The Blakely Sandstone is a Middle Ordovician geologic formation in the Ouachita Mountains of Arkansas and Oklahoma. First described in 1892,[3] this unit was not named until 1909 by Albert Homer Purdue in his study of the Ouachita Mountains of Arkansas. Purdue had initially named this unit the Caddo Shale at a 1907 Geological Society of America meeting,[4] but later redefined and renamed the unit as the Ouachita Shale.[5] He again renamed the unit to the Blakely Sandstone in a letter to Edward Oscar Ulrich, to which Ulrich used in a 1911 publication, becoming the first reference using this name.[2] Ulrich assigned the Blakely Mountain in Garland County, Arkansas as the type locality, but did not designate a stratotype. As of 2017, a reference section for this unit has yet to be designated.
Blakely Sandstone | |
---|---|
Stratigraphic range: Ordovician | |
Type | Formation |
Unit of | none |
Sub-units | none |
Underlies | Womble Shale |
Overlies | Mazarn Shale |
Thickness | up to 700 feet[1] |
Lithology | |
Primary | Sandstone |
Location | |
Region | Arkansas, Oklahoma |
Country | United States |
Type section | |
Named for | Blakely Mountain, Garland County, Arkansas |
Named by | Albert Homer Purdue[2] |
Paleofauna
Conodonts
- C. horridus[6]
- Hisiodella
- H. holodentata[6]
- Leptochirognathus
- L. quadratus[6]
- Paraprioniodus
- P. costatus[6]
- P. aculeatus[6]
Graptolites
- Glossograptus