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Silfra Fissure
Silfra Fissure

Silfra Fissure

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The Silfra fissure is a water-filled crack between the North American and Eurasian tectonic plates, where the two continents drift apart from each other. Water travels from the Langjökull glacier through porous lava rock during a journey that takes between 30 and 100 years before seeping into the fissure.

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