Ad
related to: unusual facts about iceland
Search results
Results From The WOW.Com Content Network
One of the rare examples of sedimentary rocks in Iceland is the sequence of marine and non-marine sediments present on the Tjörnes Peninsula in northern Iceland. These Pliocene and late Pleistocene deposits are composed of silt and sandstones, with fossils preserved in the lower layers. [11]
Iceland's stock market, the Iceland Stock Exchange (ISE), was established in 1985. [147] Iceland is ranked 27th in the 2012 Index of Economic Freedom, lower than in prior years but still among the freest in the world. [148] As of 2016, it ranks 29th in the World Economic Forum's Global Competitive Index, one place lower than in 2015. [149]
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 ...
Dettifoss, located in northeast Iceland. It is the second-largest waterfall in Europe in terms of volume discharge, with an average water flow of 200 m 3 /s. Iceland is an island country in Northern Europe, straddling the Eurasian and North American plates between the Greenland Sea and the North Atlantic Ocean, northwest of the British Isles.
Iceland as seen from space, with Vatnajökull appearing as the largest white area to the lower right. Vatnajökull (Icelandic pronunciation: [ˈvahtnaˌjœːkʏtl̥] ⓘ, literally "Glacier of Lakes"; sometimes translated as Vatna Glacier in English) is the largest and most voluminous ice cap in Iceland, and the second largest in area in Europe after the Severny Island ice cap of Novaya Zemlya ...
Bárðarbunga was a little-known volcano in Iceland due to its remote location and infrequent eruptions approximately once every 50 years, but recent studies have shown that many tephra layers originally thought to be from other volcanoes were ejected from Bárðarbunga, [1] and that lateral dyke intrusions may trigger eruptions in adjacent ...
Mid-Atlantic Ridge and adjacent plates. Volcanoes indicated in red.. In geological terms, Iceland is a young island. It started to form in the Miocene era about 20 million years ago from a series of volcanic eruptions on the Mid-Atlantic Ridge, where it lies between the North American Plate and Eurasian Plate.
Laki (Icelandic pronunciation: ⓘ) or Lakagígar ([ˈlaːkaˌciːɣar̥], Craters of Laki) is a volcanic fissure in the western part of Vatnajökull National Park, Iceland, not far from the volcanic fissure of Eldgjá and the small village of Kirkjubæjarklaustur.