| Pinyon Conglomerate | |
|---|---|
| Stratigraphic range: Maastrichtian–Paleocene PreꞒ Ꞓ O S D C P T J K Pg N | |
| Type | Geological formation |
| Underlies | Harebell Formation |
| Location | |
| Region | North America |
| Extent | Yellowstone National Park |
The Pinyon Conglomerate is a geological formation in Wyoming whose strata date back to the Late Cretaceous and Paleocene. Dinosaur remains are among the fossils that have been recovered from the formation.
Vertebrate paleofauna
See also
References
- Love, J.D. (1973). "Harebell Formation (Upper Cretaceous) and Pinyon Conglomerate (uppermost Cretaceous and Paleocene), northwestern Wyoming". Professional Paper. doi:10.3133/pp734a. ISSN 2330-7102.
- Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574-588. ISBN 0-520-24209-2.
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