In February 2012, a rare phenomenon occurred in The Netherlands. The fascinating appearance of ‘kruiend ijs’ – drifting ice, a sight that is usually confined to (sub) Arctic environments much further north.
Huge sheets of chunky ice blocks washed up on the shore and piled several meters high around the IJsselmeer and Afsluitdijk. This is the famous dike created to dam the former inland sea Zuiderzee, in order for a whole new province to be pumped up from below the enclosed waters.
Piles of kruiend ijs at the shores around Urk.
One of the places where this unusual phenomenon was most visible was at the fishing village of Urk. It was once an island in the Zuiderzee, now enclosed by the new land since the province of Flevoland was created during the 1940’s and 1950’s.
What causes drifting ice
The shifting and drifting ice is caused by strong winds occurring after a prolonged period of frosty temperatures. Ice sheets that have formed on the surface of large bodies of water are gradually pushed onto the shore by a combination of prevailing currents and wind.
As the ice sheets are blown across the water, they collide and crash into each other, creating iceberg-like piles of jumbled cubes when they reach the shore.
Arctic scenes in The Netherlands
They attracted huge amounts of visitors from all over the country, marvelling at the bizarre otherworldy Arctic scenes, and frolicking on the ice blocks.
Iceberg lagoon at the IJsselmeer.
Black and white ice, and frozen rain on the lake.
Drifting ice along the shores of IJsselmeer.
(c) Nancy Claus – Wilderness Coffee & Natural High
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