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Cody Scarp
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The Cody Scarp or escarpment is located in north and north central Florida USA. It is a persistent topographical feature, an ancient early Pleistocene shoreline formed from 1.8 million to 10,000 years BP during a period of higher sea level. The Cody Scarp has a slope of 5% to 12%.
The scarp is most prominent in Leon County, Florida where the scarp runs east to west. The scarp separates the Hawthorn Group of fine to medium grained sandy clays and silty, clayey sands of the Red Hills Region of north Florida and southwest Georgia to the north from the fine to medium fine grained, partially recrystallized, silty to sandy limestones of the Gulf Coastal Lowlands to the south.

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Encyclopedia
The Cody Scarp or escarpment is located in north and north central Florida USA. It is a persistent topographical feature, an ancient early Pleistocene shoreline formed from 1.8 million to 10,000 years BP during a period of higher sea level. The Cody Scarp has a slope of 5% to 12%.
The scarp is most prominent in Leon County, Florida where the scarp runs east to west. The scarp separates the Hawthorn Group of fine to medium grained sandy clays and silty, clayey sands of the Red Hills Region of north Florida and southwest Georgia to the north from the fine to medium fine grained, partially recrystallized, silty to sandy limestones of the Gulf Coastal Lowlands to the south. A dramatic difference in elevation is seen here as the Red Hills, at a maximum of 230 feet (70 meters) mean sea level (MSL), drops to the area known as the Woodville Karst Plain, an elevation of 50 to 80 feet (15 to 24 meters) within 15 miles (24 km).
On the Woodville Karst Plain, the Suwannee Limestone of the Floridan Aquifer is shallow and exposed in many places. This is the primary recharge area for Wakulla Springs and where the aquifer is most vulnerable to pollution on the land surface. It is also a zone of high sinkhole activity.
In Alachua County, Florida this westward-facing escarpment between an upland plateau to the east and a karst plain to the west has elevations up to 190 feet (57.9 meters) mean sea level (MSL).
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