In the context of this dissertation, the place of Volakas in Tinos is approached as a field of differentiation. A landscape of contrast, in terms of the scale and extent of its granitic formations - its geological phenomenon. The geological interior with strong signs of disintegration and changes in space and time is seen with bumps and holes. A place where the architectural footprint is indistinguishable as the landscape prevails. The intensity of the soil eruptions here is predominant and is chosen as such a place. As a destabilizing dynamic capable of introducing and producing spatial synergies. Experiments with "real" and "construction".