Much of our understanding of the character of Earth’s interior comes from analyzing seismic waves that travel through Earth. As these waves move through Earth’s interior, they may pass through, bounce off (reflect), or bend (refract) at boundaries between different rock types. The time it takes a seismic wave to travel from a source in one location to a recording station at another location can be used to decipher the internal structure of Earth. Identify three similar methods that are commonly used to view the interior of objects in daily life without cutting or breaking them open.
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