Rarely, eroded unconsolidated sediments can be preserved in the till along with their original sedimentary structures.

Landslides occurred in unconsolidated sediment and fissures up to 30 cm wide were observed.

Ball-and-pillow deformations are a result of a physical shock that has been applied to unconsolidated sediment.

The point at which a stream emerges from an underground course through unconsolidated sediments or through caves.

It contains a large wedge of unconsolidated sediments that have been deposited since the Cretaceous Period.

Floodplains generally contain unconsolidated sediments, often extending below the bed of the stream.

Around the world, soft bottom consist of unconsolidated sediment and unvegetated areas.

The unconsolidated sediments of the coastal plain range in age from Cretaceous to recent.

Deglaciation left a substantial amount of unconsolidated sediment.

Currently, these unconsolidated sediments are strongly eroded and reworked by the sea.