Geological and Ecological Foundations

The Landscape and Formation


Faver-Dykes State Park is situated within the St. Johns River watershed, a vast basin that supports a wide array of ecosystems. The park’s terrain is characterized by flatwoods and wetlands formed on coastal plain sediments deposited over millions of years.

The region’s sandy soils, combined with periodic fires and seasonal rainfall, foster a mosaic of habitats:

  • Pine flatwoods dominated by longleaf and slash pines


  • Bay swamps and cypress domes


  • Freshwater lakes and streams


  • Wet prairies



These habitats support diverse flora and fauna, including rare orchids, black bears, white-tailed deer, and numerous bird species.

The St. Johns River Influence


Though the park lies west of St. Augustine, it is part of the larger St. Johns River system, which is Florida’s longest river. The watershed’s hydrology has influenced the development of wetlands and forests in the area, shaping the availability of resources that have supported human life for millennia. shutdown123

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