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The Keyser is a nodular limestone overlain by thick- and thin-bedded limestone and laminated limestone at its type locality in Keyser, West Virginia . In central Pennsylvania, the basal "calico" limestone is a fossiliferous, medium-light- to medium-gray very thick bedded calcilutite containing numerous small irregular patches of clear calcite.
The Keyser Limestone Formation is a geologic formation in West Virginia. It preserves fossils dating back to the Silurian period. See also. Earth sciences portal; Paleontology portal; List of fossiliferous stratigraphic units in West Virginia; References. Various Contributors to the Paleobiology Database.
The Corriganville Limestone was first described by J. W. Head in 1972 as part of the Helderberg Group in Allegany County, Maryland, as a gray limestone with chert. C. R. Wood first mapped it as part of the Old Port Formation in Pennsylvania. The type locality is a railroad cut 0.3 mi southeast of Corriganville, Alleghany County, Maryland.
Named for. Tonoloway Ridge, Rock Ford, WV. Named by. E. O. Ulrich, 1911 [2] The Late Silurian Tonoloway Formation is a mapped limestone bedrock unit in Pennsylvania, Maryland, Virginia and West Virginia. The Tonoloway is roughly equivalent to the Salina group that is found to the north and west.
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Horse - Also known as Dead Horse Cave, it is located 1,000 yards (910 m) south of Twiggs Cave, near the Twiggtown-Spring Gap road. Developed in the Favosites zone of the Keyser limestone at 1,440 feet (440 m) elevation. The cave is relatively shallow, with 8 to 10 feet of overburden at the entrance room.
Greenbrier River. The Greenbrier Limestone, also known locally as the "Big Lime", is an extensive limestone unit deposited during the Middle Mississippian Epoch (345.3 ± 2.1 – 326.4 ± 1.6 Ma), part of the Carboniferous Period. This rock stratum is present below ground in much of West Virginia and neighboring Kentucky, and extends somewhat ...
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