Amplitude, mm 12 10 4208642 246821 10 Amplitude, mm Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 P Salt Lake City, UT Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 60 1208642 2468 24 14 P S 10 12 Tucson, AZ Amplitude, mm 1208642 10 12 14 246824 Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 זיזיז'ז'ז'די P Yuma, AZ Amplitude, mm 14 8 120 %642 10 12 14 246824 80 100 120 140 160 Time, seconds 180 200 220 240 260 280 Amplitude, mm 14 12 10 8 6 Pinyon Flats, CA 300 Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 8 10 P S 12 14 Pasadena, CA
Amplitude, mm 12 10 4208642 246821 10 Amplitude, mm Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 P Salt Lake City, UT Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 60 1208642 2468 24 14 P S 10 12 Tucson, AZ Amplitude, mm 1208642 10 12 14 246824 Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 זיזיז'ז'ז'די P Yuma, AZ Amplitude, mm 14 8 120 %642 10 12 14 246824 80 100 120 140 160 Time, seconds 180 200 220 240 260 280 Amplitude, mm 14 12 10 8 6 Pinyon Flats, CA 300 Time, seconds 80 100 120 140 160 180 200 220 240 260 280 300 8 10 P S 12 14 Pasadena, CA
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question
Using the differences between P and S arrival times (S minus P), and the travel time curves, estimate the distances from the epicenter to each location.
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