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.