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Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound. The sudden return of deformed...

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Section Review 12-1 Section Review 12-1 Page #300: 1-10 Page #300: 1-10
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Page 1: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

Section Review 12-1Section Review 12-1

Page #300: 1-10Page #300: 1-10

Page 2: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

#1#1

Describe elastic rebound.

http://www.sceyencestudios.com/animation.htm

The sudden return of deformed rock back to its original shape.

http://www.sceyencestudios.com/movies/elasticrebound.swf

Page 3: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

#2#2Explain the difference between the epicenter

and the focus of an earthquake.

The focus is located within Earth. The epicenter is a point on the surface above the focus.

Page 4: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

#3#3

Compare body waves and surface waves.

http://www.pbs.org/wnet/savageearth/earthquakes/index.html

Body waves travel through Earth’s interior, while surface waves travel only along the outer surface.

Page 5: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

#4#4

Explain how seismic waves help scientists learn about Earth’s interior.

Seismic waves behave differently as they pass through layers composed of different materials. These differences help create a picture of Earth’s interior.

Page 6: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

Earth’s InteriorEarth’s Interior

Page 7: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

#5#5

Explain how the structure of Earth’s interior affects seismic wave speed and direction.

When seismic waves reach boundaries between rock layers their speed changes. They are reflected or change direction as they pass through layers of different composition.

Page 8: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

Earth’s InteriorEarth’s Interior

Page 9: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

#6#6

Explain why earthquakes generally take place at plate boundaries.

Earthquakes result from stress within the lithosphere. They commonly occur at plate boundaries because stress on rock is greatest near plate boundaries, which may be faulted, and thus weaker than plate interiors.

Page 10: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

#7#7

If a seismologic station measures P waves but no S waves from an earthquake, what can you conclude about the earthquake’s location?

The location of the epicenter was on the opposite side of Earth, because the S waves could not pass through the liquid outer core.

Page 11: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.
Page 12: Section Review 12-1 Page #300: 1-10. #1 Describe elastic rebound.  The sudden return of deformed rock back.

The End????The End????

POOR FROSTY……..


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