Gogottes
The Cloud, Quaternary Period; formed within Oligocene Fontainebleau sand
Naturally formed silica-cemented sandstone concretion
mounted on a metal base
mounted on a metal base
55.5 x 61 x 22 cm
21 7/8 × 24 × 8 5/8 in.
50kg
21 7/8 × 24 × 8 5/8 in.
50kg
Further images
A naturally formed sandstone concretion from Fontainebleau, France, composed of exceptionally fine quartz sand cemented by silica. Mounted on a metal base; 55.5 × 61 × 22 cm (21 7/8...
A naturally formed sandstone concretion from Fontainebleau, France, composed of exceptionally fine quartz sand cemented by silica. Mounted on a metal base; 55.5 × 61 × 22 cm (21 7/8 × 24 × 8 5/8 in.); 50 kg.
The Cloud is a substantial example of the sandstone concretions known as Gogottes, found within the exceptionally pure sands of the Fontainebleau region in northern France. These sands were deposited during the Oligocene Period, approximately 30 million years ago, although the process through which they became cemented into sculptural formations occurred considerably later, during successive Quaternary glacial periods.
The formation extends horizontally through a series of rounded layers, swelling projections and deeply recessed passages. Its overlapping lobes appear to gather and disperse across the surface, creating a sense of continuous movement within the compact sandstone mass. The pale, finely granular surface softens the transitions between these forms, while the title The Cloud reflects their resemblance to suspended banks of vapour.
Gogottes developed as silica-rich groundwater circulated through the Fontainebleau sands. Dissolved silica precipitated between the exceptionally fine quartz grains, binding them together through a gradual and discontinuous process. Variations in water movement and mineral deposition produced their characteristic ridges, cavities and fluid contours. Despite its resemblance to modelled clay or carved stone, The Cloud is entirely unworked and was shaped exclusively through natural geological processes.
Fontainebleau sandstone formations have been admired as natural curiosities since at least the seventeenth century and were incorporated into several of the gardens at Versailles under Louis XIV. Their flowing, biomorphic forms have subsequently invited comparison with the sculpture of Jean Arp, Henry Moore and Barbara Hepworth. Combining geological rarity with an evocative abstract presence, The Cloud occupies an ambiguous position between natural-history specimen and sculptural object.
A detailed condition report is available upon request.
The Cloud is a substantial example of the sandstone concretions known as Gogottes, found within the exceptionally pure sands of the Fontainebleau region in northern France. These sands were deposited during the Oligocene Period, approximately 30 million years ago, although the process through which they became cemented into sculptural formations occurred considerably later, during successive Quaternary glacial periods.
The formation extends horizontally through a series of rounded layers, swelling projections and deeply recessed passages. Its overlapping lobes appear to gather and disperse across the surface, creating a sense of continuous movement within the compact sandstone mass. The pale, finely granular surface softens the transitions between these forms, while the title The Cloud reflects their resemblance to suspended banks of vapour.
Gogottes developed as silica-rich groundwater circulated through the Fontainebleau sands. Dissolved silica precipitated between the exceptionally fine quartz grains, binding them together through a gradual and discontinuous process. Variations in water movement and mineral deposition produced their characteristic ridges, cavities and fluid contours. Despite its resemblance to modelled clay or carved stone, The Cloud is entirely unworked and was shaped exclusively through natural geological processes.
Fontainebleau sandstone formations have been admired as natural curiosities since at least the seventeenth century and were incorporated into several of the gardens at Versailles under Louis XIV. Their flowing, biomorphic forms have subsequently invited comparison with the sculpture of Jean Arp, Henry Moore and Barbara Hepworth. Combining geological rarity with an evocative abstract presence, The Cloud occupies an ambiguous position between natural-history specimen and sculptural object.
A detailed condition report is available upon request.
Provenance
Fontainebleau,
France
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