
La falaise de Penarth, le soir, temps orageux
Alfred Sisley·1897
Historical Context
La falaise de Penarth, le soir, temps orageux of 1897, at the Beaverbrook Art Gallery in Fredericton, Canada, was painted during Sisley's final significant creative journey — a summer visit to Wales where the Gower Peninsula's rocky coast presented him with a dramatically different landscape challenge from his customary Loing valley subjects. Penarth's chalk headlands above the Bristol Channel required a more dynamic painterly response than the horizontal, reflective landscapes he was accustomed to: the cliff face vertical rather than horizontal, the sea below turbulent rather than still, the stormy evening light charged rather than quietly luminous. Sisley's late Welsh paintings show a more expressively energetic handling than his French work — the impasto thicker, the color contrasts more pronounced, the compositional drama more explicitly acknowledged. The Beaverbrook Gallery, dedicated largely to British and Canadian art, holds this as evidence of Sisley's British heritage surfacing in the final years of his primarily French career. Two years after this visit he would be dead, and these Welsh canvases represent his last significant departure from the Loing valley that had defined his mature practice.
Technical Analysis
The stormy evening palette uses deep mauves, greys, and ochres in dramatic contrast. The cliff face is rendered with vigorous, forceful strokes that suggest both its physical solidity and the turbulent atmosphere surrounding it. The livid sky is painted in broad, urgent sweeps. The overall effect is more dramatically emotional than his typical Loing valley manner.
Look Closer
- ◆The chalk cliffs glow with an internal orange-pink light as evening sun catches the stone face.
- ◆Storm clouds are rendered in deep blue-purple above, contrasting with the warm cliff face below.
- ◆Rough sea texture is built up with short, directional strokes varying in pressure and direction.
- ◆A tiny silhouetted figure at the cliff's edge gives scale to the dramatic geological mass.





