earthquakes occur in the
    circum-Pacific belt
  • most of these result from convergent margin
    activity
  • 15 occur in the Mediterranean-Asiatic belt
  • remaining 5 occur in the interiors of plates and
    on spreading ridge centers
  • more than 150,000 quakes strong enough to be felt
    are recorded each year

4
The Economics and Societal Impacts of EQs
Damage in Oakland, CA, 1989
  • Building collapse
  • Fire
  • Tsunami
  • Ground failure

5
How is an Earthquakes Epicenter Located?
  • Three seismograph stations are needed to locate
    the epicenter of an earthquake
  • A circle where the radius equals the distance to
    the epicenter is drawn
  • The intersection of the circles locates the
    epicenter

6
Why do earthquakes occur?
  • Fractures, faults
  • Energy released
  • and propagates in all directions as seismic
    waves causing
  • earthquakes

7
Crater Lake, Oregon
8
The Stump of Mount Mazama
9
Ash
What comes out of a volcano?
10
Gas
What comes out of a volcano?
Most common H2O CO2 SO2 HCl
11
What comes out of a volcano?
Lava
12
Mauna Loa (Hawaii) A typical shield volcano
13

Mt. St. Helens A typical composite volcano
14
Mt. St. Helens after its 1980 eruption
15
How Calderas Form
16
Plate-tectonic setting of volcanism
Explosive (andesitic) volcanoes form at
subduction zones.
17
Plate-tectonic setting of volcanism
At spreading centers, low pressure
triggers mantle meltingfluid basaltic magma
rises.
18
Plate-tectonic setting of volcanism
Within plates, rising plumes of hotter mantle
feed hot spots varied volcanoes result (basaltic
on Hawaii).
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Mt. St. HelensPyroclasticEruption
21
Mount Saint Helens- after
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Mt. Saint Helens before
36
Phreatic (vapor) eruption
37
Bulge
38
After the eruption
39
Pyroclastic eruption
40
Volcanic landscape A Caldera (Crater Lake)
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