Which of the following is NOT typical of glacial deposits?

Glacial deposits are formed from the erosion and sediment transport by glaciers, and they exhibit characteristic features based on the processes involved.

A stratified serpentine-shaped deposit refers to drumlins or similar formations that glaciers shape as they move. These deposits often display stratification, reflecting the layered nature of sediments deposited by meltwater.

An unstratified, unsorted mixture of sediment is typical of glacial till, which glaciers transport and deposit as they advance and retreat. This characteristic signifies that glaciers do not sort the sediments they carry, leading to a jumbled mix of various particle sizes.

Elongated ellipsoidal hillsides, such as those created by drumlins, are also a common result of glacial activity. These landforms typically represent the accumulation of till that has been streamlined by the moving ice.

The feature described as a pile of rocks at the base of a steep slope, often referred to as a talus slope or debris slope, typically results from processes such as gravity and erosion, which are not directly related to glacial actions. While glaciers do contribute to the creation of loose rock through weathering and erosion, the arrangement of rocks at the base of a slope in a pile does not reflect the unique characteristics associated with primary glacial