Isopachs are lines that connect points where there is an equal amount of thickness of a geologic formation. The map shown above is of the Upper Hutchinson Salt and Overlying Permian strata beneath Hutchinson, Kansas. It is of the interval between markers S3/M7 and S4. The contour interval is 2 feet.
Source URL: http://www.kgs.ku.edu/PRS/publication/2003/ofr2003-66/figure4.html
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