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Chapter 8 terms - Earthquakes

Terms from Chapter 8 in our Earth Science text

AB
focuspoint in earth's crust where the rocks actually broke and moved
epicentermap location of the earthquake
Richter Scalescale measuring earthquake magnitude
elastic reboundprocess of rocks snapping back into position - the cause of an earthquake
aftershock"earthquake after the earthquake"
seismographinstrument that detects seismic waves
list 3 earthquake wavesP,S,L
New Madridmid-plate fault zone in N.A.
faultcrack in rocks along which movement has occured
Mohoboundary between crust and mantle
shadow zonebelt around earth that receive no earthquake waves
time it takes a P-wave to travel 4000km7 minutes
distance to an earthquake with an S-P lag of 8min. 20s6800km
anticlineupfold in rock layers
synclinedownfold in rock layers
normal faulthanging wall moves down
reverse faulthanging wall moves up
active continental marginoccurs along plate boundaries; ex. west coast of N.A.
passive continental marginnot at plate boundary;ex. east coast of N.A.
strikecompass direction of a fold
limbside of a fold
list three evidences of uplifting1. fossils high above sea level 2.raised beaches 3. using instruments to measuring it
give an example of fault-block mountainsSierra Nevadas
What lifts up a plutonic dome mountain?a laccolith
what process raises a tectonic dome mountain?uplifting due to compressional forces
How far away is an earthquake if the S-P time lag is 3min30s?about 2000km
How long does it take an S wave to travel 6000km?about 16min40s
How far is an earthquake's epicenter if the P waves arrive at 4:00 and the S-waves arrive at 4:05?about 3400km


Earth-Space Science and Planetarium instructor
Mt. Pleasant Jr./Sr. High School

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