15.- Edge of Dissolution

At Cabo de Lata, within Costa Quebrada, the coast is encountered less as exposed geological structure than as a boundary becoming unstable beneath water, mist, and changing light. Waves, sea spray, distance, and long exposure reduce the clarity of cliffs and fractured surfaces, softening the separation between sea and land. The sequence moves from recognizable rock formations toward increasing atmospheric diffusion, until coastline, horizon, and open water begin to merge into a shifting field shaped by erosion, movement, and fading visibility.