Logan Formation
Template:Short description Script error: No such module "Infobox".Script error: No such module "Check for unknown parameters".Script error: No such module "Check for conflicting parameters". The Logan Formation is the name given to a Lower Carboniferous (early Osagean) siltstone, sandstone and conglomeratic unit exposed in east-central Ohio and parts of western West Virginia, USA.
Stratigraphy and paleoenvironment
The Logan Formation was named by Andrews (1870) and originally described as a "buff-colored, fine-grained sandstone" above the Waverly Formation and below the Maxville Limestone. Bork and Malcuit (1979) concluded that the Logan Formation was deposited on a shallow marine shelf in a generally transgressing sea. The age of the Logan Formation has been established as early Osagean (Tn3) by the occurrences of brachiopods, ammonoids, conodonts and miospores (Clayton et al., 1998; Matchen and Kammer, 2006).
References
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Conglomerate in the Logan Formation exposed in Wooster, Ohio, USA.
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Brachiopod internal and external molds in the Logan Formation in Wooster, Ohio.
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The bivalve Aviculopecten subcardiformis from the Logan Formation in Wooster, Ohio (external mold).
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Bivalves (Aviculopecten) and brachiopods (Syringothyris) in the Logan Formation in Wooster, Ohio.
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Cross-bedding and scour in the Logan Formation of Jackson County, Ohio.
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Schizodus medinaensis; a bivalve from the Logan Formation in Wooster, Ohio (internal mold).
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Syringothyris sp.; a spiriferinid brachiopod from the Logan Formation in Wooster, Ohio (internal mold).
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Syringothyris external mold with borings; Logan Formation; Wooster, Ohio.
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Syringothyris texta (Hall 1857), dorsal view, internal mold. Lower Carboniferous of Wooster, Ohio.
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Helminthopsis ichnosp.; a trace fossil from the Logan Formation in Wooster, Ohio.
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Crinoid calyx from the Logan Formation in Wooster, Ohio, with a conical platyceratid gastropod (Palaeocapulus acutirostre) attached.