time (s) 1) The USGS collected seismic refraction data in California. The data are shown in the image below. Interpret the data – be quantitative in determining layer thickness and velocity, and also determine likely geological material. (25 pts) Distance (m) 100 75 50 25 25 0 25 50 75 15 0.0 0.02- 0.04- 0.06- 0.08- 0.10- 0.12- 0.14- 0.16- 0.18- 0.20- 0.22- 0.24- 0.26- 0.28- 0.30- 0.32- 0.34- 0.36 0.38- 100

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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Show all work and calculations by hand. Please do not use any AI generative tools (I can tell what is AI and what is not). Do not use ChatGPT. Please explain every step and what it means. Thanks

time (s)
1) The USGS collected seismic refraction data in California. The data are shown in the
image below. Interpret the data – be quantitative in determining layer thickness and
velocity, and also determine likely geological material. (25 pts)
Distance (m)
100
75
50
25
25
0
25
50
75
15
0.0
0.02-
0.04-
0.06-
0.08-
0.10-
0.12-
0.14-
0.16-
0.18-
0.20-
0.22-
0.24-
0.26-
0.28-
0.30-
0.32-
0.34-
0.36
0.38-
100
Transcribed Image Text:time (s) 1) The USGS collected seismic refraction data in California. The data are shown in the image below. Interpret the data – be quantitative in determining layer thickness and velocity, and also determine likely geological material. (25 pts) Distance (m) 100 75 50 25 25 0 25 50 75 15 0.0 0.02- 0.04- 0.06- 0.08- 0.10- 0.12- 0.14- 0.16- 0.18- 0.20- 0.22- 0.24- 0.26- 0.28- 0.30- 0.32- 0.34- 0.36 0.38- 100
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