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Earthquakes

Science

TermDefinition
earthquake vibrations in the earth caused by the sudden release of energy, usually the result of movement of rocks along a fault
crust the earth's outer layer; the coolest and least dense layer of the earth
fault a fracture in a bed rock, along with blocks of rock on opposite sides of the fracture move
mantle the layer of the earth beneath the crust, it is about 2900 km thick and makes up about 83% of the earth's interior
lithosphere the cool solid outer shell of the earth, it consists of the crust and the rigid uppermost part of the mantle and is broken up into segments or plates
seismologists scientists who study earthquakes
convergent boundary tectonic plates that collide (crash) into each other
divergent boundary tectonic plates that move away (divide) from each other
transform boundary tectonic plates that slide past each other
subduction the process by which collision of the earth's plates results in one plate being drawn down and melted back into the mantle
convection when the liquid mantle is heated and move in two circles that move away from each other
s-wave secondary seismic wave that moves side to side
p-wave primary seismic wave that pushes and pulls
surface wave strongest and most damaging to things on the surface: the slowest seismic wave
focus the point beneath Earth's surface at which rock under stress breaks and triggers and earthquake
epicenter the point on the surface directly above the point at which an earthquake occurs
Mercalli scale describes earthquakes according to the level of damage at a location
Richter scale a rating of an earthquakes intensity off of the size of the seismic waves, on a scale form 1 to 10
moment magnitude scale estimates the amount of energy released during an earthquake
lithospheric plates broken up pieces of the Earth's crust and uppermost mantle
magnitude the amount of energy released during an earthquake
tsunami large ocean waves caused by strong earthquakes below the ocean floor
liquefaction the process in which an earthquake's shaking turns loose, soft, soil into liquid mud
aftershock smaller earthquakes after one large earthquake
seismology the study of earthquakes
seismograph a machine that records the movement of the earth's surface
compression a stress that pushes rock together, the rock folds or breaks
tension a stress that pulls rock apart, the rock stretches until it evenyually breaks
shearing a stress that pushes rock in two different directions, the rock breaks and sometimes changes shape or volume
plateau a large area of flat land elevated high above the sea level
normal fault the hanging wall slips downward below the footwall
reverse fault the hanging wall slides up and over the footwall
Created by: 1964968716
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