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Continental drift, Þingvellir (Thingvellir) National Park, Iceland

One of the many cracks or faults that traverse the rift valley that marks the crest of the Mid-Atlantic Ridge. The continental drift between the North American (left) and Eurasian Plates (right) is the boundary where the tectonic plates run through Iceland and are slowly drifting apart (about 2cm a year).

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Thingvellir-continental-rift-Iceland-1739.jpg
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Rozanne Hakala
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2616x1744 / 8.0MB
Bláskógabyggd Bláskógabyggð boundaries canyon continental drift crack crust earth Eurasian Plate fault fissure geologic geology Golden Circle HDR Iceland Ísland landmark landscape Mid-Atlantic Ridge mountains National Park North American Plate Parliament Plains rift rift valley rifting rock Rozanne Hakala scenic southwest Iceland tectonic Thing Fields Thingvellir tourism tourist UNESCO vatn volcanic water World Heritage Site Þingvellir Þingvellir National Park
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Iceland
One of the many cracks or faults that traverse the rift valley that marks the crest of the Mid-Atlantic Ridge. The continental drift between the North American (left) and Eurasian Plates (right)  is the boundary where the tectonic plates run through Iceland and are slowly drifting apart (about 2cm a year).
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