What kind of feature is Kettle Moraine State Forest?

The Kettle Moraine State Forest is a state forest in southeastern Wisconsin. 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.

Why is it called the Kettle Moraine?

The retreating glacier left behind geological indentations, known as kettles, and deposited debris—silt, rocks, and boulders—that produced topographical accumulations called moraines.

What are kettles Kames and eskers?

Kames are often associated with kettles, and this is referred to as kame and kettle or knob and kettle topography. Kame terraces are frequently found along the side of a glacial valley and are stratified deposits of meltwater streams flowing between the ice and the adjacent valley side.

What are the two lobes that formed a prominent boundary near Whitewater?

The most prominent of these is the Kettle Moraine in southeast Wisconsin formed by the contact between the Lake Michigan Lobe and the Green Bay Lobe.

What kind of Moraine is Kettle Moraine?

Kettle Moraine. The Kettle Moraine is a belt of irregular ridges and upland areas that extends for more than 120 miles, mostly in Sheboygan, Washington, and Waukesha Counties.

How long is Kettle Moraine?

Take a leisurely drive along the 115-mile Kettle Moraine Scenic Route, bike the 6.5-mile crushed limestone Lake-to-Lake Bike Trail connecting Mauthe and Long Lake Recreation Areas, hike to the top of an observation tower (there are three located in this region), or canoe along crystal clear lakes.

What does moraine look like?

Characteristics. Moraines may be composed of debris ranging in size from silt-sized glacial flour to large boulders. The debris is typically sub-angular to rounded in shape. Moraines may be on the glacier’s surface or deposited as piles or sheets of debris where the glacier has melted.

What kind of moraine is Kettle moraine?

What is the difference between horns and kettles?

A horn results when glaciers erode three or more arêtes, usually forming a sharp-edged peak. Cirques are concave, circular basins carved by the base of a glacier as it erodes the landscape. The Matterhorn in Switzerland is a horn carved away by glacial erosion.

How can you tell the difference between an end moraine and an Esker?

End Moraine: A type of moraine formed at the outer edge of a glacier or glacial lobe where it paused or stopped. Esker: A sinuous rounded ridge of sand and gravel deposited by the streams that flowed through tunnels at the base of the glacier.

How is a till formed?

Till or glacial till is unsorted glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines.

What is a glaciation?

Glaciers are made up of fallen snow that, over many years, compresses into large, thickened ice masses. Glaciers form when snow remains in one location long enough to transform into ice. Due to sheer mass, glaciers flow like very slow rivers.

How big is the Kettle Moraine State Forest?

Covering more than 22,000 acres of forested glacial hills, kettle lakes and prairies, the Southern Unit of the Kettle Moraine State Forest is interlaced with more than 100 miles of mountain biking, horseback riding and hiking and nature trails. Paddling, boating, swimming, fishing, hunting and winter sport opportunities are all available.

Where is the Kettle Moraine in Wisconsin located?

Kettle Moraine. Kettle Moraine is a large moraine in the state of Wisconsin, United States.

How long is the drive to Kettle Moraine?

The Kettle Moraine drive This 115-mile drive follows the Kettle Moraine, a long ridge of forested hills that mark where two great arms of the last glacier butted up against each other. The route follows the Kettle Moraine Scenic Drive developed and maintained by the Kettle Moraine State Forest staff.

How did the Kettle Range get its name?

Kettle Moraine. It has also been referred to as the Kettle Range and, in geological texts, as the Kettle Interlobate Moraine . The moraine was created when the Green Bay Lobe of the Laurentide Ice Sheet, on the west, collided with the Lake Michigan Lobe of that glacier, on the east, depositing sediment.