Woods Bay State Park | |
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Nearest city | Olanta, South Carolina |
Coordinates | 33°56′38″N79°59′28″W / 33.944°N 79.991°W Coordinates: 33°56′38″N79°59′28″W / 33.944°N 79.991°W |
Area | 1,590 acres (6 km2) |
Elevation | 36.91 m |
Created | 1973 |
Woods Bay State Park is a state park located near the town of Olanta in Florence County, South Carolina. The park contains some of the last remaining large Carolina Bays. [1] Recent work by the U.S. Geological Survey has interpreted the Carolina Bays as relict thermokarst lakes that formed several thousands of years ago when the climate was colder, drier, and windier. [2] Thermokarst lakes develop by thawing of frozen ground (permafrost) and by subsequent modification by wind and water. Thus, this interpretation suggests that permafrost once extended as far south as the Carolina Bays during the last ice age and (or) previous ice ages.
Activities available at the park include picnicking, fishing, hiking, bird watching and geocaching. Canoeing is also popular on the one-mile canoe trail in the Carolina Bay. While private boats are not allowed, rental canoes and kayaks are available.
Amenities include a picnic shelter, a boardwalk through a cypress-tupelo swamp and a nature center. [3]
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Lake Waccamaw State Park is a North Carolina state park in Columbus County, North Carolina, in the United States. Located near the town of Lake Waccamaw, North Carolina, it covers 2,398-acre (9.70 km2), along the shores of Lake Waccamaw, a Carolina bay. Recent work by the U.S. Geological Survey has interpreted the Carolina Bays as relict thermokarst lakes that formed several thousands of years ago when the climate was colder, drier, and windier. Thermokarst lakes develop by thawing of frozen ground (permafrost) and by subsequent modification by wind and water. Thus, this interpretation suggests that permafrost once extended as far south as the Carolina Bays during the last ice age and (or) previous ice ages.
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Singletary Lake, surrounded by Singletary Lake State Park in Bladen County, North Carolina in the United States, is one of a series of Carolina bay lakes that stretch from New Jersey to Florida along the Atlantic Coastal Plain. Recent work by the U.S. Geological Survey has interpreted the Carolina Bays as relict thermokarst lakes that formed several thousands of years ago when the climate was colder, drier, and windier. Thermokarst lakes develop by thawing of frozen ground (permafrost) and by subsequent modification by wind and water. Thus, this interpretation suggests that permafrost once extended as far south as the Carolina Bays during the last ice age and (or) previous ice ages. Singletary Lake is not fed by any stream, but relies entirely upon rain. The land beneath and surrounding the lake is mica-rich sandy clay and sand that is from the Upper Cretaceous era with a thin layer of Pleistocene deposits covering it. This land is lower than the surrounding land and drains very poorly, creating Singletary Lake.
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Little Pee Dee State Park is a state park located near the town of Dillon in Dillon County, South Carolina. The park land includes a part of a Carolina Bay and adjacent sand rim. Recent work by the U.S. Geological Survey has interpreted the Carolina Bays as relict thermokarst lakes that formed several thousands of years ago when the climate was colder, drier, and windier. Thermokarst lakes develop by thawing of frozen ground (permafrost) and by subsequent modification by wind and water. Thus, this interpretation suggests that permafrost once extended as far south as the Carolina Bays during the last ice age and (or) previous ice ages.
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