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From Wikipedia, the free encyclopedia
The Cambrian Chickies Formation is a mapped bedrock unit in Pennsylvania, New Jersey, and Maryland. It is named for Chickies Rock, north of Columbia, Pennsylvania along the Susquehanna River.
| Chickies Formation | |
|---|---|
| Stratigraphic range: Cambrian | |
Chickies Rock (1892) | |
| Type | Metamorphic |
| Sub-units | Hellam Conglomerate Member |
| Lithology | |
| Primary | Quartzite |
| Other | Slate, schist |
| Location | |
| Region | Pennsylvania, New Jersey, Maryland |
| Country |  United States |
| Extent | Mid-Atlantic United States |
| Type section | |
| Named for | Chickies Rock |
| Named by | J. Peter Lesley |
| Year defined | 1876 |
The Chickies Formation is described as a light-gray to white, hard, massive quartzite and quartz schist with thin interbedded dark slate at the top. Included at the base is the Hellam Conglomerate Member. It is a rare metamorphic rock that has fossils; Skolithos is found throughout the formation.[1]
Relative age dating places the Chickies in the Lower Cambrian Period, deposited between 542 and 520 million years ago (±2 million years).[2]
The Chickies is quarried as a building stone and for aggregate. The stone used to build the restrooms at Valley Forge National Historical Park is Chickies quartzite.[3]
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