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Arkansas Novaculite

Arkansas Novaculite - Includes upper division (Mississippian), middle division (Mississippian and Devonian), and lower division (Devonian)
StateArkansas
NameArkansas Novaculite
Geologic agePhanerozoic | Paleozoic | Devonian-Late Carboniferous Mississippian-Early
Original map labelMDa
CommentsUpper division -massive calcarous novaculite; middle division -dence dark novaculite interbedded with shale; and lower division-massive white nonaculite. Approximately 950 ft. maximum thickness. This area is the "type" occurrence for novaculite. Novaculite refers to a dense cryptocrystalline siliceous sediment similar to chert but characterized by dominance of microcrystalline quartz over chalcedony- distinquished by polygonal triple-point texture.
Primary rock typenovaculite
Secondary rock typeshale
Other rock types
Lithologic constituents
Major
Sedimentary > Chemical > Novaculite (Bed)
Minor
Sedimentary > Clastic > Mudstone > Shale (Bed)
Map references
Haley, B. R., Glick, E. E., Bush, W. V.; Clardy, B. F.; Stone, C. G.; Woodward, M. B., Zachry, D.L., 1993, Geologic Map of Arkansas: U.S.Geological Survey Special Geologic Map. Scale 1:500K
Unit references
Ferguson, J.G., 1920. Outlines of the geology, soils, and minerals of the State of Arkansas: Arkansas State Bureau of Mines, Manufactures and Agriculture,192 pp.
Stone, C. G. and Bush, W. V. 1982, Summary of the geology of the eastern Ouachita Mountains, Arkansas: Guidebook - Arkansas Geological Commission, vol.82-2, 24 pp.
Scull, B. J., 1958, Origin and occurrence of barite in Arkansas: Ark. Geol. and Conserv. Comm. Inf. Circ. 18, 101 pp.
Geographic coverageClark - Garland - Hot Spring - Howard - Montgomery - Pike - Polk - Pulaski - Saline

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