What is a kettle lake in geology?

Kettle, also called Kettle Hole, 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. When filled with water they are called kettle lakes.

Read remaining answer here. Subsequently, one may also ask, what is a kettle lake and how is it formed?

Kettles form when a block of stagnant ice (a serac) detaches from the glacier. Eventually, it becomes wholly or partially buried in sediment and slowly melts, leaving behind a pit. In many cases, water begins fills the depression and forms a pond or lake—a kettle.

Furthermore, is a kettle lake erosion or deposition? Glaciers cause erosion by plucking and abrasion. Valley glaciers form several unique features through erosion, including cirques, arêtes, and horns. Glaciers deposit their sediment when they melt. Landforms deposited by glaciers include drumlins, kettle lakes, and eskers.

what are kettle lakes used for?

kettle lakes. Kettles are depressions left behind after partially-buried ice blocks melt. Many are filled with water, and are then called "kettle lakes". Most lakes in Michigan could be described as kettle lakes, and the term "kettle lake" describes the way the lake basin was formed.

How are glacial kettle lakes formed?

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 friction. The lakes that fill these holes are seldom more than 10 m (33 ft) deep and eventually become filled with sediment.