Between History and Innovation with Terrazzo
© Peter Frese
Stones hold time. Some are formed by the sudden solidification of magma, like basalt, whose dense structure and dark color result from rapid cooling at the surface. Others, such as granite, are born slowly in deep magmatic chambers, where gradual cooling allows the growth of visible crystals, creating unique patterns and colors. There are also sedimentary rocks, formed by the compaction of mineral and organic debris over millions of years, with tones that reflect their chemical composition and the environment in which they were deposited. Transforming this geological diversity into a single continuous surface, terrazzo is a cementitious or mineral composite in which fragments of marble, granite, quartz, basalt, and other lithologies are embedded in a binding matrix, then polished to reveal the structure and luster of each particle. Unlike a homogeneous surface, terrazzo acts as a mineralogical showcase, where each aggregate retains its identity while contributing to a coherent whole, which can become a floor, wall cladding, or even furnitures.
