When glaciers recede, large features such as moraines, eskers, and kettle lakes typically form in their place.
When glaciers recede, they leave behind a variety of large landforms that shape the post-glacial landscape. Moraines, which are deposits of till (unsorted glacial sediment), often form along the edges of the glacier or as ridges within its path. Eskers are winding ridges of gravel and sand that were deposited by meltwater streams flowing within or beneath the ice.
Kettle lakes result from blocks of ice left behind by retreating glaciers, becoming partially or entirely buried by sediments and eventually melting to create depressions filled with water. These features collectively contribute to the unique topography and geological legacy of areas once covered by glaciers. The process of glacial recession and the subsequent formation of these landforms play a crucial role in shaping the Earth's surface over geological time scales.
Complete ques:
What large features typically form in the place of receding glaciers?