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The surface was formed on the Upper Cretaceous Almond Formation throughout the study area.
This change in facies has been used to map the contact between the Fort Union Formation of Paleocene age in this area, and the Wasatch Formation which was though to be of Eocene age.
This study demonstrates that, as currently mapped, the lower part of the Wasatch Formation is Paleocene in age.
Stratigraphically higher parts of the Wasatch, which presumably contain rocks of latest Paleocene (P6 zone) and earliest Eocene age, were not studied.
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