Flashcards in VOCAB GHC Ch 3: Earthquake Geology and Seismology Deck (52):
(1) To cause to move faster. (2) The rate of change of motion.
A smaller earthquake following a mainshock on the same section of a fault. Aftershocks can continue for years following a large mainshock.
The maximum displacement or height of a wave crest or depth of a trough.
Protecting buildings from earthquakes ny isolating the base of the building form the shaking ground via rollers, shock absorbers, etc.
Seismic wave that travels through the body of the earth-- for example, primary and secondary waves.
A state of stress that causes a pushing together or contraction.
A two-dimensional drawing showing features in the vertical plane, as in a canyon wall or road cut.
The angle of inclination measured in degrees from the horizontal.
Fault where most of the movement is either up or down in response to pushing or pulling.
A fracture or belt of fractures where the two sides move past each other.
The underlying side or block of a fault.
A smaller earthquake that precedes a mainshock on the same section of a fault.
A general term for any breaks in rock. Fractures include faults, joints, and cracks.
Number of events in a given time interval. For earthquakes, it is the number of cycles of seismic waves that pass in a second; frequency = 1/period.
The resistance to motion of two bodies in contact.
A quartz-rich plutonic rock.
The overlying side or block of a fault.
One hertz equals one cycle per second.
The initial portion of a fault that moved to generate an earthquake.Hypocenters are below the ground surface; epicenters are above them on the surface.
The property of matter by which it will remain at rest unless acted on by an external force.
A fracture or parting in rock.
law of original continutiy
A water-laid sediment body continues laterally in all directions until it thins out do to nondeposition or butts against the edge of the basin of deposition.
law of original horizontality
Sediments are deposited in nearly horizontal layers.
law of superposition
In a sequence of sedimentary rock layers, the oldest layer is at the base, and ages are progressively younger to the top.
A strike-slip fault where most of the displacement is toward the left hand of a person straddling the fault.
An assessment of the size of an an event.
The largest earthquake in a sequence.
A two-dimensional representation showing the features in a near-horizontal surface, such as the ground.
A dip-slip fault in which the upper fault block has moved downward in response to tensional stress.
The length of time for a complete cycle of seismic waves to pass; equals 1/frequency.
The capacity of a porous material to transmit fluids.
primary (P) wave
The first seismic wave to reach a seismometer. Movement is by alternating
The act of resounding, ringing.
Reinforcement or strengthening of an existing building or other structure.
A dip-slip fault where the upper fault block has moved upward in response to compressional stresses.
A strike-slip fault where most of the displacement is toward the right hand of a person straddling the fault.
secondary (S) wave
Second seismic wave to arrive at the seismometer. S waves move only through solid bodies.
A measure of earthquake size that involves amount of movement on the fault, the shear strength of the rocks, and the area of fault rupture.
A general term for all waves generated by earthquakes.
The record made by a seismograph.
An instrument that records vibrations of the Earth.
The study of seismic waves generated by earthquakes.
An instrument that detects Earth motions.
The failure of a body where the mass on one side slides past the portion on the other side.
External forces acting on masses or along surfaces; forces include shear, tension, and compression.
The compass bearing of the trend of a rock layer as viewed in the horizontal plane.
Fault where most of the movement is horizontal or slide-past in character.
A class of seismic waves that travel along the surface only-- for example, Love and Rayleigh waves.
A state of stress that tends to pull a body apart.
A strike-slip fault that connects the ends of two offset segments of plate edges, such as spreading centers or subduction zones.