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chapter 19

Vocabulary

TermDefinition
stress forces per unit area taht act on material compression tension and shear.
strain deformation of materials in response to stress
elastic deformation causes material to bend and stretch;proportational to stress, so if the stress is reduced or returns to zero the strain or deformation is reduced or disappears.
plastic deformation permanent deforamtion casued by strain when stress exceeds a certain
fault fracture or system of fractures in Earth's crust that occurs when stress is applied too quickly or stress is too great; can form as a result of horizontal compression
seismic wave the vibration of the ground during an earthquake
primary wave seismac wave that squeezes and pushes rocks int he same direction that the wave travels known as p wave
secondary wave seismic wave that causes rock particles move at the right angles to thedirection of the wave,known as an s wave
focus point of theinitial fault repture where an earthquake originates that usually lies at least several kilometers beneath earth's surface
epicenter point on earth's surface directly a above the focus of an earthquake
seismeter instruction used to measure horizontal or verical motion during an earthquake.
seismogram record produced by a seissmometer that can provide individual tracking of each type of seismic wave
richter scale numerical rating system used to measure the amount of energy released during an earthquake
magnitude measure of the energy released during an earthquake, which can be described using the richter scale
amplitude the size of rhe seismic waves; an increase of 1 in the scale reprsenets an increawse in amplitude of a factor of 10
moment magnitude scale scale suded to measure earthquake magnitude taking into account the size of the fault reputure the rocks stiffness and amound of movement aling the fault
modified mercelli scale measure earthquake intensity on a scale from 1 to 5
soil liquefaction process associated with seismic vibrations that occur in areas of sand that is nearly saturated; resulting in the ground behaving like a liquid
tsunami large powerful ocean wave generated by the vertical motions of the seafloor during an earthquake; in shallow water, can form huge.
seismic gap place along an active fault that hass nt experienced an earthquake for a long time.
Created by: louizatamez
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