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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.
Keyser, the county seat of Mineral County, is located on the North Branch of the Potomac River at its juncture with New Creek in the Eastern Panhandle of West Virginia. Throughout the centuries, the town went through a series of name changes, but was ultimately named after William Keyser, a Baltimore and Ohio Railroad official.
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Jim Thome, a baseball Hall of Famer and Limestone grad, again wore Rockets blue and served as first base coach in a high school game in LaGrange Park.
Oct. 1—WEIRTON, W.Va. — Weir tallied more than 400 yards and seven rushing touchdowns to pull away from No. 5 Keyser, 49-21, on Friday night. Keyser (3-2) trailed 15-7 after the first quarter ...
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.
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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.