Maximum deviation from mean of centerline of a wave
Aftershock
One of a series of smaller quakes following the main shock of the earthquake.
Core
The central part of the earth below a depth of 2,900 kilometers. It is thought to be composed of iron and nickel and to be molten on the outside with a central solid inner core.
Crust
The lithosphere, the outer 80 kilometers of the earth’s surface made up of crustal rocks, sediment and basalt. The general composition is silicon-aluminum-iron.
Deflection
The horizontal or vertical displacement of a member due to the application of external force.
Deformation
Permanent distortion due to seismic forces.
Depth of Focus
the depth of the focus or hypocenter beneath the earth’s surface commonly classes Earthquakes: Shallow (0- 70 kilometers), intermediate (70-300 kilometers), and deep (300-700 kilometers).
Displacement
Lateral movement of the structure caused by lateral force.
Drift
Horizontal displacement of basic building elements due to lateral earthquake forces.
Epicenter
The point of the earth’s surface directly above the focus or hypocenter of an earthquake
Fault
A fracture plane in the earth’s crust across which relative displacement has occurred. (Location of slippage between the earth’s plates).
Normal Fault
A fault under tension where the overlying block moves down the dip or slope of the fault plane.
Strike-Slip Fault (or lateral slip)
A fault whose relative displacement is purely horizontal.
Thrust (Reverse) Fault
A fault under compression where the overlying block moves up the dip or slope of the fault plane.
Oblique-Slip Fault
A combination of normal and slip or thrust and slip faults whose movement is diagonal along the dip of the fault plane.
Faulting
The movement which produces relative displacement of adjacent rock masses along a fracture.
Fault Zones
The zone surrounding a major fault, consisting of numerous interlacing small faults.
Focal Depth
Depth of the earthquake (or hypocenter) below the ground surface.
Focus (of an earthquake) or Hypocenter
The point at which the rupture occurs; (It marks the origin of the kinetic waves of an earthquake).
Hypocenter or Focus
The point below the epicenter at which an earthquake actually begins; the focus.
Frequency
The number of wave peaks or cycles per second. The inverse of Period.
Intensity
A subjective measure of the force of an earthquake at a particular place as determined by its effects on persons, structures and earth materials. Intensity is a measure of energy.
MM (or Modified Mercalli) scale
The principal scale used in the United States today. It is based on observation of the effects of the earthquake MM-I thru MM-XII (MM-I = not felt, MM-XII = damage nearly total).
Landslide
Earthquake triggering land disturbance on a hillside where one land mass slides over the other.
Liquefaction
Transformation of a granular material (soil) from a solid state into a liquefied state as a consequence of increased porewater pressure induced by vibration. Normally solid soil suddenly changes to liquid state (usually sand or granular soil in proximity to water) due to vibration.
Magnitude
A measure of earthquake size which describes the amount of energy released.
Moment Magnitude
is the measure of total energy released by an earthquake. It is based on the area of the fault that ruptured in the quake. It is calculated in part by multiplying the area of the fault’s rupture surface by the distance the earth moves along the fault.
Richter Magnitude Scale
A measure of earthquake size which describes the amount of energy released. The measure is determined by taking the common logarithm (base 10) of the largest ground motion observed during the arrival of a P-wave or seismic surface wave and applying a standard correction for distance to the epicenter. (Each unit of the Richter Scale represents a 10 times increase in wave amplitude. This corresponds to approx. 31 times increase of energy discharge for each unit on the Richter Scale.)
Seismograph
A device, which writes or tapes a permanent, continuous record of earth motion, a seismogram.
Tsunami
A sea wave produced by large area displacements of the ocean bottom, the result of earthquakes or volcanic activity. (Tidal wave caused by ground motion.)
Body Wave
Seismic waves within the earth.
Longitudinal Wave
Pure compressional wave with volume changes.
Love Wave
Surface waves that produce a sideways motion.
Rayleigh Wave
Forward and elliptical vertical seismic surface waves.
P-Wave
A type of body wave; the fastest waves traveling away from a seismic event through the earth's crust, and consisting of a train of compressions and dilatations of the material (push and pull).
S-Wave
Secondary wave, or Shear wave, sometimes called an elastic S-wave, produced essentially by the shearing or tearing motions of earthquakes at right angles to the direction of wave propagation.
Surface Wave
Also known as L-waves; a seismic wave that follows the earth's surface only, with a speed less than that of S-waves.
Wave Length
The distance between successive similar points on two wave cycles.
Richter magnitude scale
most common standard of measurement of earthquakes.