Earthquake Notes Powerpoint
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Transcript Earthquake Notes Powerpoint
Earthquakes!!
Shake, Rattle and Roll
Earthquake Video
Earthquakes
Earthquakes are the rapid shaking of the
lithosphere at faults, caused by the
release of the potential energy stored in
the rock layers.
Focus
Epicenter
Seismic
Waves
P-waves
S-waves
Click Map for Link to USGS Website
Click Map for Link to USGS Website
Elastic Rebound Hypothesis
Elastic Rebound
Earthquakes
The focus is the point of stress relief in an
earthquake (the point inside Earth).
The epicenter is the location directly
above the focus on Earth’s surface.
Focus, Epicenter, and Fault
Seismic Waves
P-waves
Primary
seismic waves that travel fastest after
an earthquake
Arrive first
Known as compression waves (push and pull motion)
Movement is in the direction of wave motion (slinky)
S-waves
Secondary
seismic waves that travel slower
after an earthquake
Arrive second
Known as transverse waves (shaking up and down
motion)
Movement is perpendicular to the direction of motion
(slinky)
Seismic Waves
Earthquake Waves
Seismic Wave Animation
Seismic Wave Motion
Seismograph
An instrument
that measures
seismic waves
and records
them
Seismogram
Seismographs
Locating an Earthquake Epicenter
ESRT p. 11
Earthquake Magnitudes
Emergency Planning
Death and injury from earthquake damage
can be greatly reduced with proper
planning.
Remember:
Drop, Cover, and Hold
Drop
down under a strong object
Cover your eyes with one hand
Hold the strong object with the other hand
Earthquakes
last 10-30 seconds
Practice earthquake drills
Have emergency supplies
Flashlight
First
Aid
w/ extra batteries
Tsunami
Large wavelength wave produced by
strong underwater earthquakes in the
oceanic crust.
As wave approaches shore the height
grows and can produce 30 m waves in
extreme cases.
Tsunami