Big Clifty Sandstone

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Big Clifty Sandstone
Stratigraphic range: Mississippian
Big Clifty Sandstone over Girkin Limestone (Upper Mississippian; Dixon Cave Trail, Mammoth Cave National Park, Kentucky, USA) 2 (8329373829).jpg
Big Clifty Sandstone over Girkin Limestone (Upper Mississippian; Dixon Cave Trail, Mammoth Cave National Park, Kentucky)
TypeFormation
Unit ofGolconda Formation[1]
UnderliesHaney Limestone[2]
OverliesGirkin Formation
Lithology
PrimarySandstone
Location
Region Illinois,  Kentucky
Country United States

The Big Clifty Sandstone is a geologic formation in Illinois and Kentucky. It is a subunit of the Golconda Formation[1] in Kentucky and is correlative with the Fraileys Shale[3] to which it grades to in southern Illinois.[4] The Big Clifty and Golconda are part of the Chesterian Series[5] of late Mississippian age. The Big Clifty Sandstone was deposited in deltaic to marginal marine environment by the paleo Michigan River which in modern directions flowed south from the Canadian shield, the sediment source, and then westward depositing sediment across Illinois, Kentucky,[6][7] and Indiana, as the Big Clifty Formation of the .[8] At Mammoth Cave National Park the Big Clifty overlies the Girkin Formation, the uppermost of three cave forming carbonate formations which the Mammoth-Flint Ridge cave system spans.[9] Below the Girkin Formation are the Ste. Genevieve Limestone, and the St. Louis Limestone respectively. The chemically resistant sediments comprising the Big Clifty, and similar siliciclastics, act as a caprock over the dissolving carbonates. The presence of the Big Clifty is one of several contributory factors that create favorable conditions for the formation, and subsequent preservation, of connected cavernous porosity in the Mammoth-Flint Ridge cave system.

The Big Clifty Sandstone also appears as sandstone throughout south-central Kentucky, including the 200-foot-tall (61 m) on the border of Todd County.

References[]

  1. ^ a b "Geolex — Golconda publications". Ngmdb.usgs.gov. Retrieved 30 June 2018.
  2. ^ Sable, E.G. (1964). "Geology of the Constantine quadrangle, Kentucky". Geologic Quadrangle. 302. doi:10.3133/GQ302. ISSN 0375-8117. Wikidata Q61824243.
  3. ^ "Geolex — Fraileys publications". Ngmdb.usgs.gov. Retrieved 30 June 2018.
  4. ^ Treworgy, J.D. (January 1990). Kaskaskia Sequence: Mississippian Valmeyeran and Chesterian Series. Q66309374. Vol. 51. pp. 109–112. doi:10.1306/M51530C10. ISBN 978-1-62981-125-3. ISSN 0271-8529. Wikidata Q66309302.
  5. ^ Treworgy, J.D., and Devera, J.A., 1990, Kaskaskia Sequence Overview: Middle Devonian Series through Chesterian Series, in M.W. Leighton, D.R. Kolata, D.T. Oltz, J.J. Eidel, eds., Interior Cratonic Basins: AAPG Memoir 51, p.109-112
  6. ^ Swann, D.H., 1963, Classification of Genevivian and Chesterian (Late Mississippian) Rocks of Illinois: Illinois State Geological Survey Report of Investigations 216, 91 p.
  7. ^ Treworgy, J.D., 1998, The Illinois Basin-a Tidally and Tectonically influenced Ramp During the Mid-Chesterian Time, Illinois State Geological Survey, Circular 544, 20 p.
  8. ^ "Big Clifty Formation". Igs.indiana.edu. Retrieved 30 June 2018.
  9. ^ Palmer, A.N., 1981, Geologic Guide to Mammoth Cave National Park: Teaneck, N.J., Zephyrus Press, 210 p.


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