Stanley Shale
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| Stanley Shale | |
|---|---|
| Stratigraphic range: Mississippian | |
| Type | Formation |
| Unit of | none |
| Sub-units | Hatton Tuff Lentil (AR/OK), Hot Springs Sandstone (AR) Member,[1] Chickasaw Creek Shale Formation (OK), Moyers Formation (OK), Tenmile Creek Formation (OK)[2] |
| Underlies | Jackfork Sandstone |
| Overlies | Arkansas Novaculite |
| Thickness | 3,500 to 10,000+ feet[1] |
| Lithology | |
| Primary | Shale |
| Location | |
| Region | Arkansas, Oklahoma |
| Country | United States |
| Type section | |
| Named for | Stanley, Pushmataha County, Oklahoma |
| Named by | Joseph A. Taff[3] |
The Stanley Shale, or Stanley Group, is a Mississippian stratigraphic unit in the Ouachita Mountains of Arkansas and Oklahoma. First described in Arkansas in 1892,[4] this unit was not named until 1902 by J.A. Taff in his study of the Ouachita Mountains of Oklahoma.[3] Taff assigned the town of Stanley in Pushmataha County, Oklahoma as the type locality, but did not designate a stratotype. After introduction into Arkansas in 1909 by Albert Homer Purdue,[5] the unit was redefined in 1918, when the formation known as the Fork Mountain Slate was abandoned and partially combined into the Stanley Shale.[6] As of 2017, a reference section for the Stanley Shale has yet to be designated.
The Stanley Shale is recognized as a geologic formation with two sub-units in Arkansas, the Hatton Tuff Lentil and the Hot Springs Sandstone Member,[1] however, several others have been proposed. These include the Chickasaw Creek Member,[7] Chickasaw Creek Tuff,[8] Gap Ridge Sandstone Member,[9] Moyers Member,[7] Parker Hill Sandstone Member,[9] Polk County Ash Bed,[10] and Tenmile Creek Member.[7] In 1963, it was first proposed to raise the rank of the Stanley Shale Formation to Group status in Arkansas,[11] with proposed sub-units consisting of the Chickasaw Creek Formation, Moyers Formation (with the Gap Ridge Sandstone and Parker Hill Sandstone Members), and Ten Mile Creek Formation.[12] However, the proposal was not accepted and the unit remained as a formation.
In Oklahoma, this unit is recognized as a group called the Stanley Group composed of three formations: the Chickasaw Creek Shale Formation, the Moyers Formation, and the Tenmile Creek Formation. The Hatton Tuff Lentil, recognized in Arkansas, is also in Oklahoma as a unit of the Tenmile Creek Formation. Several informal members have been noted including the Smithville chert lentil, the Faith chert member, and the Chickasaw Creek tuff among others [2]
Mining in the Stanley Shale is limited to cinnabar, barite, and quartz. Cinnabar is primarily used for mercury, however, production in Arkansas essentially ended by the mid-20th century. Barite mining, mostly useful for oil and gas drilling fluid, is ongoing.[13]
