earthquakes. by: laura barjarow chapter 12.. earthquakes a movement or trembling of the ground that...
TRANSCRIPT
Earthquakes
• A movement or trembling of the ground that is caused by a sudden
release of energy when rocks along a fault move
Seismograph.
• Earthquakes generate seismic waves which can be detected with a sensitive instrument called a seismograph.
• Instrument that records vibrations in the ground
• Seismogram- a tracing of earthquake motion that is recorded by a seismograph.
seismic waves.
• Body waves- in geology, a seismic wave that travels through the body of a medium.
• Surface waves- in geology, a seismic that travels along the surface of a medium and that has a stronger effect near the surface of the medium than it has in the interior.
Body waves.
• P waves- (primary waves, or compression wave); a seismic wave that causes particles of rock to move in a back-and-forth direction parallel to the direction in which the waves traveling; fastest traveling seismic waves and can travel through solids, liquids, and gases.
• S waves- (secondary waves, or shear wave); a seismic wave that causes particles of rock to move in a side-to-side direction perpendicular to the direction in which the wave is traveling; second-fastest seismic waves and can travel only through solids.
Epicenters.
• The point on earth’s surface directly above an earthquakes starting point, of focus.
• Focus- the location within earth along a fault in which the first motion of an earthquake occurs.
How to Locate Epicenter.
• Get three different seismograph reading and plot them on a map. The point which all the circles meet is where the epicenter is.
Elastic Rebound Theory.
• Elastic rebound- the sudden return of elastically deformed rock to its undeformed shape.
• Two blocks of crust push against each other at a fault. Which causes stress but doesn’t move because of friction .
• As stress builds up at the fault, the crust deforms.• The rock fractures and then snaps back into its
original shape, causing an earthquake.