What do we call the type of sediment found in erosional landforms?

The type of sediment found in erosional landforms can vary greatly, and the correct choice encompasses a range of sediment types that can indeed be found in these landforms.

Erosional landforms develop primarily through the processes of weathering and the subsequent removal and transport of soil and rock material by various agents like water, wind, or ice.

Pedisediment refers to sediment that has undergone pedogenic processes and is generally found in areas where soil formation has been influenced by erosion.

Residuum is weathered material that remains in place on the landscape after the bedrock has been eroded away. It may become part of the sedimentary deposits formed after erosion has acted on the original material.

Glacial till is another type of sediment associated with glacial erosion, consisting of unsorted debris deposited directly by glacial ice. This material is common in regions that have been scoured by glaciers, contributing to the erosional features present in those landscapes.

Thus, all of these sediment types can be associated with erosional landforms, making the broad answer encompassing all of them accurate. Each plays a significant role in the types of sediments found in areas characterized by erosion, reflecting the diverse processes and materials involved in shaping the landscape.