What process resulted in the rock formation similar to Pedestal Rock?

The process that resulted in the formation of rock structures similar to Pedestal Rock is indeed aeolian. Aeolian processes are related to the actions of the wind. Over time, wind can contribute to the erosion of rock formations by lifting and transporting sediment and fine particles. In areas with little vegetation and significant wind activity, this erosion can lead to unique rock formations characterized by their distinct shapes, such as pedestal rocks.

Pedestal rocks often have broader, more resistant caps that remain intact while the softer materials beneath are eroded away. The wind's ability to sculpt the landscape over long periods is key in the formation of these types of rocks. In contrast, fluvial processes involve water erosion, glacial processes involve ice movement, and mechanical weathering refers to the physical breakdown of rocks without chemical change, none of which creates the specific configurations seen in pedestal rock formations.