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View full screen - View 1 of Lot 69. "ALIEN" GOGOTTE FORMATION, OLIGOCENE (30 MILLION YEARS AGO), FONTAINEBLEAU, FRANCE.

From a Distinguished French Private Collection

"ALIEN" GOGOTTE FORMATION, OLIGOCENE (30 MILLION YEARS AGO), FONTAINEBLEAU, FRANCE

Auction Closed

December 17, 08:56 PM GMT

Estimate

4,000 - 6,000 USD

Lot Details

Description

From a Distinguished French Private Collection

"ALIEN" GOGOTTE FORMATION

FONTAINEBLEAU, FRANCE


Oligocene (30 million years ago), the body of a naturally and densely formed ass🐼emblage the natural sandstone concretion with various 🅘cascading layers forming protrusions with softly rounded edges, the sandstone of a pale greyish-white colour. 


This gogotte is a particularly fine example of these spectac🐼ular natural sculptures. Its shape can be associated with supernatural or perhaps extraterrestrial forms and open to a variety of interpretations. 


A Gogotte is a millions-of-years old, naturally shaped sandstone concretion, consisting of tiny quartz fragments held together by calcium carbonate. The finest specimens are found in Fontainebleau, France, renowned for its extremely fine-grained, porcelain-like sands, and each of these natural mineralogical works of art take on unique forms, often evoking clouds, whirlwinds, animals, or ghosts. Gogottes were a great inspiration to the Surrealists, as well as Louise Bourgeois and Henry Moore, and have captured the imaginations of some of the most powerful aristocrats in Europe. Louis XIV, “The Sun King” was so seduced by them, that he had numerous specimens excavated to decorate the gardens at the Palace of Versailles, and a great number of the ornately rounded, scrolling formations can be found surrounding the mysterious grove of the Three Fountains (designed by Le Nôtre in 1677). Destroyed during the time of Louis XVI, the Grove was reconstructed in 2004, with the Gogottes appearing in all of their natural glory, thanks to the patronage of the Société des Amis de Versailles and The American Friends of Versailles. A particularly well-preserved example of a sandstone concretion is on di🀅splay at the Smithsonian Institution National Museum of Natural History in Washing🎐ton D.C.

Please note, the Oligocene was 30 million years ago, and not 300 years ago as stated in the printed catalogue