The data is in the strata
Shown below is a well-developed flooding surface in carbonate strata. Note the sharp contact between dissimilar facies at the hammer head, with shallow subtidal facies below the hammer and deep subtidal above. This photography was taken in the Middle Ordovician Chickamauga Group near Fort Oglethorpe, Georgia.
Return to parasequences
Comments or questions? Please contact Steven Holland at stratum@uga.edu
All original material Copyright 2008. No part of this site may be reproduced without written permission.
The content and opinions expressed on this web page do not necessarily reflect the views of
nor are they endorsed by the University of Georgia or the University System of Georgia.