Aeolian processes encompass the mechanical and chemical actions of wind that shape the Earth's surface and transport sediments. These processes are fundamental drivers of geomorphology, leading to various forms of erosion and deposition. Wind movement generates high-velocity flows that pick up and move particles, ranging from fine dust and silt to larger pebbles. The primary mechanisms include saltation, where particles bounce along the ground, suspension, which carries fine material far from the source, and surface creep, where heavier debris is rolled or pushed. The resulting deposits and erosional features, such as ventifacts and loess sheets, provide critical insight into past atmospheric conditions and climatic change.