Costa Quebrada - Wave Impact (1:2)
Costa Quebrada - Worn Strata (2:3)
Costa Quebrada - Receding Layers (2:3)
Costa Quebrada - Inverted Cliffs (3:2)
At Costa Quebrada, fracture, tectonic displacement, and erosion dominate the visual structure of the coastline. Sedimentary layers tilt, cliffs divide, and isolated rock masses emerge through continual geological pressure and marine exposure. Waves, weather, and shifting light activate these formations, revealing instability within surfaces that still retain monumental force. The sequence approaches the coast as a terrain of fractured planes and intersecting forces where geological time remains visibly inscribed into the landscape.