
Glacier of Rosenlaui
John Brett·1856
Historical Context
Glacier of Rosenlaui was painted in 1856 when John Brett was twenty-three and had just encountered the Pre-Raphaelite Brotherhood's insistence on direct, unmediated observation of nature. The Rosenlaui glacier in the Bernese Oberland of Switzerland had attracted painters and tourists since the early nineteenth century, but Brett's version is unusual in its extreme fidelity to the specific geological character of the ice — crevasses, moraine, and the blue-green translucency of glacial ice are rendered with scientific exactness rather than sublime vagueness. John Ruskin, who would become Brett's demanding mentor, praised the painting for its geological accuracy. The National Gallery holds the canvas as an example of Pre-Raphaelite landscape's insistence on truth to nature extended to geological as well as botanical subjects.
Technical Analysis
Brett uses a near-vertical compositional arrangement that places the glacier's face as the dominant element, minimising sky and foreground. The blue-green tones of the ice are built up in layers to suggest the characteristic translucency of glacial ice. Rock and moraine in the foreground are painted with individual attention to the character of different stone types.
Look Closer
- ◆Crevasses in the glacier are rendered with their characteristic blue shadow colour rather than generic dark tone
- ◆Individual rocks in the moraine foreground are differentiated by colour and texture, reflecting geological variety
- ◆The glacier's surface shows the compression ridges and flow patterns of actual glacial movement
- ◆A precisely observed waterfall threads through the composition, its movement captured through careful tonal layering
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