Why go
The Big Bend's wetlands, the Atlantic's barrier islands and the Keys' reefs offer different ways to understand Florida's edge. This overview helps distinguish those landscapes before selecting a coastal region. It also explains why the interior's modest hills and the low southern peninsula feel so different despite belonging to the same state.
The full story
Barrier islands and sand spits shape much of Florida's Atlantic and northwestern shoreline. Lagoons and shallow water sit behind or beside these coastal strips. Farther south, salt marshes and mangroves border the peninsula, while coral reefs distinguish the Keys. The Big Bend coast has extensive marshes and tidal flats, giving it a character unlike an open beach resort. The Keys stretch outward from the southern tip, with Key Largo forming a major island at their northeastern end. Surrounding shallows and reefs have long influenced navigation. Warm currents also connect Florida's waters to wider marine systems: the Florida Straits lead toward the Gulf Stream, while the Loop Current circulates within the Gulf. On land, the state remains low. Northern and central uplands introduce gentle hills, and Britton Hill marks its highest point. This modest relief makes water and coastline more useful guides to the landscape than dramatic changes in elevation.