Kärdla Crater

Kärdla sits inside a meteorite impact crater, though you would never guess it from walking the streets. The crater is about 4 kilometres in diameter and was formed roughly 455 million years ago. The original bowl has been largely filled by sediment and vegetation over the geological ages, leaving only a slight depression and the circular arrangement of the crater rim visible in the landscape.

The crater is not a tourist attraction in the conventional sense — there is no visitor centre, no signage on the street, and most of the crater floor is now occupied by the town itself. What you can do is walk to the rim, which rises gently on the north side of town, and look back across Kärdla to appreciate the topography. The Hiiumaa Museum has a display on the crater's geology and discovery. For anyone interested in impact structures, this is a genuinely significant site — one of the better-preserved Ordovician impact craters in Europe.

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A story
The Kärdla crater was formed around 455 million years ago when a meteorite about one kilometre in diameter struck what was then a shallow tropical sea. The impact liquefied the rock, which then re-solidified in the characteristic circular pattern still visible in aerial photographs. The town of Kärdla was built inside the crater rim without anyone noticing — the geological structure was only identified in the 1970s.