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Silfra fissure The Mid-Atlantic Ridge passing through Þingvellir Rocks and boulders that have piled up in the fissure due to earthquakes.. Silfra (Icelandic pronunciation: [ˈsɪl(v)ra]) is a rift formed in the Mid-Atlantic Ridge – the divergent tectonic boundary between the North American and Eurasian plates – and is located in the Þingvallavatn Lake in the Þingvellir National Park in ...
The volcanic origin of the islands in the lake is clearly visible. The cracks and faults around it, of which the Almannagjá [ˈalˌmanːaˌcauː] ravine is the largest, is where the Eurasian and North American tectonic plates meet. Silfra fissure is a popular scuba and snorkeling site.
The continental drift between the North American and Eurasian Plates can be clearly seen in the cracks or faults and rifts which traverse the region. The largest, Almannagjá, is a significant canyon. See Þingvellir index Þingvellir National Park rift valley. See Þingvellir index Þingvellir, Snorkeling in the Silfra canyon.
It is the only place in the world where you can dive or snorkel directly in a crack between two tectonic plates. [22] The tunnel from the entrance of Silfra to the cave is commonly known as ‘The Tunnel’, due to the strong current that ‘flushes’ divers attempting to swim through.
Located between the Eurasian and the North American tectonic plates, Iceland is a perennial seismic hot spot, but direct volcanic threats to inhabited areas are still rare.
Þingvellir is a site of historical, cultural, and geological significance, and is one of the most popular tourist destinations in Iceland. The park lies in a rift valley that marks the crest of the Mid-Atlantic Ridge and the boundary between the North American and Eurasian tectonic plates.
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