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  2. Lögberg - Wikipedia

    en.wikipedia.org/wiki/Lögberg

    Lögberg. 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.

  3. Geology of Iceland - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Iceland

    The geology of Iceland is unique and of particular interest to geologists. Iceland lies on the divergent boundary between the Eurasian Plate and the North American Plate. It also lies above a hotspot, the Iceland plume. The plume is believed to have caused the formation of Iceland itself, the island first appearing over the ocean surface about ...

  4. Silfra - Wikipedia

    en.wikipedia.org/wiki/Silfra

    Silfra. 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 Iceland.

  5. Húsafell Stone - Wikipedia

    en.wikipedia.org/wiki/Húsafell_Stone

    The Húsafell Stone. The Húsafell Stone is a legendary lifting stone weighing 186 kg (410 lb) [1] located in a west country farming estate in Húsafell, Iceland about 132 km (82 mi) northeast of Reykjavík. [1] The slightly triangular, slab shaped stone is kept at a sheep and goat pen built from natural stones by Reverend Snorri Björnsson ...

  6. Reynisdrangar - Wikipedia

    en.wikipedia.org/wiki/Reynisdrangar

    Reynisdrangar captured from Reynisfjall Landscape with the sea stacks in the background. Basalt columns on the beach at Reynisfjara. Reynisdrangar (Icelandic pronunciation: [ˈreiːnɪsˌtrauŋkar̥]) are basalt sea stacks situated under the mountain Reynisfjall [ˈreiːnɪsˌfjatl̥] near the village Vík í Mýrdal in southern Iceland.

  7. Iceland hotspot - Wikipedia

    en.wikipedia.org/wiki/Iceland_hotspot

    The Iceland plume is a postulated upwelling of anomalously hot rock in the Earth's mantle beneath Iceland. Its origin is thought to lie deep in the mantle, perhaps at the boundary between the core and the mantle at about 2,880 km (1,790 mi) depth. Opinions differ as to whether seismic studies have imaged such a structure. [8]

  8. Hvítserkur - Wikipedia

    en.wikipedia.org/wiki/Hvítserkur

    Vatnsnes, Iceland. Hvítserkur (Icelandic pronunciation: [ˈkʰvitˌsɛr̥kʏr̥], regionally also [-ˌsɛrkʰʏr̥]) is a 15 m high basalt stack along the eastern shore of the Vatnsnes peninsula, in northwest Iceland. [1] The rock has two holes at the base, which give it the appearance of a dragon that is drinking. The base of the stack has ...

  9. Þorbjörn (mountain) - Wikipedia

    en.wikipedia.org/wiki/Þorbjörn_(mountain)

    The name of Þorbjörn or Þorbjarnarfell [ˈθɔrˌpja(r)tnarˌfɛtl̥], the “mountain of Þorbjörn” is a popular man's name in Iceland connected with the son of a farmer in the region. When a group of bandits were tyrannizing the farmers in the area and disappeared into hiding after their raids, the young man pretended to be part of the ...