Strata of nonmarine sediments are pictured just across the state line in Phenix City, Alabama. Alternating layers of marine and nonmarine rock formations in the Coastal Plain reveal that long-term fluctuations in sea level occurred in Georgia throughout the Late Cretaceous period.
Photograph by Pamela J. W. Gore
The New Georgia Encyclopedia does not hold the copyright for this media resource and can neither grant nor deny permission to republish or reproduce the image online or in print. All requests for permission to publish or reproduce the resource must be submitted to the rights holder.
