is found in Onion Creek where the peculiar geology of the salt-dominated formation is on full display. The light-colored gypsum caprock is highly structurally distorted, demonstrating the plastic nature of the buoyant salt body as it rises and displaces other clastic rocks in the geologic section.
View eastward, across the Onion Creek diapir. The Paradox Formation (Middle Pennsylvanian (315.2Ma - 307Ma)) is the light-colored unit in contact with the red beds of the Cutler Formation (Lower Permian (298.9Ma - 273.01Ma)).