Winter Landscape with Ice Skaters
Hendrick Avercamp·1608
Historical Context
Winter Landscape with Ice Skaters, painted in 1608 and now in the Art Museums of Bergen, Norway, is among the earlier dated works in Hendrick Avercamp's known output. The 1608 date places it during Avercamp's Amsterdam period, before his relocation to Kampen in 1613, and it documents the early development of a compositional type that would define his career. The frozen Dutch waterway with its crowds of skaters, sledge-pullers, and onlookers was already a well-established genre when Avercamp began painting — Pieter Bruegel the Elder's winter landscapes had established the precedent in the previous century — but Avercamp brought to it a new systematic thoroughness and social attentiveness. The Bergen museum's acquisition of this panel reflects the extensive dispersal of Avercamp's work to Scandinavian collections, where his cold-climate subjects presumably resonated. By 1608 Avercamp had already developed his characteristic panoramic format, low horizon, and practice of distributing varied figure types across the frozen surface. The panel's relatively small scale is typical of his working practice.
Technical Analysis
An early work by Avercamp shows the characteristic compositional elements already in place — low horizon, wide panoramic format, distributed figures — while the figure handling may be slightly less refined than in his mature works. The paint application on the small panel is precise, suited to the detailed documentation of individual figures at small scale.
Look Closer
- ◆As an early work, the figure types and compositional strategies show the nascent form of what would become a signature format
- ◆The panoramic width relative to height maximises the sense of the frozen surface as an open social arena
- ◆Individual skaters and their equipment — blades, poles, costumes — are depicted with the specificity that characterises Avercamp's figure work
- ◆The winter sky, occupying a significant portion of the panel, is rendered with the pale, cold luminosity appropriate to the season







