Tag Archives: Georgia Geology

Burkett’s Ferry Landing, Ocmulgee River

The site of a historic ferry on the Ocmulgee, this landing now provides public access to the river. It’s truly one of the most appealing areas on the river, just upstream from the confluence with the Oconee and the beginning of the Altamaha River.

Rock outcrops common to the Altamaha Formation are found here as they are in other parts of the county.

Jesse M. Bookhardt recently shared this about Burkett’s Ferry: Burkett’s Ferry is a wonderful place and occupies a special place in my memory. Located in Jeff Davis County just off the old Pioneer Tallahassee Trail, it represents one of several ferries that provided river crossing services. Though not in operation during my time, I remember the site well. Folks from the neighboring communities such as Snipesville often went there fishing, boating, and picnicking. There existed a small spring of cool clear water that seeped from a bank just up stream from the landing. From this pool of fresh water, many fishermen and visitors to the river stopped to drink. It is unknown to me whether the spring still runs or has succumbed to the dynamic forces of nature. Burkett’s Ferry was one of two closely geographically connect fishing spots. Nearby is Pike Creek recorded as Pipe Creek in the original land survey of the area. Both places provided rich fishing waters. Perhaps the “Pipe” referred to a site for making Native American tobacco medicine pipes. Obviously Native Americans once occupied the Burkett’s Ferry site, for in the 1950s when I was a kid, I found pottery and stone artifacts. During the pioneer period, the ferry connected Telfair with Ocmulgeeville, and further to the east Holmesville, the county seat of Appling. When the original plan was made for the old Macon and Brunswick Railroad, it called for the route to cross the Ocmulgee near Burkett’s Ferry. Later the plan was changed and the railroad was scheduled to be built across the Ocmulgee at Lumber City further down stream. Burkett’s Ferry is historically significant to the Ocmulgee and Wiregrass region for it provided much needed access to the hinterland of South Georgia.

 

Altamaha Formation Outcrop, Jeff Davis County

If you’ve ever traveled Georgia Highway 107 between Jacksonville and Snipesville, you’ve undoubtedly noticed these large outcrops near the Coffee/Jeff Davis County line. They’re an extension of the better-known Broxton Rocks, a natural area protected by the Nature Conservancy of Georgia. The area, known as Flat Tub,  is accessible as a Georgia Wildlife Management Area (WMA) and recent covenants have led to further protections of this fascinating resource.

Long thought to be Altamaha Grit, different hypotheses suggest that it could be of Altamaha Formation, but not as “gritty” as other such areas previously identified. Another thesis suggests this may be a more specific “Ocmulgee Formation”, the result of a meteorite impact which may have created the Big Bend of the Ocmulgee.

Whatever the specific geology, it’s certainly an amazing environment, almost alien in comparison to adjacent lands.

 

Rio Piedra Plantation, Mitchell County

This sign marks an entrance, at Turkey Road, to Rio Piedra Plantation. This area of southwest Georgia is nationally known for its Northern Bobwhite (Colinus virginianus) populations and the hunting lodges which cater to the sport.

There is a large field of gigantic chert rocks on the plantation. I’m not quite sure why they’re here. Janet Peek McGill writes: The rock in this picture looks like fossiliferous chert. It is really a very ugly rock on the outside…..all crusted over with crumbly white yuk with often, many fossils though. (which helps with dating the geology of the land and aboriginal peoples) On the inside is a beautiful rock, with chalcedony, vugs, druzy, sometimes hyalite opal, bands of agate and or jasper. It is stunning when faceted and polished. Native Americans frequently used this for knapping for their tools and in the Lee, Dougherty, Baker, Early, Mitchell county area, you often find native American lithic scatter along and near the outcrops of this type of rock.

This is a relatively well-preserved example of one of Georgia’s most iconic rural architectural styles.

Altamaha Iron, Fort Barrington

The dark colors and reds, atypical along the banks of the lower Atlamaha region, are a result of ancient iron deposits.

Providence Canyon, Stewart County

Providence Canyon is actually a series of canyons believed to be named for Providence Methodist Church, which still stands near the state park entrance. Also known as the “Little Grand Canyon”, it was formed by erosion in the early 19th century. Pioneer farmers clear cut much of the land and did little to mitigate the effect of rainwater runoff.

The deepest gullies are about 150 feet from rim to floor.

It’s considered one of Georgia’s Seven Natural Wonders and Providence Canyon State Park is one of my favorite places in Georgia.