
Rock of ten hours
Gustave Courbet·1855
Historical Context
Dated 1855 and held by Musées Nationaux Récupération, this painting of a distinctive rock formation in the Franche-Comté landscape belongs to the geological landscape subjects Courbet pursued alongside his more celebrated figure works. The Jura plateau features dramatic limestone formations — cliffs, overhangs, and isolated rock masses — that Courbet returned to repeatedly with the same focused attention a geologist might bring. The 'rock of ten hours' name likely refers to a local toponym, and Courbet's use of specific local place-names reinforces his commitment to the particularity of real landscape over generalized picturesque composition.
Technical Analysis
The isolated rock mass required careful attention to the geological character of Jura limestone — its horizontal bedding, its weathered and fissured surface, the way moss and vegetation colonize its crevices. Palette knife work builds the rock's surface with actual physical relief on the canvas. Sky behind the rock is relatively simple, providing the tonal contrast that articulates the formation's silhouette.
Look Closer
- ◆The rock's geological layering — horizontal strata of Jura limestone — is rendered with palette knife strokes that follow the actual bedding planes
- ◆Surface fissures and weathered channels are painted with darker, recessed marks that describe the rock's history of erosion
- ◆Vegetation in the rock's crevices — moss, small shrubs, grasses — is painted at fine scale to convey the rock's inhabitable surfaces
- ◆The sky's tonal contrast against the rock's silhouette is managed with care, the sky lightening toward the horizon to maximize the rock's presence


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