| top down abstract patterns salt flats | ||||||||||||||||||||||||||||||||||||||||
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| Cracked terrain forms a pattern of irregular polygons in varying sizes, characteristic of salt flats. The surface is a pale brownish-white, with darker lines marking the cracks. Textured and dry, these crusty salt formations are due to evaporated mineral-rich water. The top-down perspective highlights the mosaic-like structure typical in arid regions, reminiscent of desiccated clay. The intricate network of fissures suggests geological processes influenced by climate and evaporation. | ||||||||||||||||||||||||||||||||||||||||
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