Ringbone Formation
Appearance
Ringbone Formation | |
---|---|
Stratigraphic range: Campanian ~ | |
Type | Geological formation |
Lithology | |
Primary | Mudstone |
Other | Sandstone |
Location | |
Coordinates | 31°54′N 108°30′W / 31.9°N 108.5°W |
Approximate paleocoordinates | 39°18′N 80°42′W / 39.3°N 80.7°W |
Region | New Mexico |
Country | United States |
The Ringbone Formation is a Campanian geologic formation in New Mexico. The formation comprises mudstones and yellow sandstones deposited in a lacustrine to deltaic environment.[1] Dinosaur remains of tyrannosaurs and hadrosaurs are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.[2]
See also
References
- ^ Little Hatchet Mountains at Fossilworks.org
- ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
Bibliography
Further reading
- S. G. Lucas, G. Basabilvazo, and T. F. Lawson. 1990. Late Cretaceous dinosaur from the Ringbone Formation, southwestern New Mexico, USA. Cretaceous Research 11:343-349