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Earthquake
Term | Definition |
---|---|
earthquake | the shaking that results from the movement of rock beneath earth's surface. |
crust | the layer of rock that forms earth's outer surface. |
fault | a break or crack in earth's lithosphere along which the rocks move. |
mantle | the layer of hot, solid material between earth's crust and core. |
lithosphere | a rigid layer made up of the uppermost part of the mantle and the crust. |
lithosphereric | the plates in the outer crust. |
seismologists | a person who studies energy waves caused by rocks suddenly breaking apart with in the earth. |
P-wave | type of wave called seismic waves, that travel through a continuum |
S-wave | seismic wave that shakes the ground back and forth |
Surface waves | mechanical wave that propagates along the interface between differing media |
Focus | center point, of attraction, attention, or activity |
Epicenter | the location where the greatest damage associated with an earthquake occurs |
richer scale | earthquake with a magnitude of 1 is detectable only by seismograph |
moment- magnitude | scale used by seismologists to measure size of an earthquake |
mercali scale | seismic scale used to measure the intensity of an earthquake |
seismic waves | elastic wave in the earth produced by an earthquake |
magnitude | the greatest size or extent of something |
seismograph | measures and records details of earthquakes |
liquefaction | strength and stiffness of the soil reduced by an earthquake |
aftershock | smaller earthquake after a lager earthquake |
tsunami | long high sea waves caused by an earthquake |
base isolator | designed to reduce the amount of energy that reaches the building during an earthquake. |
shear core/walls | shear wall transfers some of a quakes energy from roofs to floors to the building foundation and roof. |
tension ties | these devices firmly tie the floors and ceilings of a building to a walls. |
cross bracing | steel cross bracing are placed between stories to stiffen a building's frame and absorbs energy during an earthquake. |
mass damper | dampers that work like the shock absorbs in a car to absorb some of the energy of seismic waves. |
flexible pipe | is water and gas pipes that have flexible joints. Flexible pipes bend as energy goes through them, greatly reducing damage |
compression | stress that squeezes rock until it folds or breaks. |
tension | stress that stretches rock so that it becomes thinner in the middle. |
stress | a force that acts on rock to change its shape and volume. |
strike-slip fault | a type of fault where rocks on either side move past each other sideways with little up or down motion. |
normal fault | a type of fault where the hanging wall sides downward; caused by tension in the crust. |
reverse fault | a type a fault where the hanging wall sides upward; caused by compression in the crust. |
shearing | stress that pushes masses of rock in opposite directions, in a sideways movement. |
San Andreas Fault | a fault in California. |
plateau | a land form that has high elevation and a more or less level surface. |
hanging wall | the block of rock that forms the upper half of a fault. |
foot wall | the block of rock that forms the lower half of a fault. |
Anticline | an upward fold in rock former by compression of earths crust. |
Syncline | a downward fold in rock formed by compression of earths crust. |
asthenospere | located in the upper mantle, between the depths of 100 to 660 kilometers and not rocky material. |
mantle | is solid rock |
crust | very thin outer skin |
inner core | is solid |
outer core | is fluid |
lithosphere | includes the upppermost mantle, strong and has cool rocks. |