Bull Run Formation Explained

Bull Run Formation
Type:Geological formation
Age:Norian
~
Period:Norian
Prilithology:Mudstone
Otherlithology:Shale, siltstone
Region:Maryland, Virginia
Coordinates:38.9°N -77.4°W
Paleocoordinates:13.3°N -21.8°W
Unitof:Chatham Group
Subunits:Ball's Bluff & Groveton Members
Extent:Culpeper Basin

The Bull Run Formation is a Late Triassic (Norian) stratigraphic unit in the eastern United States.[1] Fossil fish bones and scales have been found in outcrops of the formation's Groveton Member in Manassas National Battlefield Park.[2] Indeterminate fossil ornithischian tracks have been reported from the formation.[3]

The Bull Run Formation was once considered part of the Culpeper Group of the Newark Supergroup, but the United States Geological Survey no longer formally recognizes this formation (it is abandoned).[4]

Fossil content

The following fossils were reported from the formation:[1]

Ichnofossils

See also

References

Bibliography

Notes and References

  1. http://www.fossilworks.org/cgi-bin/bridge.pl?action=collectionSearch&geological_group=Chatham&formation=Bull%20Run Bull Run Formation
  2. Hunt et al., 2006, p.64
  3. Weishampel et al., 2004, pp.517-607
  4. https://ngmdb.usgs.gov/Geolex/Units/BullRun_715.html Bull Run