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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.
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The Loew Lake Unit of the Kettle Moraine State Forest is a 1,090-acre (4 km 2) member of the Wisconsin state park system.The unit offers hiking, hunting, and horse riding along the east branch of the Oconomowoc River and the shore of 23-acre (0 km 2) Loew Lake, and also features a number of large conifer plantations.
Lapham Peak is a Wisconsin state park located in the Kettle Moraine State Forest. It is just south of Delafield and seven miles (11 km) west of Waukesha. The park entrance is two miles (3 km) north of the Glacial Drumlin State Trail.
Chippewa Moraine State Recreation Area: Chippewa: 3,272 1,324 1971 Numerous kettle lakes: Interprets varied glacial landforms. The park is a unit of the Ice Age National Scientific Reserve. [15] Copper Culture State Park: Oconto: 42 17 1959 Oconto River: Interprets a burial ground used by the Old Copper Culture from 3000 to 2000 BCE. [16]