The park was drained by several tidal creeks that flowed east into the intracoastal waterway. Ocean water entered the intracoastal waterway from the Boynton Inlet, located 2.2 km to the north.
The park was drained by several tidal creeks that flowed east into the intracoastal waterway. Ocean water entered the intracoastal waterwayfrom the Boynton Inlet, located 2.2 km to the north.