Clark Quarry
Clark Quarry
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Clark Quarry

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Clark Quarry

Clark Quarry is a paleontological dig site in southern Georgia. The site first discovered fossils by the building of the Brunswick Canal in 1838-1839.

Clark Quarry is a cut and fill fluvial deposit overlying a marine sand, near Brunswick, Georgia, United States in Glynn County. The marine unit is characterized by a well-sorted, subrounded, low sphericity, fine- grained quartz arenite representing sediments of the Princess Anne Terrace. This site is in the pleistocene era on the geologic timescale.

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