Chapter 10 - Earthquakes and Earth's Interior Flashcards
Seismology
Study of earthquakes
Seismometer
used to record shocks and vibrations from earthquakes
Inertial Seismometer
Relies on resistance of stationary mass to movement
Focus
point where earthquake starts to release elastic strain of surrounding rock
Epicenter
point on earth’s surface lying vertically above focus
Seismic Waves
vibrational waves that spread out in all directions initially from focus
Body waves
seismic waves that travel through earth’s interior
Primary (P) Wave
compressional - can pass through solids or fluids - rock vibrates back and forth in line of wave motion - fastest
Secondary (S) Wave
cannot pass through fluids - rock moves sideways perpendicular to direction of wave travel - slower that P waves
Surface Wave
pass around earth rather than through it - slower than either P waves or S waves - different wavelengths develop different velocities (dispersion)
Determining Epicenter
locate from arrival times of P waves and S waves at 3 or more seismometers
Richter Magnitude Scale
estimated by measuring amplitudes of seismic waves - divided into steps representing 30 times increase in energy
Earthquake Hazard
most large earthquakes occur along plate boundaries - seismic risk maps based on acceleration relative to gravity used to design roadways and public buildings
Earthquake Disasters
Based on number of people killed
Earthquake Damage
1) Ground motion - 2) displacement along faults - 3) fire - 4) landslides - 5) liquefaction - 6) tsunamis