A Gogotte formation, Oligocène period

A Gogotte Formation
Oligocene (approx. 30 million years ago)
Fontainebleau, France

Gogottes are beautiful and beguiling mineral formations. Once thought to have been composed from chalk, they are actually the rare and entirely natural result of calcium carbonate binding with extremely fine quartz grains. Each sculptural layer is a unique composition from the mineral-rich waters of Fontainebleau, south east of Paris, France, with the shapes evoking clouds and tangible representations of dreamlike imagery. The mineralization process takes place over the course of approximately 30 million years, with every formation a uniquely shaped wonder. As a prime example of the blend between nature and art, gogottes can be appreciated as sandstone variants of the Gongshi (scholar’s rocks) tradition.

These sandstone concretions boast an international popularity and an acclaimed reputation spanning centuries. As early as the late seventeenth century for example, gogottes were lauded for their aesthetic by the highest echelons of French nobility. Louis XIV “the Sun King” of France (r. 1643-1715) was so enamored by these formations that he ordered extensive excavations around Fontainebleau, in order to decorate his palace gardens. Gogottes still adorn L’Encelade, Les Trois Fontaines, and La Salle de Bal at Versailles, and continue to enchant and delight visitors as they have for over 300 years.

It is perhaps unsurprising that gogottes served as inspiration for artists well into the 20th century. As dynamic snapshots of elemental metamorphosis, they were particularly well received by impressionist and surrealist sculptors. In particular, the recumbent figures by Henry Moore, and white marble compositions by Jean Arp (S’accroupissant, 1960-1962) and Louise Bourgeois (Cumul I, 1969) all evoke the arresting and unpredictable formations of gogottes.

Height with stand : 51cm
Dimensions : 48x23x22cm