The Menefee Formation consists of
fluvial sandstone,
shale, and
coal. Based on
ammonite biostratigraphy, the age of the Menefee Formation can be constrained to 84.2-79 million years (
Ma), based on the presence of
Baculites perplexus in the overlying
Cliff House Sandstone, and ammonites from the late
Santonian in the underlying
Point Lookout Sandstone. Named members include a lower Cleary Coal Member and an upper Allison Member. The
Mesaverde Group in the
San Juan Basin records a
marine regression-
transgression sequence of the western margin of the
Western Interior Seaway. The Menefee Formation was deposited at the peak of the regression as coastal
river delta and swamp sediments, and includes numerous coal beds. The formation is exposed at
Chaco Canyon National Park, where many of the coal beds have been burned to produce distinctive red cinder outcrops. ==Fossils==