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15 Cards in this Set

  • Front
  • Back

Elastic limit

Max amount of strain that an object can accumulate before fracturing or undergoing deformation.

Body waves

Underground waves that spread in a spherical shape like a firework.

Surface waves

Waves that move along the surface once the body waves reach it.

P-Waves

Type of body wave where particles vibrate in the same direction that the wave is traveling (compressing and decompressing).

S-Waves

Type of body wave where particles vibrate perpendicular to the direction that the wave is traveling (side to side motion)

Rayleigh waves

Type of surface wave where particles vibrate in the same direction as the wave and also up and down (rolling motion)

Love waves

Type of surface wave where particles vibrate back and forth and side to side at the same time.

Inertia

Objects at rest stay at rest and objects in motion stay in motion until acted on by outside force.

Mercalli intensity scale

A quantitative means of ranking the intensity of earthquakes based on first-hand human observations, particularly the amount of structural damage.

Richter magnitude scale

The original magnitude scale, developed by Charles Richter and Beno Gutenberg, used to quantify the amount of ground motion.

Subduction zone earthquakes

Earthquakes that occur when an oceanic plate is overridden by another plate, generating some more powerful earthquakes.

Natural vibration frequency

The frequency at which a building will naturally vibrate when the ground shakes during an earthquake.

Wave attenuation

The steady decrease in seismic wave energy that occurs as the waves travel away from their point of origin at the focus

Ground amplification

When seismic waves encounter weaker materials and begin to slow down, causing an increase in wave amplitude and ground shaking

Seismic gap

A tool for predicting the likelihood of an earthquake, based on sections of an active fault where the strain has not been released for an extended period of time.