Mazarn Shale | |
Type: | Formation |
Age: | Ordovician |
Prilithology: | Shale |
Namedfor: | Mazarn Creek, Montgomery County, Arkansas |
Namedby: | Hugh Dinsmore Miser[1] |
Region: | Arkansas, Oklahoma |
Country: | United States |
Unitof: | none |
Subunits: | none |
Underlies: | Blakely Sandstone |
Overlies: | Crystal Mountain Sandstone |
Thickness: | 1000 to 2500+ feet[2] |
The Mazarn Shale is an Early Ordovician geologic formation in the Ouachita Mountains of Arkansas and Oklahoma. This interval was first described in 1892,[3] but remained unnamed until 1918 as part of a study by U.S. Geological Survey geologist Hugh Dinsmore Miser.[1]
C. wrighti[4]
C. antennarius[4]
D. caduceus[4]
D. caduceus nana[4]
D. filiformis[4]
D. nitidus[4]
D. similis[4]
G. hystrix[4]
P. typus[4]
T. clarkei[4]
T. fruticosus[4]
T. quadribrachiatus[4]
T. pendens[4]
T. serra[4]
T. similis[4]