Clark Quarry Explained
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.[1] [2]
Geology
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.[3] This site is in the pleistocene era on the geologic timescale.
Fossils
External links
Notes and References
- Joshua L. Clark. Kelly A. Clark. Alfred J. Mead. Dennis Parmley. Robert A. Bahn. A Preliminary Description of the Pleistocene Herpetofauna from Clark Quarry, Brunswick, Georgia. Georgia Journal of Science. 1 April 2005. 63. 1. 31. 12 March 2011. https://web.archive.org/web/20110719201914/http://facstaff.gpc.edu/~jaliff/GAJsci%2063-1.pdf. 19 July 2011. dead.
- Book: Cooper, J. Hamilton. Proceedings of the Geological Society of London. 1846. Oxford University. London. 33–34.
- Web site: Tenth Annual GCSU Student Research Conference. Georgia College and Georgia State University. 12 March 2011. 7. 16 March 2007. https://web.archive.org/web/20110719200655/http://www.gcsu.edu/engagement/studentresearch/docs/10th_Annual_SRC_Spring_2007.pdf. 19 July 2011. dead.
- Web site: Gelbart. Mark. Shit-eating Sharks and Fish of the Cretaceous. 15 October 2010. 12 March 2011.
- Robert A. Bahn. Alfred J. Mead. BISON LATIFRONS (ARTIODACTYLA) FROM THE PLEIS- TOCENE OF BRUNSWICK, GEORGIA. Georgia Journal of Sciences. 1 April 2005. 63. 1. 31. 12 March 2011. https://web.archive.org/web/20110719201914/http://facstaff.gpc.edu/~jaliff/GAJsci%2063-1.pdf. 19 July 2011. dead.