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What the Heck is Karst
Bill Walker
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Karst is very vulnerable
to groundwater pollution, due to ease of water flow. Natural
filtration is nearly nonexistent in karst. This section will
explore the unique problems associated with living in karst
areas in Central Florida.
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Karst is a term geologists use to describe a landscape found on
carbonate rocks (limestone in our case). Karst contains such features
as caves, sinkholes, large springs, and sinking streams. These landforms
are created by water dissolving the bedrock over many thousands of
years. Much like a piece of Swiss cheese coated with soil, Central
Florida contains these features and the unique environmental problems
associated with them.
As rain falls through the atmosphere, it picks up CO2 which dissolves
in the droplets. Once the rain hits the ground, it percolates through
the soil and picks up more CO2 to form a weak solution of carbonic
acid. The infiltrating water naturally exploits any cracks or crevices
in the rock. Over long periods, with a continuous supply of CO2
- enriched water, the limestone bedrock begins to dissolve. Openings
in the bedrock increase in size and an underground drainage system
begins to develop, allowing more water to pass, further accelerating
the formation of karst. Eventually this leads to the development
of subsurface caves.
Karst is all about drainage. Karst areas are typically devoid of
surface water because all of the water is channeled underground
by sinkholes and caves. You can compare karst features to plumbing.
Sinkholes are the drains and caves are the pipes.
The entire state of Florida is a karst region. The state is a limestone
plateau formed millions of years ago when the area was a shallow
sea. As tiny sea creatures died, their bodies piled up on the bottom
of the sea and formed the 1000 foot thick limestone bedrock that
underlies the entire state.
Although the entire peninsula has karst activity going on under
the ground, only certain areas of the state is it visible. Certain
areas of the state have less overburden (clay and soil) on top of
the bedrock. SEE
MAP
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