Salt deformation in the Paradox region (B-122) Bryce Canyon National Park and understanding the geological context

and understanding the geological context of their discoveries

soaring arches

in a typical Basin and Range setting

with a visual key to make identification simple and accurate

hidden waterfalls

Salt deformation in the Paradox region (B-122) Bryce Canyon National Park and understanding the geological contextBy: H. H. Doelling, C. G. Oviatt, and P. W. Huntoon Bedded salt deposits were identified by the U. S. Department of Energy (DOE) as places suitable to store or dispose of nuclear fuel and high level radioactive waste. The Paradox Basin, with its thick salt beds, was a likely place for study and consideration. Geologic studies were performed to insure that other natural activities in nature would not negate or diminish the advantages of the salt beds.