chapter 9, test 2, earhtquakes Flashcards
earthquakes
a vibration of earth produced by rapid release of energy
focus (hypocenter)
the place within the earth where earthquake waves orginate
energy released radiates in all directions from its source
epicenter
point at the surface directly above the focus
found by using the difference in velocities between the S and P waves
seismic waves
energy is in form of waves (like a droplet of water in a pond)
move faster in consolidated bedrock
move slower through unconsolidated sediment
move slowest through unconsolidated materials with water
elastic rebound
as a rock deforms, it bends, storing elastic energy. when strained beyond its breaking point the rock cracks and releases the stored up energy as seismic waves
aftershocks
adjustments that follow a major earthquake often generate smaller earthquakes
foreshocks
small earthquakes that often precede a major earthquake by days or in some cases several years
fault creep
slow gradual displacement
seismology
study of earthquake waves.
surface waves
travel along the outer part (surface) of the earth.
cause greatest destruction
waves exhibit greatest amplitude adn slowest velocity
body waves
travel through earths interior
primary (P) waves
secondary (S) waves
Primary (P) waves
travel through solids, liquids, and gases
generally P waves travel faster than S waves in solid materials
push/pull motion changing the volume of the intervening material
Secondary (S) waves
travel only through solids (not liquids)
slower velocity than P waves
slightly greater amplitude than P waves.
shaking motion at right angles to their direction of travel
Major Earthquake zones
pacific belt, Himalayas, and the oceanic ridge system
Intensity
a measure of the degree of earthquakes shaking at a given local based on the amount of damage