A Natural Sculpture
The Gogotte
The finest concretion recovered from the most important discovery at the famed site of Fontainebleau. ‘The Gogotte’ challenges the boundary between nature and art. It stands as perhaps the most anthropomorphic natural formation known, epitomising the pinnacle of pareidolia – that innate human tendency to see meaningful shapes in abstract forms. It is inescapably a figure; a god, an idol or a warrior.
A Natural Formation
Almost otherworldly in its appearance, the present piece is an entirely natural formation. It is believed to have been formed between 300,000 and 30,000 years ago by the almost instantaneous cementation of silica-rich groundwater percolating through the pure quartz sand of the Fontainebleau desert1. But its sparkling white surface is due to a much earlier geological process, occurring over 30 million years before present. During this period, the continually flooding and retreating seas filtered the sand dunes of the Paris Basin, leaving behind some of the purest sand in the world. Coveted for its important properties, often reaching 99.7% silica, the desert has been mined throughout history, beginning in 1752, with the establishment of glass factories under the reign of Louis XVI2.
During one such extraction in the late 1980s, miners unearthed a considerable cache of these specimens. Fascinated by the recent discoveries in Fontainebleau and likening them to works by Michelangelo, Seattle-based mineral collector and dealer, Richard Berger sought to acquire as many as he could, for his exhibition, the ‘Masterworks of the Earth’. From a 520-million-year-old crystal cluster from Namibia, to a giant ammonite fossil from the Chihuahuan Desert, the collection certainly lived up to its name. But it was the gogottes of Fontainebleau that were its crowning glory. In particular, the present specimen was singled out for use on the promotional material for the exhibition.
1. M. Thiry, et al, ‘Sables et Gres de Fontainebleau: que reste-t-il des facies sed imentaires initiaux?’(2013): 37-90; P. Thomas, ‘Les Calcites de Bellecroix, fruits des variations climatiques pléistocènes,’ (2020).
2. M. Welland, ‘Two museums and the Fontainebleau glass sand,’ (2010).