
Rock arches are considered unique geological and natural phenomena that always captivate explorers and lead them to insights and interpretations regarding the temporal and spatial dimensions of any habitat.
Scientific research attributes the causes of these formations in the “Hisma” desert to the combined action of wind and basic geology. The wind naturally pushes sand particles up the slope to the fossilized formation, leading to the deposition of sand on the more downward and wind-facing side. Over time, this process creates rock arches, affecting their size and shape. Other factors such as wind speed, sand supply, and the region’s basic geology also play a role.
Rock arches usually form in areas with plenty of sand and a stable, flat rock base. Erosion carries sand to the mountains, and the shapes depend on the balance between these forces and local wind conditions, which often enhance their beauty.
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