The Moreno Hill Formation is a geological formation in western New Mexico whose strata were deposited in the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.^[2] The age of the formation is dated between approximately 90.9 to 88.6 million years ago based on detrital zircons.^[1]

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Moreno Hill Formation
Stratigraphic range: Turonian–Coniacian PreꞒ Ꞓ O S D C P T J K Pg N [1]
Type	Geological formation
Underlies	Fence Lake Formation
Overlies	Atarque Sandstone
Thickness	217 meters (712 ft)
Lithology
Primary	Sandstone, Shale
Other	Siltstone, Coal
Location
Coordinates	34.5893°N 108.7592°W / 34.5893; -108.7592
Region	New Mexico
Country	United States
Type section
Named for	Moreno Hill
Named by	McLellan, Haschke, Robinson, Carter, and Medlin
Year defined	1983
Moreno Hill Formation (the United States) Show map of the United States Moreno Hill Formation (New Mexico) Show map of New Mexico

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The formation is a nonmarine coal-bearing formation composed mostly of sandstone and shale with minor siltstone. The shales are brownish gray in color, and the sandstones are discontinuous beds of very pale orange to light brown poorly sorted grains that usually show steep crossbedding. The sandstones are interpreted as channel or splay deposits in a fluvial environment. The shales include thin lenses of bituminous coal, including tonsteins (distinctive thin ash beds). The total maximum thickness is 217 meters (712 ft). It overlies the Atarque Sandstone and is in turn overlain by the Fence Lake Formation.^[3]

Moreno Hill Formation was first named by McLellan and coinvestigators in 1983 for exposures around Moreno Hill in the Salt Lake coal field of western New Mexico. The beds were originally mapped as Mesaverde Group, but were found to be much lower in the stratigraphic column.^[3] The formation is also laterally equivalent to the Tres Hermanos Formation, Pescado Tongue of the Mancos Shale, Gallup Sandstone, and lower Crevasse Canyon Formation. It represents beds southwest of the pinchout of the Pescado Tongue where the Tres Hermanos Formation and Gallup Sandstone are no longer lithologically distinguishable.^[4] It also documents a time of tectonic upheaval, volcanic activities, humid paleoclimate, and North American coastal margin shifts.^[1]

The Moreno Hill Formation was originally thought to be devoid of fossils,^[3] but it has since yielded a diverse vertebrate paleofauna. An indeterminate crocodyliform fossil has been reported.^[4][5]

• List of dinosaur-bearing rock formations