Eutawville in Orangeburg County, South Carolina — The American South (South Atlantic)
Santee Limestone / Limestone and Marl Formations
Photographed By Mike Stroud, August 15, 2009
1. Santee Limestone Marker
Inscription.
Santee Limestone, also, Limestone and Marl Formations. . marker Front:
Santee Limestone. Sir Charles Lyell (1797-1875), noted British geologist, visited S.C. in 1842 and described its geology in his Travels in North America..., published in several editions. He named the bedrock limestone underlying this area "Santee Limestone." Lyell estimated Santee Limestone to date from the Eocene epoch, more than 40 million years ago., Marker Reverse:
Limestone and Marl Formations. Many kinds of fossil marine animals are found embedded in Santee Limestone. This limestone, in solution, forms sinks and subsurface caves. Eutaw Springs, now flooded by Lake Marion, flowed from such channels. An impure limestone-bases clay known as "Cooper Marl" overlies Santee Limestone throughout the lowcountry. Both are primary raw materials in portland cement produced nearby.
marker Front:
Santee Limestone
Sir Charles Lyell (1797-1875), noted British geologist, visited S.C. in 1842 and described its geology in his Travels in North America..., published in several editions. He named the bedrock limestone underlying this area "Santee Limestone." Lyell estimated Santee Limestone to date from the Eocene epoch, more than 40 million years ago.
Marker Reverse:
Limestone and Marl Formations
Many kinds of fossil marine animals are found embedded in Santee Limestone. This limestone, in solution, forms sinks and subsurface caves. Eutaw Springs, now flooded by Lake Marion, flowed from such channels. An impure limestone-bases clay known as "Cooper Marl" overlies Santee Limestone throughout the lowcountry. Both are primary raw materials in portland cement produced nearby.
Erected 2004 by the Carolina Geological Society, replacing marker erected in 1964 by the Division of State Parks, S.C. Commission of Forestry. (Marker Number 38-29.)
Topics. This historical marker is listed in these topic lists: Industry & Commerce • Natural Features. A significant historical year for this entry is 1842.
Location. 33° 24.485′ N, 80° 17.901′ W. Marker is in Eutawville
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, South Carolina, in Orangeburg County. Marker can be reached from Old Number Six Highway (State Highway 6 / 45) near Fredcon Road, on the left when traveling east. Located on the site of the Eutaw Springs Battleground park, shoreline of Lake Marion. Touch for map. Marker is in this post office area: Eutawville SC 29048, United States of America. Touch for directions.
Also see . . . Sir Charles Lyell, Wikipedia entry. He was the foremost geologist of his day, and an influence on the young Charles Darwin. (Submitted on August 28, 2009, by Mike Stroud of Bluffton, South Carolina.)
Photographed By Mike Stroud, August 15, 2009
2. Limestone and Marl Formations Marker
Photographed By Mike Stroud, August 15, 2009
3. Santee Limestone / Limestone and Marl Formations Marker, Lake Marion seen in background
Photographed By Mike Stroud, August 15, 2009
4. Santee Limestone / Limestone and Marl Formations Marker along Lake Marion shoreline
South Carolina Department of Archives and History, circa 1970
5. At center, Previous Santee Limestone / Limestone and Marl Formations Marker
1964 by the Division of State Parks, S.C. Commission of Forestry
Photographed By Wikipedia
6. Sir Charles Lyell (1797-1875), noted British geologist, as mentioned on marker
South Carolina Department of Archives and History,, circa 1970
7. Santee River / Lake Marion, view from marker
Credits. This page was last revised on June 16, 2016. It was originally submitted on August 28, 2009, by Mike Stroud of Bluffton, South Carolina. This page has been viewed 2,087 times since then and 46 times this year. Photos:1, 2, 3, 4. submitted on August 28, 2009, by Mike Stroud of Bluffton, South Carolina. 5. submitted on August 29, 2009, by Mike Stroud of Bluffton, South Carolina. 6. submitted on August 28, 2009, by Mike Stroud of Bluffton, South Carolina. 7. submitted on August 29, 2009, by Mike Stroud of Bluffton, South Carolina. • Craig Swain was the editor who published this page.