13.- Lines of Resistance

Geological strata, fractured ridges, and exposed rock formations organize the coastline through directional tension and structural resistance. Stone surfaces confront the continual movement of water and weather while erosion, shifting light, and changing tides repeatedly alter the apparent stability of the terrain. Each formation records compression, fracture, and gradual transformation across geological time. The sequence approaches the coast as a physical structure continually shaped by the repetitive force of the sea.