fluvioglacial landform

Fluvioglacial landforms are landforms molded by glacial meltwater.

Kettle - fluvioglacial landform occurring as the result of blocks of ice calving from the front of a receding glacier and becoming partially to wholly buried by glacial outwash.

The Shonkin Sag is a prehistoric fluvioglacial landform located along the northern edge of the Highwood Mountains in the state of Montana in the United States.

In 1793, work began on the Ellesmere Canal, connecting the River Mersey with Chester and Shropshire through the fluvioglacial landform known as the Backford gap, and the town of Ellesmere Port began to develop.