Reservoir characterization of clastic cycle sequences in the Paradox Formation of the Hermosa group, Paradox Basin, Utah (OFR-543) SH-6B late Pleistocene Lake Bonneville

late Pleistocene Lake Bonneville

but observations indicate that movement likely started in 1997 or 1998 when other nearby landslides reactivated

At twenty special sites in this timeless landscape

slab houses

Reservoir characterization of clastic cycle sequences in the Paradox Formation of the Hermosa group, Paradox Basin, Utah (OFR-543) SH-6B late Pleistocene Lake BonnevilleBy: B. D. Trudgill and W. C. Arbuckle This extensive report includes maps and correlations of the evaporite facies within the Pennsylvanian Paradox Formation throughout the northern Paradox Basin. This includes correlation of individual evaporite cycles and their respective clastic zones. The resulting associations are used to better understand the cyclicity of the Paradox Formation and its relationship to the structural development and evolution of