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Chapter 7  Earthquakes What are Earthquakes? Section 1
Seismology The study of earthquakes
Fault A break in the Earth’s crust along which the crust slide relative to one another Normal Thrust Strike-slip
Deformation Change in the shape of a rock in response to stress
Elastic Rebound Sudden return of elastically deformed rock
Transform Motion  Two plates slip past each other                      
Strike-Slip Fault Blocks of crust slide past each other
Convergent Occurs where two plates push together                             
Reverse Fault Blocks of crust that are pushed together slide vertically
Divergent Motion Two plates pull away from each other                      
Normal Faults Block of crust are pulled away from each other slide vertically
Seismic Waves Waves of energy that travel through the Earth
P Waves Travel through solids liquids & gases. Fastest  seismic waves (Primary Waves)
S Waves Shear waves, second fastest seismic wave(Secondary Wave)
Surface Waves Moves the ground up and down in circles as the waves travel along the surface
Chapter 7  Earthquakes Earthquake Measurement Section 2
Seismographs Instruments that record seismic waves
Seismogram Tracing of an earthquake motion created by a seismograph
Epicenter Point on the Earth’s surface directly above an earthquakes starting point
Focus The point inside the Earth where the earthquake begins
Finding the Epicenter A circle is drawn around 3 different seismograph station
Richter Scale Tool used to measure the earthquake strength
Chapter 7  Earthquakes Earthquakes and Society Section 3
Earthquake Hazard How prone an area is to experiencing earthquakes in the future
Strength & Frequency The weaker the earthquake the more often they occur
Gap Hypothesis Sections of active faults that have few earthquakes are likely to be sites of strong earthquakes
Seismic Gaps Areas along the fault where relatively few earthquakes have occurred
Mass Damper Weight placed on the roof of the building
Cross - Braces Braces placed between floors
Flexible Pipes Prevent water & gas lines from breaking
Base Isolators Act as shock absorbers during an earthquake
Active Tendon System Works like damper system in the roof
Chapter 7  Earthquakes Earthquake Discoveries near and Far Section 4
Moho Space within the Earth where the speed of seismic waves increase sharply
Shadow Zone Area on the Earth’s surface where no waves from a particular earthquake can be detected
Inner Core Solid inner core
Moonquakes Seismograph event on the moon
Mars Space probe  Viking I
The Sun Seismic Waves

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