The Heiberg Formation is a geological formation in Northwest Territories, Canada.
The Grès de l'Infralias is a geological formation in France. It dates back to the Rhaetian.
The Marnes Irisees Superieures Formation is a geological formation in France. It dates back to the Late Triassic.
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 Rhaetian sandstone or Rhatsandstein is a geological formation in Germany. It dates back to the "Rhaetian - ?early Hettangian."
The Feuerletten Formation is a geological formation in Germany. It dates back to the late Norian.
The Obere Bunte Mergel is a geological formation in Switzerland. It dates back to the late Norian.
The Laguna Colorada Formation is a geological formation of the Austral Basin in Patagonia, Argentina. The formation belongs to the El Tranquilo Group and dates back to the Early Jurassic, with a maximum age of 192.78 ± 0.14 Ma.
The Mpandi Formation is a geological formation in Zimbabwe. It dates back to the Late Triassic to Early Jurassic.
The Moon-Airel Formation is a geological formation in France. It dates back to the late Rhaetian and early Hettangian.
The Guettioua Formation is a geological formation in Morocco. It dates back to the Middle Jurassic. It largely consists of sandstone, and is of continental origin. It is the lateral equivalent of the marine El Mers Formation.
The Paw Paw Formation is a geological formation in Texas whose strata date back to the late Albian stage of the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.
The Bauxite of Cornet is a geological formation in Romania whose strata date back to the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. It exists as karstic sediments infilling fissures and caves in limestone.
The Almond Formation is a geological formation of Late Cretaceous age in Wyoming. It was deposited in marsh, deltaic, lagoonal, estuarine, and shallow marine environments along the western shore of the Western Interior Seaway. It consists primarily of fine- to medium-grained sandstone, siltstone, shale, and coal. Fossils from the Almond Formation include remains of dinosaurs and plants.
La Bocana Roja Formation is a geological formation in Baja California, Mexico 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 Ansbachersandstein is a Late Triassic (Carnian) geologic formation in Germany. Indeterminate fossil ornithischian tracks have been reported from the formation.
The Lossiemouth Sandstone is a Middle to Late Triassic 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.
The Manassas Sandstone is a Carnian Stage sandstone geological formation in Virginia, United States.
South Africa 
