This list of stratigraphic units with indeterminate dinosaur fossils includes stratigraphic units of formation rank or higher that have produced dinosaur body fossils, although none of these remains have been referred to a specific genus in the scientific literature.
| Name | Location | Description | |
|---|---|---|---|
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
| Monti Prenestini Carbonatic Platform | |||
Description | |||
Description | |||
Description | |||
Description | |||
Description | |||
| Name | Location | Description |
|---|---|---|
Description | ||
Description | ||
| Mugher Mudstone | Description | |
Description | ||
Description | ||
| Name | Location | Description |
|---|---|---|
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
| Khooldzin Svita | Description | |
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
| Name | Location | Description |
|---|---|---|
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
Description | ||
The Tendaguru Formation, or Tendaguru Beds are a highly fossiliferous formation and Lagerstätte located in the Lindi Region of southeastern Tanzania. The formation represents the oldest sedimentary unit of the Mandawa Basin, overlying Neoproterozoic basement, separating by a long hiatus and unconformity. The formation reaches a total sedimentary thickness of more than 110 metres (360 ft). The formation ranges in age from the late Middle Jurassic to the Early Cretaceous, Oxfordian to Hauterivian stages, with the base of the formation possibly extending into the Callovian.
Argiles et Grès à Reptiles Formation also known as the Argiles Rutilantes Formation is an early Maastrichtian French geologic formation in the département of Var preserving the remains of several types of dinosaurs and other extinct organisms.
The Bushveld Sandstone is a geological formation dating to roughly between 201 and 189 million years ago and covering the Carnian to Norian stages. The Bushveld Sandstone is found in Transvaal, South Africa, and is a member of the Stormberg Group. As its name suggests, it consists mainly of sandstone. Fossils of the prosauropod dinosaur Massospondylus have been recovered from the Bushveld Sandstone.
The Foremost Formation is a stratigraphic unit of Late Cretaceous (Campanian) age that underlies much of southern Alberta, Canada. It was named for outcrops in Chin Coulee near the town of Foremost and is known primarily for its dinosaur remains and other fossils.
The St. Mary River Formation is a geologic formation of Late Cretaceous age of the Western Canada Sedimentary Basin in southwestern Alberta and northwesternmost Montana. It was first described from outcrops along the St. Mary River by George Mercer Dawson in 1883, and it takes its name from the river.
The Moreno Hill Formation is a geological formation in western New Mexico whose strata were deposited in the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. The age of the formation is dated between approximately 90.9 to 88.6 million years ago based on detrital zircons.
The Aguja Formation is a geological formation in North America, exposed in Texas, United States and Chihuahua and Coahuila in Mexico, whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. Fossil palms have also been unearthed here.
The Eagle Sandstone, originally the Eagle Formation, is a geological formation in Montana whose strata date back to the Late Cretaceous. It is a light to brownish gray to pale yellow-orange, fine-grained sandstone. It contains areas of crossbedding and local shale members. It contains large sandy calcareous concretions. Its thickness varies from 100 to 350 feet due to the lens nature of the individual sandstone layers and local interbedded sandy shale layers.
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.
The El Gallo Formation is a geological formation in Mexico whose strata date back to the Late Cretaceous, Campanian epoch, specifically dated to 75.21 ± 0.07 Ma and 74.55 ± 0.09 Ma. Dinosaur remains are among the fossils that have been recovered from the formation.
The Argiles de Châtillon is a geologic formation in France. It preserves fossils dating back to the Jurassic period. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
The Benkersandstein is a geologic formation in Germany. It preserves fossils dating back to the Late Triassic (Carnian) period. Fossil theropod tracks have been reported from the formation.
