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CM Earth Science 3-1

Unit 3 Mr. Wilbur/Barbis: Chapter 12

QuestionAnswer
Earthquake A movement or trembling of the ground that is caused by a sudden release of energy when rocks along a fault move; vibrations of Earth’s crust by a sudden release of energy;
Most earthquakes occur along what geologic structures? Faults & Subduction Zones
Seismic waves Travel in all directions from focus point
Elastic rebound A sudden return of elastically deformed rock to its undeformed state
Elastic rebound causes earthquakes After return to undeformed state, rocks on each side move slowly, if the fault is locked, stress increases and the earthquake occurs
Causes of Earthquakes Faulting; volcanoes; landslides; human causes; impact from space objects
Focus Location within the Earth along a fault at which the first motion of an earthquake occurs
Epicenter The point on Earth’s surface directly above an earthquake’s starting point, or focus
Body wave In geology, a seismic wave that travels through the body of a medium; Generated at focus; travel through Earth’s interior
Surface wave In geology, a seismic wave 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
2 main types of seismic waves P-waves; S-waves
P-wave Primary wave or compression wave; 1st to arrive; back-and-forth motion parallel to direction wave is traveling; fastest; travel through solids, liquids, and gasses; bend and change speed at boundaries
S-wave Secondary wave or shear wave or transverse wave; 2nd to arrive; side-to-side motion perpendicular to direction wave is traveling; second-fastest waves; travel only through solids
L-Waves Surface waves or Love waves; travel along Earth’s surface; do most damage; can produce tsunamis if epicenter is on sea floor; slowest moving ; side to side motion
Rayleigh Rolling motion
3 ways that P-waves differ from S-waves P-waves are faster than S-waves;P-waves move parallel to direction of wave vs. S-waves move perpendicular to wave;P-waves move through solids, liquids, and gasses vs. S-waves move through solids
Why seismic waves are important in understanding Earth’s interior By measuring the P-waves & S-waves scientists can determine what type of material the Earth is made up of based on what the waves can pass through; speed & direction changes as waves move through different mediums
Shadow zone Areas waves cannot move through
Seismology Study of earthquakes and seismic waves
Seismometer Detects current earthquake activity
Relationship between a seismograph and a seismogram A seismograph is an instrument that records vibrations in the ground and a seismogram traces the motion of an earthquake that is recorded by a seismograph
Minimum number of seismic stations needed to triangulate position of earthquake epicenter 3
Magnitude Measure of energy released by earthquake; Richter Scale; each increase in magnitude represents a 31x increase in energy; results in an increase in shaking by a factor of 10
Intensity Amount of damage caused by an earthquake to people and property; Modified Mercalli Intensity Scale
5 dangers resulting from earthquakes that could cause injury or death Collapsing buildings;Falling objects;Flying glass;Landslides, fires, explosions;Broken electric and gas lines, flooding
3 steps that should be taken before an earthquake occurs Keep an emergency supply of food, bottled water, flashlights, batteries, portable radio;Plan what you will do when at home, school or work;Discuss plans with family, learn how to turn off gas, water, and electricity in home
How seismic gaps help seismologists predict where and earthquake could occur Area along a fault where relatively few earthquakes have occurred recently but where strong earthquakes are known to have occurred in the past
Fault A break in a body of rock
Created by: vbarbis
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