Leon Sinks Geological Area
5.7 miles south of Capitol Circle on US 319
Welcome to the fascinating world of karst. The term is applied to terrain
that rain and groundwater have changed by dissolving underlying limestone bedrock.
The porous limestone bedrock was formed long ago from ancient coral reefs and
shell deposits. Rain and groundwater have dissolved the limestone to form
sinkholes, swales and underground caverns. The Woodville Karst Plain runs from
Tallahassee southward to the Gulf of Mexico.
I began hiking the Sinkhole Trail at 12:15pm, reached Big Dismal at 12:47pm,
Lost Stream Sink at 1:20pm, Fisher Creek Rise and the Crossover Trail at 1:27pm,
Gopher Hole at 1:45pm and was back at the parking lot at 2:00pm.
Along the way I stopped to take 231 photographs, some of my favorites are in this gallery.
Entrance on US 319
My truck in the parking lot
Restrooms - Pileated Woodpecker's favorite
Notice the holes made by the pileated
Map of the area
Sights to be seen in the Apalachicola National Forest