Cedarpelta is a extinct genus of basal ankylosaurid dinosaur from Utah that lived during the Late Cretaceous period (Cenomanian to lower Turonian stage, 98.2 to 93 Ma) in what is now the Mussentuchit Member of the Cedar Mountain Formation. The type and only species, Cedarpelta bilbeyhallorum, is known from multiple specimens including partial skulls and postcranial material. It was named in 2001 by Kenneth Carpenter, James Kirkland, Don Burge, and John Bird. Cedarpelta has an estimated length of 7 metres (23 feet) and weight of 5 tonnes (11,023 lbs). The skull of Cedarpelta lacks extensive cranial ornamentation and is one of the only known ankylosaurs with individual skull bones that are not completely fused together. Discovery and naming The partial remains of an ankylosaur were discovered by Evan Hall and Sue Ann Bilbey at the CEM site near the Price River in Carbon County, Utah while they were visiting an excavation in the surrounding area. The site was originally interpreted as being from the top of the Ruby Ranch Member of the Cedar Mountain Formation, but was later interpreted as being from the bottom of the Mussentuchit Member. The age of the layer was originally thought to have been 104.46 ± 0.95 Ma, but more recent estimates date it to 98.2 ± 0.6 to 93 Ma. In 1998, the discovery was reported by Kenneth Carpenter and James Kirkland. In 2001, it was subsequently described, along with other material, by Kenneth Carpenter, James Kirkland, Don Burge, and John Bird. The holotype specimen, CEUM 12360, consists of a partial skull that is missing the snout and lower jaws. Numerous osteoderms, postcranial material and a disarticulated skull were designated as paratype specimens. Both holotype and paratype specimens represent at least three individuals and are currently housed at the College of Eastern Utah, Prehistoric Museum, Utah. The generic name, Cedarpelta, is derived from the Cedar Mountain Formation and the Greek word "pelte" (small shield). The specific name, bilbeyhallorum, honours Sue Ann Bilbey and Evan Hall, who discovered the remains of Cedarpelta. In 2008, additional specimens were referred to Cedarpelta from the Price River II Quarry, which is about 24.5 km southeast of Price River, Utah and at the base of the Mussentuchit Member. The quarry also produced specimens pertaining to four individuals of a brachiosaurid, an iguanodontian, a turtle, a pterosaur, and specimens of the nodosaurid Peloroplites. The referred material includes: CEUM 10396, a