The Lameta Formation is a sedimentary rock formation found in Madhya Pradesh, Gujarat, and Maharashtra, India. It is of Maastrichtian age, and is notable for its dinosaur fossils. Many dubious names have been created for isolated bones, but several genera of dinosaurs from these rocks are well-supported, including the titanosaur sauropod Isisaurus and the abelisaurs Indosaurus, Indosuchus, Laevisuchus, and Rajasaurus.
The Löwenstein Formation is a lithostratigraphic formation of the Keuper in Germany. It is underlain by the Mainhardt Formation and overlain by the Trossingen Formation. It dates back to the middle Norian.
The Arén Formation or Arén Sandstone Formation is a geological formation in Arén, Spain whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.
The Trichinopoly Group is a geological formation in India whose strata date back to the Late Cretaceous. It lies between the Ootatoor and Ariyalur groups. It is broad in its southern extremity but thins as it gradually proceeds northwards as it ultimately meets the Ariyalur group. Dinosaur remains are among the fossils that have been recovered from the formation.
The Viñita Formation is a geological formation in Coquimbo, Chile, whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.
The Kuangyuan Series is a Mesozoic geologic formation in Szechuan, China. Dinosaur remains are among the fossils that have been recovered from the formation.
The Mitsuse Formation is a Mesozoic geologic formation in Japan. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
The Pictured Cliffs Formation is a Campanian geologic formation in New Mexico. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
The Raritan Formation is a Mesozoic geologic formation. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
The Tiki Formation is a Mesozoic geologic formation in India. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
The Williams Fork Formation is a Mesozoic geologic formation. Dinosaur remains are among the fossils, most notably an unnamed chasmosaurine ceratopsian, that have been recovered from the formation, although none have yet been referred to a specific genus.
The Ampthill Clay is a Mesozoic geologic formation in southern England. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation.
The Mowry Shale is a Late Cretaceous geologic formation. The formation was named for Mowrie Creek, northwest of Buffalo in Johnson County, Wyoming. The Mowry outcrops or occurs at depth in parts of Colorado, Montana, North Dakota, South Dakota, Utah and Wyoming. It occurs within the following geologic regions:
The Turney Ranch Formation is a Mesozoic geologic formation. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation.
The Sengoku Formation is an Early Cretaceous geologic formation. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation.
The Baños del Flaco Formation is a Mesozoic geologic formation in central Chile. Fossil ornithopod tracks have been reported from the formation.
The Marnes Rouges Inferieures Formation is a Mesozoic geologic formation in France. Fossil dinosaurs, dinosaur eggs and avialian stem-birds have been reported from the formation.
The Sânpetru Formation is a Mesozoic geologic formation. Dinosaur remains are among the fossils that have been recovered from the formation. It is located in Romania, near Sânpetru village, part of Sântămăria-Orlea commune. It forms a component of the Hațeg Island fauna.
The Lossiemouth Sandstone Formation is a Late Triassic (Ladinian–Norian) age geological formation. It is exposed on the south side of the Moray Firth near Lossiemouth and near Golspie in Sutherland. Dinosaur remains are among the fossils that have been recovered from the formation.
