How do earthquake waves make these findings possible?

Analysis of the Earth’s internal structure is made possible because earthquakes produce vibrations called seismic waves. These waves travel through the interior of the Earth and can be measured with sensitive detectors called seismographs. Scientists have seismographs set up all over the world to track movement of the Earth’s crust.

Explanation:

a pan containing water is placed in a positio n where it is exposed to a 10 mile per hour wind. the pan contains a uniform depth of 1.27 cm of water, is quite wide, and has a length of 2.44 m in the wind direction. the water in the pan is at a constant temperature of 15.5 °c.

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