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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 ...
Þingvellir is now a national park in the municipality of Bláskógabyggð in southwestern Iceland, about 40 km (25 miles) northeast of Iceland's capital, Reykjavík. 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 ...
Snæfellsjökull (Icelandic pronunciation: [ˈs (t)naiːˌfɛlsˌjœːkʏtl̥] ⓘ, snow- fell glacier) is a 700,000-year-old glacier -capped stratovolcano in western Iceland. [3] It is situated on the westernmost part of the Snæfellsnes peninsula. Sometimes it may be seen from the city of Reykjavík over Faxa Bay, at a distance of 120 km (75 mi).
Katla (Icelandic pronunciation: [ˈkʰahtla] ⓘ) is an active volcano in southern Iceland. This volcano has been very active historically with at least twenty documented major eruptions since 2920 BC. In its recent history though, Katla has been less active as the last major eruption occurred in 1918. These eruptions have had a Volcanic ...
The pyroclastic cones. Stóra-Eldborg undir Geitahlíð is a pyroclastic cone, [1] built up mostly from spatter and scoria it forms part of a crater row. Another such eruption fissure is to be found nearby, therefore Icelanders prefer the plural Eldborgir undir Geitahlíð. [5] One of the eruption fissures dissects the older tuya Geitahlíð.
Volcano House is a geology exhibition in Reykjavík, Iceland, located at Tryggvagata 11. [1] The exhibition gives a brief overview of Iceland's geological history and volcanic systems. [2] Every hour the Volcano House shows two documentaries, one about the volcanic eruption of Eyjafjallajökull in 2010 and one about the volcanic eruption in the ...
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