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The major part of the Kettle Moraine area is considered interlobate moraine, though other types of moraine features, and other glacial features are common. [1] The moraine is dotted with kettles caused by buried glacial ice that calved off the terminus of a receding glacier and got entirely or partly buried in glacial sediment and subsequently ...
The chief feature of the reserve is the Kettle Moraine, a highly glaciated area. The area contains very hilly terrain and glacial landforms, such as kettles , kames and eskers . The 56,000-acre (23,000 ha) [ 1 ] forest is divided into two large and three small units, which are spread across a hundred miles.
Kettle Moraine Scenic Drive generally follows county and local roads. It begins near Whitewater – at the southern expanse of the Kettle Moraine State Forest's southern unit ( 42°45′56″N 88°42′18″W / 42.76556°N 88.70500°W / 42.76556; -88.70500 ), the drive takes a northeast trek and passes through six counties: Walworth ...
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A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased ...
The Kettle Moraine Scenic Railway (reporting mark KMRY) was a heritage railway once located in North Lake, Wisconsin.It was founded in 1971 by Richard Hinebaugh, who bought a branch line from the Chicago, Milwaukee, St. Paul and Pacific Railroad (Milwaukee Road) to create a small museum.
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Kettle Moraine High School (KMHS) is a secondary school located in Wales, Wisconsin. It is a part of the Kettle Moraine School District. It is accredited by the North Central Association of Colleges and Schools (NCA CASI). [3] Kettle Moraine was named a National Blue Ribbon School of Excellence in 2002 by the U.S. Department of Education. [4]