
Falaise de mer près du Tréport
Maximilien Luce·c. 1900
Historical Context
Falaise de mer près du Tréport (Sea Cliffs near Le Tréport), dated around 1900 and executed on paper, depicts the chalk sea cliffs of the Normandy coast near Le Tréport — a coastal town in the Seine-Maritime department where the chalk cliffs of the Pays de Caux reach the English Channel. Le Tréport was a popular destination for Parisian day-trippers and vacationers from the mid-nineteenth century, accessible by the railroad from Paris, and its dramatic white cliffs had been depicted by Courbet, Monet, and other painters of the sea. Luce's version, made on paper rather than canvas, indicates a relatively informal or rapid study — perhaps made on site as a preparatory work or sketched during a brief visit. The chalk cliff subjects of the Norman coast posed particular challenges for chromatic observation: the cliffs are chalk-white but register warm ochres, cool blues, and subtle greens depending on the angle of light and weather conditions, and the sea at their base ranges from deep green-blue to grey depending on sky conditions.
Technical Analysis
The paper support and intimate scale suggest direct outdoor observation. The chalk cliffs are rendered through a nuanced range of warm and cool grey-white strokes, while the sea below is handled in the characteristic horizontal strokes Luce uses for water surfaces. The blue-green of the Channel sea and the cream-white of the cliff face create the composition's central color contrast.
Look Closer
- ◆The chalk cliff face is never pure white — look for the warm ochres and cool greys that register depending on the angle of light
- ◆The Channel sea below the cliffs is treated with horizontal strokes of blue-green that convey the specific color of cold northern seawater
- ◆The paper support gives this work a slightly different surface texture than Luce's canvases — the tooth of the paper visible in thinner paint passages
- ◆Notice how the cliff edge creates a dramatic diagonal cutting across the composition, contrasting the vertical cliff face with the horizontal sea

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