Hamada, one of the wind-formed landforms, removes smaller materials that the winds can carry in arid and semi-arid regions, causing large materials to remain.
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In geography, a pedestal rock refers to a distinctive geological feature formed through the process of erosion. It typically consists of a large, isolated rock or boulder that sits atop a narrower base or pedestal-like structure. The formation of pedestal rocks is commonly associated with differential erosion, where softer underlying rock layers erode more rapidly than the harder, resistant upper layers.
The formation of pedestal rocks typically begins with the exposure of a large boulder or rock outcrop due to weathering and erosion processes such as wind, water, and ice. Over time, the surrounding softer rock material is eroded away, leaving the harder rock elevated above the surrounding landscape on a pedestal-like base.https://mylondonpainter.co.uk/
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Roche Moutonnee or sheepback is formed by glacial eroding. Different etching levels between layers cause the formation of geographical structures in the form of camel humps.
The interior of the rocks is dissolved by the waters and reaches a loose structure. This rather soft and loose structure is eroded by the winds. As a result, cavities are formed within the rocks. This earth shape that is formed is called Tafone.
In short, Barkhan is a dune pile in the shape of a moon. It can be given as an example of wind deposition. It is formed by the effect of external forces and occurs by the effect of wind. Barkhan is known as the most common dune form. It is generally convex.