Earth:Blaylock Sandstone

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Blaylock Sandstone
Stratigraphic range: Silurian
TypeFormation
Unit ofnone
Sub-unitsnone
UnderliesMissouri Mountain Shale
OverliesPolk Creek Shale
Thicknessup to 1200 feet[1]
Lithology
PrimarySandstone
Location
RegionArkansas, Oklahoma
CountryUnited States
Type section
Named forBlaylock Mountain, Montgomery County, Arkansas
Named byAlbert Homer Purdue[2][3]

The Blaylock Sandstone is a Silurian geologic formation in the Ouachita Mountains of Arkansas and Oklahoma. First described in 1892,[4] this unit was not named until 1909 by Albert Homer Purdue in his study of the Ouachita Mountains of Arkansas.[2][3] Purdue assigned the Blaylock Mountain in Montgomery 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.

Paleofauna

D. decussatus[5]
  • Gladiograptus
G. perlatus[5]
M. argutus[5]
M. distans[5]
M. gregarius[5]

See also

  • List of fossiliferous stratigraphic units in Arkansas
  • Paleontology in Arkansas

References

  1. McFarland, John David (2004). "Stratigraphic summary of Arkansas". Arkansas Geological Commission Information Circular 36: 20–21. http://geology.ar.gov/pdf/IC-36_v.pdf. Retrieved 2018-01-09. 
  2. 2.0 2.1 Purdue, A.H. (1909). Slates of Arkansas. Geological Survey of Arkansas. pp. 30, 35. 
  3. 3.0 3.1 Purdue, A.H. (1909). "Structure and stratigraphy of the Ouachita Ordovician area, Arkansas (abstract)". Bulletin of the Geological Society of America 19: 556–557. 
  4. Griswold, L.S. (1892). "Whetstones and the novaculites". Annual Report of the Geological Survey of Arkansas for 1890 3. 
  5. 5.0 5.1 5.2 5.3 5.4 5.5 Miser, Hugh D.; Purdue, A.H. (1929). "Geology of the De Queen and Caddo Gap quadrangles, Arkansas". U.S. Geological Survey Bulletin 808: 45.