The Alcobaça Formation is a geological formation in Portugal. It dates back to the Oxfordian stage of the Late Jurassic. It is an important source of information on the diversity of Late Jurassic mammals. Many of the fossils were collected from the now disused and flooded Camadas de Guimarota coal mine.
The Grès supérieurs Formation is a geological formation in Laos whose strata date back to the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. It is equivalent to the Khok Kruat Formation of Thailand. Dinosaur remains are among the fossils that have been recovered from the formation.
The Eumeralla Formation is a geological formation in Victoria, Australia whose strata date back to the Early Cretaceous. It is Aptian to Albian in age. Dinosaur remains are among the fossils that have been recovered from the formation, particularly from the Dinosaur Cove locality It is equivalent to the Wonthaggi 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 Saltwick Formation is a Mesozoic geologic formation in Yorkshire and the western North Sea. Fossil stegosaur tracks have been reported from the formation. An indeterminate sauropod has been reported from the formation.
The Zagaje Formation is an Early Jurassic Epoch geologic formation located in Poland.
The Pajarito Formation is a Mesozoic geologic formation in eastern New Mexico and west Texas, primarily shale. Indeterminate fossil ornithischian tracks have been reported from the formation.
The Mecsek Coal Formation is a Mesozoic geologic formation in Hungary. Indeterminate fossil ornithischian tracks have been reported from the formation.
The East Berlin Formation is a Mesozoic geologic formation in New England. Indeterminate fossil ornithischian tracks have been reported from the formation.
The Balls Bluff Formation is a Mesozoic geologic formation in the eastern United States. Indeterminate fossil ornithischian tracks have been reported from the formation.
The Cow Branch Formation is a Mesozoic geologic formation in the eastern United States. Indeterminate fossil ornithischian tracks have been reported from the formation.
The Ansbachersandstein is a Mesozoic geologic formation in Germany. Indeterminate fossil ornithischian tracks have been reported from the formation.
The Abu Agag Formation is a Turonian geologic formation in Egypt and Sudan. Indeterminate fossil ornithischian tracks have been reported from the formation.
The Wangi Formation is a Mesozoic geologic formation in China. Indeterminate fossil dinosaur tracks have been reported from the formation.
The Jinjiang Formation is a Mesozoic geologic formation in China. Indeterminate fossil dinosaur tracks have been reported from the formation.
The El Jume Formation is an Early Cretaceous geologic formation in Argentina. Indeterminate fossil dinosaur tracks have been reported from the formation. The formation, belonging to the El Gigante Group, overlies the Los Riscos Formation and is overlain by the El Toscal Formation. The sandstones and claystones of the formation were deposited in a fluvial environment. Part of the formation was assigned to a new formation, Balde de Leyes Formation in 2015.
The Akaiwa Formation is a Mesozoic geologic formation in central Honshu, Japan. Indeterminate ornithischian fossils are known from the formation. Fossil ornithopod tracks have been reported from the formation. As well as the turtle Kappachelys
The Zhenzhuchong Formation is a Early Jurassic geologic formation in China. Plesiosaur remains are among the fossils that have been recovered from its strata.. Remains of the prosauropod Lufengosaurus huenei have been recovered from this formation As well as dinosaur footprints.
The Kcskehát Limestone is a Jurassic geologic formation in Hungary. Indeterminate fossil Sauropod tracks have been reported from the formation.
