The Boquillas Formation is a geologic formation deposited during the Late Cretaceous in modern-day West Texas. It is typically composed of alternating marls and limestones with thin volcanic ash beds (bentonites). It was named for outcrops near the former Boquillas post office in Big Bend National Park. The term Boquillas Formation has been used for rocks that outcrop from Del Rio, Texas to as far west as Doña Ana County, New Mexico.Lovejoy, E.M.P., 1976, Geology of Cerro de Cristo Rey uplift, Chihuahua and New Mexico: New Mexico Bureau of Mines and Mineral Resources Memoir, no. 31.
Vertebrate fossils found in the Boquillas Formation include mosasaurs, fish bones, and shark's teeth.Gorden L. Bell, Jr., Kenneth R. Barnes and Michael J. Polcyn (2013) Late Cretaceous mosasauroids (Reptilia, Squamata) of the BigBend region in Texas, USA. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, Available onCJO 2013 doi:10.1017/S1755691013000406Hunt, ReBecca K., Vincent L. Santucci and Jason Kenworthy (2006) A preliminary inventory of fossil fish from National Park Service units, in S.G. Lucas, J.A. Spielmann, P.M. Hester, J.P. Kenworthy, and V.L. Santucci (eds.), Fossils from Federal Lands. New Mexico Museum of Natural History and Science Bulletin 34, p. 63–69. Invertebrate fossils found in the formation include ammonites, swimming crinoids, inoceramid clams, sea urchins, oysters, and foraminifera
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