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Exposed bedrock ranges from the Middle Jurassic to Late Cretaceous in age, includes (in ascending order) the Carmel Formation (part), Entrada Sandstone, Curtis Formation, Summerville Formation, Morrison Formation, Cedar Mountain Formation, Dakota Formation, and the Mancos Shale (part), and is about 3700 feet (1200 m) thick. The rocks of the quadrangle dip gently northwestward from the large San Rafael Swell anticline (to the southeast) into the Wasatch Plateau syncline (to the northwest). Quaternary surficial deposits of Holocene and Pleistocene age include varieties of alluvium, eolian, mass-movement, and mixed-environment deposits. No mineral commodities are known to have been produced from the quadrangle area. 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