Chapter 16 Flashcards
epicenter
point on the surface directly above the focus
greatest ground motion and damage
body waves
energy that travels through the body of the Earth
2 types
P and S
focus
hypocenter
where the energy is released
P waves
primary waves
seismic waves where particles in rock vibrate back and forth in direction the wave is traveling (longitudinal wave)
ex: slinky
S waves
particle movement is perpendicular to the direction in which the wave is traveling (transverse wave)
ex: rope
surface waves
when p or s waves reach the surface
love waves
L waves surface wave
shear wave similar to s-waves (particles vibrate horizontally)
Rayleigh waves
R-wave
particles move in a circular pattern opposite the direction in which the wave is traveling
seismometers
detect seismic waves
measure amount of ground-movement
seismogram
printed or digital record of ground motion
Richter magnitude
based on amount of ground motion
each level is 10 times greater than the last
Mercalli Intensity Scale
based on amount of damage to structures
travel-time diagram
calculates the distance to an epicenter
moment magnitude
calculates accurately the magnitude of shallow and deep focus, local and distant and large and small earthquakes
liquefaction
seismic vibration causes friction between sand grains in waterlogged sediment to be reduced causing it to lose its ability to support overlying weight and flows like a liquid