The Groveton Member of the Bull Run Formation is exposed there.[1] The formation has produced disarticulated fish remains including isolated bones and scales.[1]
The large body of diabase in central Montgomery County, Maryland, is known as the Boyds Sill,[4] named after the town of Boyds.
^Geologic history and stratigraphy of the Triassic-Jurassic Culpeper Basin, Virginia, R. C. Lindholm. GSA Bulletin (1979) 90 (11_Part_II): 1702โ1736. https://doi.org/10.1130/GSAB-P2-90-1702
^Fisher, G. W., 1964, The Triassic rocks of Montgomery County. In Geology of Howard and Montgomery Counties, Maryland Geological Survey, Baltimore, Maryland, 1964.)
References
Hunt, ReBecca K., Vincent L. Santucci and Jason Kenworthy. 2006. "A preliminary inventory of fossil fish from National Park Service units." in S.G. Lucas, J.A. Spielmann, P.M. Hester, J.P. Kenworthy, and V.L. Santucci (ed.s), Fossils from Federal Lands. New Mexico Museum of Natural History and Science Bulletin 34, pp. 63โ69.