Gogottes
Athena, Quaternary Period; formed within Oligocene Fontainebleau sand
Naturally formed silica-cemented sandstone concretion
mounted on a metal base
Fontainebleau, France
mounted on a metal base
Fontainebleau, France
55 x 32 x 22 cm
23.45 kg
23.45 kg
A naturally formed sandstone concretion from Fontainebleau, France, composed of exceptionally fine quartz sand cemented by silica. Mounted on a metal base; 55 × 32 × 22 cm (21 5/8...
A naturally formed sandstone concretion from Fontainebleau, France, composed of exceptionally fine quartz sand cemented by silica. Mounted on a metal base; 55 × 32 × 22 cm (21 5/8 × 12 5/8 × 8 5/8 in.); 23.45 kg.
Athena is a particularly sculptural 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, while the process through which they became cemented into their present formations occurred considerably later, during successive Quaternary glacial periods.
The formation rises in an irregular vertical arrangement of rounded projections, folded layers and deeply recessed passages. A broad, disc-like form dominates its centre, surrounded by looping ridges and suspended, teardrop-shaped elements. The finely granular white surface unifies these contrasting forms, while the repeated curves create a sense of movement around the central mass. The title Athena encourages associations with a helmeted or shield-bearing figure without imposing a single interpretation upon the natural formation.
Gogottes developed as silica-rich groundwater circulated through the Fontainebleau sands. Dissolved silica gradually precipitated between the exceptionally fine quartz grains, binding them together in a discontinuous process governed by changing patterns of water movement. This intermittent cementation produced the layered contours, cavities and bulbous forms that distinguish each specimen. Although its surface resembles modelled clay or carved stone, Athena remains entirely unworked.
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 a compelling figural presence, Athena occupies an ambiguous position between natural-history specimen and abstract sculpture.
Athena is a particularly sculptural 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, while the process through which they became cemented into their present formations occurred considerably later, during successive Quaternary glacial periods.
The formation rises in an irregular vertical arrangement of rounded projections, folded layers and deeply recessed passages. A broad, disc-like form dominates its centre, surrounded by looping ridges and suspended, teardrop-shaped elements. The finely granular white surface unifies these contrasting forms, while the repeated curves create a sense of movement around the central mass. The title Athena encourages associations with a helmeted or shield-bearing figure without imposing a single interpretation upon the natural formation.
Gogottes developed as silica-rich groundwater circulated through the Fontainebleau sands. Dissolved silica gradually precipitated between the exceptionally fine quartz grains, binding them together in a discontinuous process governed by changing patterns of water movement. This intermittent cementation produced the layered contours, cavities and bulbous forms that distinguish each specimen. Although its surface resembles modelled clay or carved stone, Athena remains entirely unworked.
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 a compelling figural presence, Athena occupies an ambiguous position between natural-history specimen and abstract sculpture.