Culpeper Basin

The Culpeper Basin is one of the Newark Supergroup's Triassic rift basins.^[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.^[3]

Geologic map of Culpeper Basin from USGS, 1983
link to publication.

The Culpeper Basin is nearly continuous with the Gettysburg Basin to the north and with the Barboursville Basin to the south.

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.

• 
  Jurassic diabase boulders in the Culpeper Basin northeast of Dulles Airport
• 
  Balls Bluff Siltstone with diabase intrusion, northern face of Luck Stone Quarry, Manassas
• 
  Limestone conglomerate of Leesburg Member
• 
  Another sample of limestone conglomerate
• 
  Sandstone from southwest the Boyds Sill in Montgomery County, Maryland
• 
  Unnamed stream exposing diabase of Boyds Sill, Hoyles Mill Trail, Montgomery County, Maryland