Seismic Refraction

Seismic refraction is a relatively quick and easy way to determine the thickness of the crust.  Click on the below links for tutorials.
Geophysical Exploration
Basic explaination
Encyclopedia

In this case, data from a study conducted in 1965 has been interpreted three different times. Why three times?


Original Study
 

The original experiment went from Hanksville, Utah to Chinle, Arizona  Click here and here to see maps

Three different interpretations of the data:


Click here to see all interpretations together

Let's put it together,  Click here for conclusions!