Using the difference in the time recorded for P waves and S waves to arrive at three different seismograph stations, seismologists can find an earthquake's a. epicenter. b. surface waves. c. fault zone. d. intensity.

perlejatyh8

perlejatyh8

Answered question

2022-11-15

Using the difference in the time recorded for P waves and S waves to arrive at three different seismograph stations, seismologists can find an earthquake's a. epicenter. b. surface waves. c. fault zone. d. intensity.

Answer & Explanation

grizintimbp

grizintimbp

Beginner2022-11-16Added 16 answers

Let's define all the given examples to find the correct solution.
When two rock moves against each other they make pressure that causes the energy release. A place where two rocks are in touch is called a fault zone (c). The intensity (d) of the earthquake depends on the amount of released energy. Seismographs note Pand S waves that come in a time interval of a few seconds. Knowing this time difference, seismologists can determine a circle around the seismograph in which is an epicenter (a). An interaction of P and S wave results in another wave called surface wave (b).
We conclude three different seismograph stations are used to determine an eplcenter.
Result:
a.

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