Lanzarote anchors the project within a volcanic matrix where rock becomes a protocol of implantation. Black concrete extends this mineral stratification, absorbs solar light, and organizes a surface of thermal intensity that shifts according to time, angle, and season.
The project emerges through the fragmentation of the original volume into distinct units placed directly onto the basaltic sand. Each unit develops its own orientation determined by prevailing trade winds, solar trajectory, and local topography. The intervals between the masses structure air corridors, shaded zones, and transitional thresholds.
The interior space unfolds through disjointed sequences. Circulations pass through active voids and establish a fragmented perception of the site. The concrete material generates an artificial geological continuity with the surrounding volcanic formations. Edges capture grazing light and carve fields of shadow in constant transformation.
The cabin establishes a direct relation to the ground, the wind, and the ocean. Each fragment operates in resonance with a precise physical condition of the territory. The ensemble produces an open structure where perception oscillates between mineral density, atmospheric flows, and the marine horizon.