Fan-shaped Deposit (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team:)

This HiRISE image shows a Fan-shaped Deposit at the distal end of a Valley. The Fan is approximately 3,5x3,7 Km in size. While other similar Fans on Mars display stair-step terracing along their edges, this particular Fan does not show any Terraces. There is a Valley, instead, that appears to be the source of material that now composes much of the Fan.

Martian Fans are thought to be either Alluvial or Deltaic in origin.

On Earth, Alluvial Fans form when material upslope is eroded and transported by water down a confined Valley until reaching a flatter, broader surface downslope where the material is deposited to produce a Fan-shaped Surface Feature .
Deltaic Fans, on the other hand, form when rivers transport sediment downstream until an unconfined and flatter surface is reached under water, at which time the sediment is deposited in a Fan-shape.

Whether the Martian Fan formed by Alluvial or Deltaic processes in unknown, but both processes require a fluid (most likely water) that carved the Valley and transported the sediment downstream.