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Keyser Formation
Stratigraphic range: Pridoli-Lochkovian
Keyser Formation 522.jpg
Outcrop of the Keyser Formation on U.S. Route 522 in Fulton County, Pennsylvania, north of Warfordsburg
Type Sedimentary
Unit of Helderberg Group
Sub-units Byers Island, Jersey Shore & La Vale Members
Underlies New Creek Limestone and Old Port Formation
Overlies Tonoloway Formation
Thickness 33 m (108 ft) at Allegheny Furnace
Lithology
Primary Limestone
Location
Coordinates 38°18′N 79°36′W / 38.3°N 79.6°W / 38.3; -79.6Coordinates: 38°18′N 79°36′W / 38.3°N 79.6°W / 38.3; -79.6
Approximate paleocoordinates 36°18′S 41°30′W / 36.3°S 41.5°W / -36.3; -41.5
Region Pennsylvania, Maryland, Virginia, West Virginia
Country  United States
Extent Appalachian Mountains
Type section
Named for Keyser, West Virginia
Named by E. O. Ulrich
Year defined 1911

The Late Silurian to Early Devonian Keyser Formation is a mapped limestone bedrock unit in Pennsylvania, Maryland, Virginia, and West Virginia.

Description

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 abundantly fossiliferous, nodular limestone at the base overlies the "calico". Overlying this is 5 to 6 m of fragmental calcarenite containing abundant crinoid columnals. Above the calcarenite is 6 m of fossiliferous, banded calcisiltite. The uppermost 15 m is a sequence alternating between laminated, stromatolitic calcisiltite, and calcilutite and calcisiltite that are argillaceous and fossiliferous.

Depositional environment

The depositional environment of the Keyser is interpreted as shallow marine and tidal flats, occurring in cycles.

Stratigraphy

Contact with Tonoloway Formation is probably conformable, but sharp enough to suggest an unconformity. Upper contact with the Old Port Formation is conformable.

The Keyser was divided into three members by J. W. Head in 1972. These are, from lowest to highest, the Byers Island Member, Jersey Shore Member, and La Vale Member. The type locality of the Byers Island Member is at Selinsgrove, Pennsylvania, where it is 93 feet thick. The type locality of the Jersey Shore Member is at Jersey Shore, Lycoming County, Pennsylvania. The type locality of the La Vale Member is at the Corriganville quarry, Allegany County, Maryland, and is named for the nearby town of La Vale. This nomenclature is accepted by the USGS.

In Virginia and West Virginia the Keyser is divided into Upper and Lower Members by the Big Mountain Shale Member.

Fossil content

Crinoid fragments Keyser Formation
Crinoid fragments at the Old Eldorado Quarry outcrop along I-99, Blair County, PA
Stromatoporoid1 Keyser Formation
Stromatoporoids at the Old Eldorado Quarry outcrop along I-99, Blair County, PA
Newpariscoral
Tabulate coral in the New Enterprise New Paris Quarry on Chestnut Ridge in Bedford County, PA. Probably Halysites.

Notable outcrops

  • Keyser, West Virginia (type section), quarry and roadcut east of the town, on West Virginia Secondary Road 8
  • Old Eldorado Quarry, at Mile Marker 30 along I-99/U.S. Route 220 in Blair County, Pennsylvania
  • Alleghany Furnace Quarry, Altoona, Pennsylvania
  • St. Clairsville/Osterburg Exit of I-99 in Bedford County, Pennsylvania (nearly vertical orientation)
  • Abandoned quarry in Tyrone, Pennsylvania
  • Quarry at Canoe Creek, Pennsylvania
  • New Enterprise New Paris Quarry, Chestnut Ridge, Bedford County, Pennsylvania
  • Roadcut along U.S. Route 30 (Everett bypass) through Warrior Ridge, Bedford County, Pennsylvania
  • Strait Creek section on County Road 629, 1.5 miles south of U.S. Route 220, Strait Creek, Highland County, Virginia
  • Smoke Hole section on West Virginia Route 2, 1.5 miles west of U.S. Route 220, Pendleton County, West Virginia

Age

Relative age dating places the Keyser in the late Silurian to early Devonian, with the transition occurring near the top of the formation. Denkler and Harris used conodont biostratigraphy to confirm this.

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