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?
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!