Marble is a metamorphic rock, formed when limestone rich in calcite or dolomite recrystallises under great heat and pressure deep within the earth's crust. The transformation tightens the stone's crystal structure and gives its surface a depth that seems to hold the light.
Veins are the traces of minerals drawn into the stone as it crystallised, and it is this mineral make-up that sets the colour: iron oxides bring reds and burgundies, graphite and organic matter greys and blacks, pure calcite white. Every movement of a vein is a composition the stone arrived at under its own conditions.
Anatolia is one of the richest marble regions in the world. That range, from the deep burgundy of Elazığ Cherry to the pale stones of the Aegean, is the foundation of MUZEA's material palette.


