The Kettle Moraine is an area of varied topography–parallel, steep-sided ridges, conical hills and flat outwash plains, mostly composed of sand and gravel.
It extends for more than 120 miles, mostly in Sheboygan, Fond du Lac and Washington Counties.
The Kettle Moraine is composed of glacial sediment deposited between the Green Bay and Lake Michigan Lobes approximately 18,000 to 15,000 years ago as they receded from their maximum positions during the most recent glaciation.  We’ll cover what makes the Kettle Moraine so unique!