Tonoloway Formation

Geologic formation in the United States From Wikipedia, the free encyclopedia

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.

Typesedimentary
Thickness250+/-20 m
Quick facts Type, Underlies ...
Tonoloway Formation
Stratigraphic range: Pridoli[1]
A Tonoloway limestone "fin" known as Blue Rock, Smoke Hole Canyon, West Virginia
Typesedimentary
UnderliesKeyser Formation
OverliesWills Creek Formation
Thickness250+/-20 m
Lithology
Primarylimestone
Othershale
Location
RegionAppalachian Mountains
ExtentPennsylvania, Maryland, Virginia, West Virginia
Type section
Named forTonoloway Ridge, Rock Ford, WV
Named byE. O. Ulrich, 1911[2]
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Description

The basal 50 m consists of medium-dark-gray laminated to thin-bedded calcisiltite with shale partings and interbeds. Overlying 5 m are light-yellowish-gray to olive-gray mudstone and shale. Above this interval are 75 m of laminated calcisiltite with interbeds of thick to very thick bedded calcisiltite. The remainder of the formation is cyclic, consisting of three or four resistant ledges of laminated limestone and shale. Uppermost 20 m contains a variety of limestones. Lower contact with the Wills Creek is probably conformable. Upper contact is conformable and undulatory, occurring at the base of the "calico" limestone of the Keyser Formation.[3]

Depositional environment

The depositional environment of the Tonoloway is interpreted as shallow marine.

Notable exposures

Age

Relative age dating places the Tonoloway in the late Silurian.

References

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