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Earthquakes Chapter6

QuestionAnswer
Stress The movements of the Earth's plates creates enormous force that squeeze, pull or push rocks.
Tension Pulling of the earth's crust causing it to thin
Compression Squeezes rock until it folds or breaks
Shearing stress that pushes rock in two opposite directions
Normal Faults Tension in the earth's crust pulls rock in apart (causing the hanging wall to move down)
Reverse Fault Compression causes this fault to move (Hanging wall moves up)
Strike-Slip Faults the faults move past each other in opposite directions using shearing.
Folding the bending of the earth's crust without breaking
Anticline an upward fold in the earth
Syncline A downward fold in the earths crust
Fault-Block Mountain two narrow parallel normal faults pulling the crust apart can form these mountains
Earthquake the shaking and trembling of the earth that results from rock movement beneath the surface
Focus The place beneath the earth that moves because of stress built up releasing an earthquake
epicenter The area directly above the focus on the surface of the earth where the most violent shaking occurs
Seismic waves Waves of energy that are created during an earthquake and are carried away from the focus
P waves (Primary Waves) the fastest moving of the seismic waves moving in a compression expansion method.
S Waves (Secondary Waves) Seismic waves that vibrate from side to side as well as up and down
Surface waves Start at the epicenter from P and S waves and are the most destructive.
Mercalli Scale scale used to evaluate the level of an earthquake based on the damage that it does
Richter Scale the rating of an earthquakes magnitude based on the size of an earthquakes seismic waves
Seismograph an instrument that records and measures seismic waves
Moment Magnitude Scale the rating is based on an estimate of the total amount of energy that an earthquake releases
Locating an epicenter Scientists use the speed at which seismic waves travel to identify the epicenter. Need 3 stations to identify the epicenter
Tiltmeter Instrument that measures vertical movement across a fault
Creep Meters this instrument measures horizontal movement by using a wire stretched across a fault
Laser-Ranging Device a laser is used to detect horizontal movement
GPS Satellites Changes in vertical and Horizontal movement of a fault using Earth-orbiting satellites
Mapping of Faults using data mapping of fault areas with movement instrument help scientist make predictions and earthquake risk
Earthquake Prediction with all our knowledge we are still unable to accurately predict earthquakes and ground movements
Earthquake damage from shaking Soils and rock help determine how much damage can be done with seismic waves
Liquefaction earthquakes violent shaking can turn soils into mud because water rises up within the earth This can cause building to sink
Aftershocks is an earthquake that occurs in the same location after a large quake
Tsunamis when an earthquakes jolts the ocean floor causing the floor to rise up and push water into a giant wave that moves rapidly through the ocean
Earthquake safety in room Drop, cover and hold onto the object over your head Outside move to an open area where you can not get hit with falling debris
base-isolated buildings building rests on sock absorbing rubber pads
Large tall items in buildings Fasten large items to the wall to keep them from falling on people
Utilities keeping safe Install flexible hoses to stoves and furnaces to allow for movement during a quake and fasten down items so they will not tip over.
Ways to help keep buildings safe dampers, flexible pipes, cross braces, tension ties
Created by: P-townMr. Green
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