Culpeper Basin

[1] It lies east of the Appalachian Mountains and extends from the Madison County—Orange County line in Virginia to Frederick, Maryland.

[2] A diverse group of sedimentary rocks including siltstone, sandstone, and conglomerate within the basin were intruded by igneous rocks (primarily diabase), which caused thermal metamorphism at the contact with sedimentary rock.

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.