C. Time-Travel Graphs Time travel graphs area used to estimate the distance of an epicenter from the seismic station. This is accomplished using the time difference between the arrival of P and S waves. On this graph the vertical separation between the Pand S curves is the same as the difference in the arrival times between P and S waves. Once the distance to an epicenter is determined from 3 locations, the epicenter location can be determined. Travel-Time Graph 24 23 8. Use the travel-time graph to 22 estimate the difference in arrival times 21 20 (in minutes) between the first P-wave 19 and first S-wave for stations that are the 18 following distances from an epicenter. 17 16 15 1000 km: 14 13 minutes difference 12 11 5000 km: 10 minutes difference 8 7 8000 km: minutes difference 5 2 1000 2000 3000 4000 5000 6000 7000 8000 EPICENTER DISTANCE (KM) TRAVEL TIME (minutes) %24
C. Time-Travel Graphs Time travel graphs area used to estimate the distance of an epicenter from the seismic station. This is accomplished using the time difference between the arrival of P and S waves. On this graph the vertical separation between the Pand S curves is the same as the difference in the arrival times between P and S waves. Once the distance to an epicenter is determined from 3 locations, the epicenter location can be determined. Travel-Time Graph 24 23 8. Use the travel-time graph to 22 estimate the difference in arrival times 21 20 (in minutes) between the first P-wave 19 and first S-wave for stations that are the 18 following distances from an epicenter. 17 16 15 1000 km: 14 13 minutes difference 12 11 5000 km: 10 minutes difference 8 7 8000 km: minutes difference 5 2 1000 2000 3000 4000 5000 6000 7000 8000 EPICENTER DISTANCE (KM) TRAVEL TIME (minutes) %24
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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The immediate and short-term tremble generated on the earth surface that varying from a small tremor to a wide motion generated by the sudden release of energy stored in the rock beneath the earth surface is termed an earthquake. A point inside the earth surface where seismic waves are started to propagate is termed focus and the point immediately above the focus in the ground surface where seismic waves are first reaches is called the epicentre.
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