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Now that you have made measurements of the gradual rate of motion that leads up to the earthquake, and the resulting motion during the earthquake, calculate how long it would take for the motion to accumulate that results in the same size earthquake. Show all work. Remember: Velocity = Displacement during earthquake/ time. %3D

Now that you have made measurements of the gradual rate of motion that leads up to the earthquake, and the resulting motion during the earthquake, calculate how long it would take for the motion to accumulate that results in the same size earthquake. Show all work. Remember: Velocity = Displacement during earthquake/ time. %3D

Applications and Investigations in Earth Science (9th Edition)
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
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Data from these surveys recorded the location of a lighthouse on Farallon Island (FARB, on the oceanic side of the fault), and the location of an observatory on Mount Diablo (DIAB, on the continental side of the fault) relative to San Francisco (SBRN, right at the fault). Here are the relative locations of these monuments at two different times: Location relative to SBRN FARB DIAB 1858 27408.74 m North 4863.43 m South 1883 27409.36 m North 4864.04 m South Now that you have made measurements of the gradual rate of motion that leads up to the earthquake, and the resulting motion during the earthquake, calculate how long it would take for the motion to accumulate that results in the same size earthquake. Show all work. Remember: Velocity = Displacement during earthquake/ time. 1 year 1000 years 10,000 years 100 years 10 years SUBMIT
Transcribed Image Text:Data from these surveys recorded the location of a lighthouse on Farallon Island (FARB, on the oceanic side of the fault), and the location of an observatory on Mount Diablo (DIAB, on the continental side of the fault) relative to San Francisco (SBRN, right at the fault). Here are the relative locations of these monuments at two different times: Location relative to SBRN FARB DIAB 1858 27408.74 m North 4863.43 m South 1883 27409.36 m North 4864.04 m South Now that you have made measurements of the gradual rate of motion that leads up to the earthquake, and the resulting motion during the earthquake, calculate how long it would take for the motion to accumulate that results in the same size earthquake. Show all work. Remember: Velocity = Displacement during earthquake/ time. 1 year 1000 years 10,000 years 100 years 10 years SUBMIT
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