Florida
Britton Hill
       7½’ quadrangle: Paxton, FL/AL |
Unconsolidated |
![]() High point monument in Lakewood Park (1991). |
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Bedrock: None exposed. |
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Surficial Geology: Marine quartz sand |
Pleistocene and Holocene |
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Marine quartz sand, derived from reworking of the underlying Plio-Pleistocene Citronelle Formation during periods of higher sea level. The Citronelle is dominated by cross-bedded lenticular sands, but grain sizes range from clay to gravel. Soil Series: Fuquay loamy sand: well drained, nearly level soil formed under longleaf pine, slash pine, loblolly pine, turkey oak, laurel oak, and pineland three-awn wiregrass. Soil typically more than five feet thick. Selected References: Other suggested sources of information:
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