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Earthquakes

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Like volcanoes, they are a result of the motions of the lithosphere plates. ... They occur when stress along a fault plane overcomes the forces of friction. ... – PowerPoint PPT presentation

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Title: Earthquakes


1
Earthquakes
Earthquakes
2
What is an Earthquake?
  • Is a shaking of the Earths crust caused by a
    release of energy
  • Like volcanoes, they are a result of the motions
    of the lithosphere plates.
  • But includes a much larger area.

3
How does an Earthquake happen?Elastic Rebound
Theory
  • They occur when stress along a fault plane
    overcomes the forces of friction.
  • When friction is finally overcome, the plates
    move suddenly and release earthquake energy.
  • Then rocks along the boundary snap back to their
    original shape.

4
Elastic Rebound Theory
5
Depth of Earthquakes
  • Focus the point on the fault plane at which the
    first movement occurs
  • Epicenter the point on the Earths surface
    directly above the focus

6
Earthquake waves
  • P waves
  • primary (compressional waves)
  • S waves
  • Secondary (Shear)
  • Both are body waves because they travel through
    the body of the Earth
  • L waves
  • Surface waves

7
P waves
  • The back and forth wave motion alternately
    squeezes and stretches the rock material
  • Occur in through ANY material, even air

8
S waves
  • They are the side to side wave causing particles
    to move at right angles to the direction the
    waves are traveling.
  • Occur in solids only, not through liquid or gases.

9
L waves
  • These are the result of the p and s waves when
    they reach the surface.
  • They travel a lot slower than the P and S waves
    (they are move like ripples on the pond)

10
Seismographs
  • Instrument that detects and records the size of
    Earthquakes
  • Measures the P and S waves

11
Determine the distance to the Epicenter
  • Time Travel Graph the relationship between P
    and S wave travel times and epicenter distance

12
Locating an Epicenter
  • You need three locations to pinpoint the location
    of the Epicenter.

13
Earthquake Magnitude
  • Richter scale is designed to measure the
    intensity of the Earthquake.
  • It is a measurement of the amount of energy that
    the earthquake releases itself.
  • Seismic movement (not as easy to measure as the
    Richter scale)
  • This method, though harder, is more accurate as
    far as measuring the total energy involved.

14
Charles Richter
15
Top Ten US Quakes
16
Prince William Sound, Alaska3/28/ 1964 (9.2)
17
Andreanof Islands 1957 (9.1)
  • Damaged 2 bridges
  • Leveled houses
  • Left a 4.3 meter crack in the road
  • 15 meter tsunami
  • Mt. Vesevidof erupted (200 yrs dormant)

18
Rat Islands, Alaska2/3/1965 (8.7)
  • Created a 10.7 m tsunami
  • A crack was noted on an asphalt runway

19
Yakutat Bay, Alaska 9/10/1899 (8.6)
20
Shumagin Islands, Alaska 11/10/1938 (8.2)
  • Created a small tsunami in Hawaii

21
New Madrid (Missouri), Arkansas12/16/1811(8.1)
22
Yakutat Bay, Alaska 9/10/1899 (8.0)
  • Even shellfish and barnacles were found dead
  • 10.6 meter tsunami
  • Foreshocks even 7.0

23
Andreanof Islands, Alaska 5/7/1986 (8.0)
  • Moderate damage done to Atka
  • Masonry on buildings were destroyed

24
New Madrid, Missouri2/7/1812 (8)
  • This is one of 6 major Earthquakes that happened
    in this region over a one year period

25
Cape Yakataga, Alaska 9/4/1899 (7.9)
  • Knocked over tree
  • Generated landslides
  • Raised beaches

26
Fort Tejon, California 1/9/1857 (7.9)
  • One fatality
  • Damage to buildings
  • Major aftershocks felt for 3 days

27
Largest Earthquakes in the Cont. US
28
Largest Earthquakes in Alaska
29
Largest Earthquakes in Hawaii
30
California Seismic activity
  • What happen 1/17/94?
  • Why so much activity?

31
Northridge, Ca1/17/1994
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