The Cody Scarp or Cody Escarpment is located in north and north central Florida United States. It is a relict scarp and ancient persistent topographical feature formed from an ancient early Pleistocene shorelines of ~1.8 million to 10,000 years BP during interglacial periods. The Cody Scarp has a slope of 5% to 12%.(Main article: Leon County Pleistocene coastal terraces) In Jefferson County to the east, the scarp coincides with the Wicomico Terrace with an elevation at 40–45 feet above mean sea level.