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kettle
Kettle holes are depressions left by melted blocks of ice in glacial deposits. These features are typically surrounded by mounds of sediment called kames. Kettle holes are common in areas that were once covered by glaciers during the last Ice Age.
A kettle lake is a shallow body of water formed by receding glaciers or draining flood waters. Chunks or blocks of ice break free and soil, rocks, and gravel filled in around the ice. When the block of ice melted, some of the debris falls into the hole, creating a sediment filled basin. When a kettle is filled with water, it is called a kettle lake.
a kettle
The depressions left by melted blocks of ice in glacial deposits are called kettle holes. They are circular or oval-shaped depressions that form when large chunks of ice left behind by a retreating glacier become buried in sediment. When the ice eventually melts, it creates a hole in the ground.
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.
A kettle is a depression left by melted blocks of ice in glacial deposits.
Eskers are formed by meltwater streams flowing within or beneath glaciers, depositing sediment in long, winding ridges. Kettle lakes are formed when blocks of ice left by retreating glaciers become buried by sediment and eventually melt, creating depressions that fill with water. Both features are common in areas that have experienced glacial activity.
kettle
kettle is a result of erosion though the material is an ancient deposition
A kettle pond is a shallow, sediment-filled body of water formed by retreating glaciers during the last ice age. They are typically small and round, and can be found in regions that were once covered by glaciers.