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Geological Formation

Thingvellir Rift Valley

Structural and Tectonic Formations

The Thingvellir Rift Valley lies within Thingvellir National Park in southwestern Iceland and marks a section of the divergent boundary between the North American and Eurasian tectonic plates, where the plates are pulling apart at a rate of roughly 2 centimeters a year. This ongoing separation fractures the crust and causes the valley floor to subside gradually, producing a widening, down-dropped rift bounded by parallel fault scarps, most prominently the Almannagjá gorge along the valley's western edge. Thingvellir is also the site of the Althing, one of the world's oldest parliamentary assemblies, founded there in 930 CE, and the site was inscribed as a UNESCO World Heritage Site in 2004 for combining a rare place where mid-ocean ridge spreading is visible on land with major historical significance.

Facts
Classification
Protected Status
UNESCO World Heritage Site 1
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Rifting, Processes

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Sources
1. Wikipedia: Þingvellir National Park, Wikipedia
UNESCO World Heritage Site
Quote, UNESCO World Heritage Site
Þingvellir was designated a UNESCO World Heritage Site based on cultural criteria.
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Wikidata: Thingvellir Rift Valley
Wikidata Q107370, class allow-list match (w-wdresolver-0926)View the Source
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