Bull Run Formation
The Bull Run Formation is a Late Triassic stratigraphic unit in the eastern United States. It is part of the Newark Supergroup, exposed in the Culpeper Basin of Virginia and Maryland. Fossil fish bones and scales have been found in outcrops of the formation's Groveton Member in Manassas National Battlefield Park.
The United States Geological Survey does not formally recognize the Bull Run Formation as a distinct formation, but its validity has been promoted by some paleontologists.
Geology
The Bull Run Formation includes several subunits:Balls Bluff Member : Fluvial sandstones and shales. The oldest and most widespread subunit of the formation. It is more common near the rim of the Culpeper Basin, where the dry lake deposits of the Groveton Member are less prevalent.Groveton Member: Rhythmic playa lake shales and paleosols. Common in the central part of the Culpeper Basin, where it overlies the Balls Bluff Member.Leesburg Member : A conglomerate of limestone and dolomite fragments, outcropping in the northern Culpeper Basin above strata of the Balls Bluff Member.Mountain Run Member : A conglomerate of greenstone fragments outcropping near Cedar Mountain in Culpeper County, Virginia.Haudricks Mountain Member: Sandstones and metamorphic rock fragments outcropping near Haudricks Mountain in the Barboursville Basin.The latter two members were once identified as a separate formation, the Tibbstown Formation. However, later studies argued that they are merely local exposures where the Bull Run Formation takes on eroded rock material from surrounding mountains. The Bull Run Formation is sometimes regarded as part of the Passaic Formation.
Paleobiota
Distinctly rounded stones are common in the Balls Bluff Member, while direct fossil material is more rare. The following vertebrates have been reported from the formation:- Coelacanth scales
- Phytosaur teeth and other isolated bones
- ''Semionotus sp.''