They are both large
They are both large
They are both large
i think it is because they look like kettles
A kettle lake is a shallow, sediment-filled body of water formed by retreating glaciers or draining flood-waters.
Eskers are winding ridges of sediment deposited by meltwater streams flowing under glaciers. Kettle lakes are formed when a block of ice from a retreating glacier gets buried in sediment and then melts. Both eskers and kettle lakes are common features of glacial landscapes.
The area of Kettle Lakes Provincial Park is 12.61 square kilometers.
Yes. There are many in the area around the Kettle Moraine area of Wisconsin.
erosion
sorted
A kettle lake is a shallow, sediment-filled body of water formed by retreating glaciers or draining flood-waters.
Knob hills are small, rounded landforms with steep sides, usually formed by volcanic activity. Kettle hills are mounds of sediment deposited by melting glacial ice, often forming depressions known as kettle lakes. Both types of hills are common features in landscapes shaped by geological processes.
As the glaciers retreated after the last ice age, landforms such as moraines, eskers, and kettle lakes were left behind. The melting ice also contributed to the formation of valleys, fjords, and depressions that filled with water to create lakes and rivers. Additionally, the receding glaciers exposed previously buried land, allowing for the colonization and migration of plant and animal species.