Question
#112252. Asked by george48. (Jan 20 10 4:53 PM)
dcpddc478
During an earthquake seismic waves propagate spherically out from the hypocenter. Seismic shadowing occurs on the opposite side of the Earth from the earthquake epicenter because the liquid outer core refracts the longitudinal or compressional (P-waves) while it absorbs the transverse or shear waves (S-waves). Outside of the seismic shadow zone both types of wave can be detected but, due to their different paths through the Earth, they arrive at different times. By measuring the time difference on any seismograph as well as the distance on a travel-time graph at which the P-wave and S-wave have the same separation, geologists can calculate the distance to the earthquake's epicenter. http://en.wikipedia.org/wiki/Epicenter
Jan 20 10, 5:21 PM
Find something useful here? Please help us spread the word about FunTrivia. Recommend this page below!
"Ask FunTrivia" is for entertainment purposes only, and answers offered are unverified and unchecked by
FunTrivia. We cannot guarantee the accuracy or veracity of ANY statement posted. Feel free to post an updated
response
if you feel that an answer is inadequate or incorrect. Please
thoroughly research items where accuracy is important to you using multiple reliable sources. By accessing our
website, you agree to be bound by our terms of service.