geology

The problem of being and becoming could be modelled within a geological frame, exposing the layering of diverse groups of elements that are incorporated by deposition. Thus a new orography, consonant with continuity, is being shaped, but also the erosion and debasing of previous forms or their marginalization: their absence of participation in the novel layers, their insularity. In this model, there is not a direct contact between the plane of construction and the orography, the former is only supported by certain bumps, elevations, uneven accidents, producing deposition in the space between them and the conformation of plateaus: plains of consistence. Still the orography suffers changes by means of acclivities emerging as a product of an arrangement of elements producing a bump. What a plain of consistence assures is the swift transition from one area to the other, the appearance of order and meaning, the experience of roaming on a surface. It is the plane of construction that frames the noetic space making it conceptually coherent, the attitudes comprehensible, embodied.