Sunday column
Understanding Karst and Sinkholes in Wisconsin
Karst refers to a unique landscape shaped by the dissolution of soluble bedrock, such as limestone, gypsum, or dolomite, by slightly acidic water over time. This process leads to the formation of distinctive features like sinkholes, caves, disappearing streams, and springs. In Wisconsin, the karst landscape is primarily composed of dolostone, a type of limestone rich in the mineral dolomite. This bedrock is more resistant to dissolution compared to pure limestone, resulting in a less dramatic karst topography.
Henry Cooper
Desk editor
Editor’s note
The full column continues in quiet type below.
Section
Sunday Broadsheet
What Is Karst?
How Do Sinkholes Form?
Where Are Karst Features Found in Wisconsin?
Why Is Karst Important for Water Quality?
What Can You Do?
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