Florida Geology: Uniquely Beautiful
Florida’s highest point is the lowest of any state, but the peninsula’s remarkable geological history is anything but flat. Check out this profile of state parks that protect rockin’ geological features.
Have you ever wondered why Florida has so many lakes, springs and sinkholes? Much of Florida is “karst” terrain, a landscape resting on a water-soluble rock layer full of holes, caves and underground rivers. Rocks, sediments, landforms and water across the state tell a fascinating story.
Springs are karst features formed when limestone dissolves.
As their cool water flows to the earth’s surface, springs offer a window into the Floridan aquifer, which provides more than 90% of our drinking water. Perhaps the most famous spring is at Edward Ball Wakulla Springs State Park, but there are many spring parks, each with their own unique geology.
Sinkholes are another type of karst feature created when underground rock dissolves and collapses.
Some of Florida’s most stunning sinkholes are protected by state parks. Falling Waters State Park features Florida’s tallest waterfall at over 70 feet. At Devil's Millhopper Geological State Park, a lush subtropical forest has grown within a 120-foot-deep sinkhole. Paynes Prairie Preserve State Park, a vast wetland prairie, has karst terrain on its northern edge and a sinkhole that acts like a "drain" when water levels are high.
Pollutants from the surface can seep into the aquifer and impact water quality in sinkholes, springs and drinking water supplies.
One of Florida’s lesser-known geological features seem out of place in the flat state. Visiting a steephead ravine gives the impression that you’re in a mountainous area.
These ravines form when spring water seeps from the ground, carving a deep channel. At Ravine Gardens State Park, a paved loop road and unpaved trail network provide awesome views of clear spring streams and two ravines over 100 feet deep.