The depressions left behind are called kettles. The raised areas are called moraines.
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.
The name given to lakes formed through glacial erosion is "glacial lakes." These lakes are created when glaciers carve out depressions in the land, which then fill with melted ice and water. They often have unique characteristics, such as a circular shape and steep sides.
As the ice blocks left behind by the continental glacier melted after the last ice age, they formed bodies of water known as kettle lakes. These kettle lakes are depressions in the landscape caused by the melting of the ice blocks, which were then filled with water from the melted ice.
When the glacier melted from North America it left a mass of "heterogeneous" rock debris (loosely termed "glacial drift") etc
The depressions left behind are called kettles. The raised areas are called moraines.
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 is a depression left by melted blocks of ice in glacial deposits.
glacial lakes. These lakes were formed by the meltwater from the ice blocks, and often occupied depressions in the landscape created by glacial activity. They were temporary features that eventually drained as the ice melted away completely.
The name given to lakes formed through glacial erosion is "glacial lakes." These lakes are created when glaciers carve out depressions in the land, which then fill with melted ice and water. They often have unique characteristics, such as a circular shape and steep sides.
As the ice blocks left behind by the continental glacier melted after the last ice age, they formed bodies of water known as kettle lakes. These kettle lakes are depressions in the landscape caused by the melting of the ice blocks, which were then filled with water from the melted ice.
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.
Glacial lakes are primarily caused by deposition. As glaciers move, they erode the land beneath them and create depressions where meltwater collects, forming glacial lakes. The deposition of sediment carried by the glacier contributes to the formation and shape of the lake.
Marshes formed when glaciers created depressions on the Earth's surface are called kettle ponds. These ponds are commonly found in areas where the glacial ice melted and left behind depressions that filled with water. Kettle ponds support unique ecosystems and are important habitats for diverse plant and animal species.
When the glacier melted from North America it left a mass of "heterogeneous" rock debris (loosely termed "glacial drift") etc
All over the world. They can be found anywhere from on a mountain, like at Mount Washington's Lake of the Clouds Hut, to underground, like at Howe's Caverns.
A moraine is a landscape feature created by glacial deposits. Moraines are formations of unsorted rock debris that were transported and deposited by a glacier as it moved and melted. They can be found in various forms such as terminal moraines at the end of glaciers or lateral moraines along their sides.