Southeastern Section–56th Annual Meeting (29–30 March 2007)
Paper No. 38-1
Presentation Time: 1:00 PM-5:00 PM


KING, David T. Jr, Geology, Auburn University, Dept Geology - 210 Petrie Hall, Auburn, AL 36849,, JOHNSON, Reuben C., Dept. Geology, Auburn Univ, Auburn, AL 36849, PETRUNY, Lucille W., Astra Terra Research, Auburn, AL 36831-3323, HAMES, Willis, Geology, Auburn University, Auburn, AL 36849, and NEATHERY, Thornton L., Neathery and Associates, Tuscaloosa, AL 35404

Wetumpka impact structure is a 7.6 km diameter, semi-circular feature of the coastal plain-piedmont boundary in central Alabama. It is possible that the extant structure is but the inner bowl of a larger impact feature, which has been extensively eroded. The stratigraphic age of this feature is near the Campanian-Santonian boundary during Late Cretaceous. Wetumpka was a marine impact event in the epicontinental Gulf of Mexico. This structure exhibits telltale features of marine impact in 30-100 m of water, including aqueous rim-collapse breccias and structure-filling marine-resurge megabreccias. The lower parts of the drilled structure-filling materials contain impact breccias and other impactites with pervasive shock-metamorphosed quartz and feldspar. Ecosystem perturbation associated with this event was locally devastating, but did not rise to the level of producing biostratigraphic effects. Ejecta from Wetumpka are not known, but are predicted to occur in the lower part of the Mooreville Chalk and laterally equivalent units in the Gulf coastal plain. Distal effects such as tsunami are not known, but the coeval Alabama-Georgia clastic dike injection event may be related to the earthquake effects of Wetumpka.

Southeastern Section–56th Annual Meeting (29–30 March 2007)
General Information for this Meeting
Session No. 38
Oh! Southern Skies: Latest Results in Southeastern Planetary Science
Hyatt Regency Savannah on the Historic Riverfront: Harborside West
1:00 PM-5:00 PM, Friday, 30 March 2007

Geological Society of America Abstracts with Programs, Vol. 39, No. 2, p. 97

© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.