
Kettle (landform) - Wikipedia
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.
Fluvioglacial Landforms: What Is A Kettle? - WorldAtlas
Jan 19, 2018 · A kettle, also called a kettle hole or a pothole, is a shallow depression that fills with glacial water in addition to water from other sources and has sediments. Kettles form when previously buried blocks of ice melt.
Kettle (landform) - Simple English Wikipedia, the free encyclopedia
Kettles are landforms created by melted water from glaciers, a process called "fluvioglacial." When warming weather conditions cause a glacier to start melting, large blocks of ice can break off in a process called "calving."
Kettle | Volcanic, Erosion & Deposition | Britannica
kettle, in geology, depression in a glacial outwash drift made by the melting of a detached mass of glacial ice that became wholly or partly buried. The occurrence of these stranded ice masses is thought to be the result of gradual accumulation of outwash atop the irregular glacier terminus.
What does kettle (landform) mean? - Definitions.net
A kettle (also known as a kettle lake, kettle pond, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters.
Kame - Wikipedia
A kame, or knob, is a glacial landform, an irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depression on a retreating glacier, and is then deposited on the land surface with further melting of the glacier.
Kettles - U.S. National Park Service
Feb 22, 2018 · Depressions, known as kettles, often pockmark these outwash plains and other areas with glacial deposits. Kettles form when a block of stagnant ice (a serac) detaches from the glacier. Eventually, it becomes wholly or partially buried in …
What Are Kettle Lakes? - Owlcation
Dec 8, 2023 · In layman's terms, a kettle lake is a water-filled pothole left in the ground by a receding glacier that formed millions of years ago. When a glacier recedes, the ice breaks off the front of it in a process called "calving."
Kettle Moraine - Encyclopedia of Milwaukee
The greater Kettle Moraine stretches from Kewanee County south through Walworth County. It was created when the Green Bay and Lake Michigan “lobes” of the Wisconsin Glacier (it had six lobes all together) retreated some 10,000 years ago.
What Are Kettle Lakes? - The Environmental Literacy Council
May 12, 2024 · Kettle lakes, seemingly simple depressions of water, are in fact remarkable geological features with significant ecological value. Their formation is a direct consequence of past glacial activity, and they are often found as scattered reminders of the power of ice.