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- Holston_Formation abstract "The Holston Formation, alternately known as the Holston Limestone, is a stratigraphic unit of Ordovician age within the Chickamauga Group in the Ridge-and-Valley physiographic province of the southeastern United States. A 120-mile (190 km) long outcrop belt of the Holston in East Tennessee is the source of the decorative building stone known as Tennessee marble.Near Knoxville the Holston Formation is about 400 feet (120 m) thick but it thins toward the southwest; near Cleveland, Tennessee it is only 200 feet thick. The rock that is quarried for marble is a highly pure (97% CaCO3) crystalline limestone, pink to cedar-red in color.".
- Holston_Formation thumbnail New_York_Public_Library_Lion-27527.jpg?width=300.
- Holston_Formation wikiPageExternalLink mineral_commodities_5.html.
- Holston_Formation wikiPageExternalLink knoxvilles-marble-past.
- Holston_Formation wikiPageID "1920278".
- Holston_Formation wikiPageRevisionID "591036672".
- Holston_Formation hasPhotoCollection Holston_Formation.
- Holston_Formation subject Category:Geology_of_Tennessee.
- Holston_Formation subject Category:Ordovician_geologic_formations.
- Holston_Formation type Abstraction100002137.
- Holston_Formation type Arrangement107938773.
- Holston_Formation type Formation108426461.
- Holston_Formation type Group100031264.
- Holston_Formation type OrdovicianGeologicFormations.
- Holston_Formation comment "The Holston Formation, alternately known as the Holston Limestone, is a stratigraphic unit of Ordovician age within the Chickamauga Group in the Ridge-and-Valley physiographic province of the southeastern United States.".
- Holston_Formation label "Holston Formation".
- Holston_Formation sameAs m.0665n8.
- Holston_Formation sameAs Q5884464.
- Holston_Formation sameAs Q5884464.
- Holston_Formation sameAs Holston_Formation.
- Holston_Formation wasDerivedFrom Holston_Formation?oldid=591036672.
- Holston_Formation depiction New_York_Public_Library_Lion-27527.jpg.
- Holston_Formation isPrimaryTopicOf Holston_Formation.
