Working Stone (2009-2016)
Nearly half a billion years ago, Vermont lay under a warm, shallow sea. Prehistoric marine organisms, whose fossils are still visible on rocky outcrops, built reefs that over eons turned to limestone. Continents collided, mountains taller than the Himalayas rose, and under great pressure the marine limestone sediments on the western side of the state metamorphosed into marble. On the eastern side, igneous granite deposits formed from the slow crystallization of molten rock below the surface of the earth. Stone made from ancient undersea creatures and rocks of pressurized lava — these are the hallmarks of the geological and historical landscape.