Disconformities show erosional features such as valleys, hills and cliffs that are later covered by younger sediments.

Plunge pools are erosional features which occur in the youthful stage of a river.

They are a geologically unique erosional feature in the U.S. state of Washington.

This large difference in elevation has led to the formation of numerous canyons, cliffs, and other erosional features on the edges of the mesa.

On the headland itself is evidence of erosional features, wave cut notch and a wave-cut platform.

It is important to distinguish such erosional features from true tectonic scarps since only the latter indicate recent or current fault activity.

These erosional features are seen on scales of less than a metre to several hundred metres.

The presence of streamlined erosional features on its floor shows that fluid was involved with its formation.

A panhole is a depressed, erosional feature found on flat or gently sloping rock.

These are erosional features called potholes.