Spring water tends to be constant in more than one way: temperature, flow, and chemistry. These are kept constant because most of the water making up the spring comes from fast-flowing underground rivers. The pockets that create the openings for this moving water results from underground limestone that dissolves in acidic water.This reaction is what makes underground caves. If an area that rests on top of these pockets becomes dried out and the water removed, sinkholes can form if the weight of the land caves in. At Anderson Park we got to see up close a sink hole that is connected to the ocean. It assumed that the water in this sinkhole is fresh until it meets its salt water counterpart somewhere underground in the river systems. The water is expected to be clear because there is nothing to disturb or nutrients to make the water cloudy.
It is very important that we do not treat these sinkholes as land fills because they are still part of the underground passage ways of our drinking water.
the sinkhole sitting in front of Lake Tarpon which it has been disconnected from in order to keep the lake fresh
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