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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 ...
Þingvellir (Icelandic: [ˈθiŋkˌvɛtlɪr̥] ⓘ, anglicised as Thingvellir [Note 1]) was the site of the Alþing, the annual parliament of Iceland from the year 930 until the last session held at Þingvellir in 1798. [2] Since 1881, the parliament has been located within Alþingishúsið in Reykjavík. [3]
See Þingvellir index Þingvellir, Snorkeling in the Silfra canyon. See Þingvellir index Þingvellir (Thingvellir), Scuba diver in the Silfra canyon. See Þingvellir index Þingvellir (Thingvellir), Silfra Fissure. Rocks and boulders that have piled up in the fissure due to earthquakes.
With a surface of 84 km 2 it is the largest natural lake in Iceland. Its greatest depth is 114 m. Its greatest depth is 114 m. At the northern shore of the lake, at Þingvellir (after which the lake is named), the Alþingi , the national parliament, was founded in the year 930, and held its sessions there until 1799 and still as of today the ...
Lögberg (Icelandic pronunciation: [ˈlœɣˌpɛrk]), or Law Rock, was a rocky outcrop in south west Iceland, at the location for the assembly of the country's Althing parliament. The original Althing was gathered at Þingvellir , [ 1 ] an area of dramatic landscapes which was easily accessible from the populated areas of the south west.
Straddling the Mid-Atlantic Ridge, the lava fields from Skjaldbreiður have been torn and twisted over the millennia, forming a multitude of fissures and rifts inside the Þingvellir National Park, the best known of which are Silfra, Almannagjá [ˈalˌmanːaˌcauː], Hrafnagjá [ˈr̥apnaˌcauː] and Flosagjá [ˈflɔːsaˌcauː].
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