Description

a fault whose main motion is parallel to it's dip
a fault along which main movement is horizontal or parallel to the fault's strike; transform strike.
is a type of dip-slip fault in which the upper body of rocks drops relative to the lower body of rock.
, is a type of dip-slip fault where the upper block slides upward in relation to the lower block.
, it is the fastest and first waves to reach a seismic station from an earthquake traveling through solid and liquid rock and has the least damage.
it is the second earthquake wave that reaches a seismic station from an earthquake and it does not pass through the core.
it is the compass direction of horizontal plane of surface of fault force of rock stratum.
it is the upward force by a fluid on a less dense object in denser material.
forces acting in opposite directions on different parts of the same object; slips in layers.
any force exerted on an object
is the location on the earth's surface that is directly above the focus.
is the point of the earthquake's origin deep within the earth.
change in shape of solid due to stresses exerted on material.
is a measurable movement of the earth's crust; release of energy from stress along faults.
scale that rates magnitude of intensity of earthquakes.
forces that act to pull an object apart
is a far-reaching, devastating water wave caused by seismic activity.
is an instrument that detects the movement of the earth due to seismic waves.

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Earthquakes

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Earthquakes

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Chapter 2 Earthquakes

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Energy & Heat

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