Abstract
Waltman Arch, a transbasinal arch that trends northward across the Wind River Basin of central Wyoming, is overridden by the Owl Creek Thrust at its northern terminus (Figures 1 and 2). Fields along Waltman Arch produce from multiple stacked sandstone pays in the Fort Union, Lance, Meeteetse, Mesa Verde, Frontier, Muddy, and Lakota Formations (Figures 3 and 4). To the northwest, in Madden Field, there is excellent production from deeper Madison carbonates.
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