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Vífilsfell
Vífilsfell () is a hyaloclastite ridge in southwestern Iceland (Weichselian). It is 655 m high and located west of Jósepsdalur valley on the volcanic plateau of Hellisheiði. It forms the northernmost offset of the Bláfjöll mountain massif and is situated on top of the fissure volcanism, fissure system of Brennisteinsfjöll. Name The name comes from one of the freed slaves of Iceland's first settler Ingólfur Arnarson. The man, called ''Vífill'', is said to have had his own farm at Vífilsstaðir, now in the vicinity of the city of Hafnarfjörður. From there – according to the Landnámabók – he went daily up to the top of Vífilsfell, some 20 km away, to look after the weather.Ari Trausti Guðmundsson, Pétur Þorleifsson: Íslensk Fjöll. Gönguleiðir á 151 tind. Reykjavík 2004, p.300Snæbjörn Guðmundsson, Vegvísir um Jardfræði Íslands. Reykjavík 2015, p.50 When the weather seemed promising, he went fishing from the tip of the Seltjarnarnes peninsula ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bláfjöll
Bláfjöll (, "blue mountains") are a small mountain range in the southwest of Iceland on Reykjanes peninsula at about 30 km from Reykjavík. They form sort of a double mountain massif to the west and in the east of JósepsdalurÞór Vigfússon: Í Árnesþingi vestanverðu. Ferðafélag Íslands Árbók 2003. Reykjavík 2003, p.83 on Hellisheiði.Íslandshandbókin. Náttúra, saga og sérkenni. Reykjavík 1989, p. 780 Geography The mountain massif has a length of about 9 km. The western part includes Vífilsfell as well as , the eastern one reaches from to . The highest mountain is ''Hákollur'' (685 m). Geology The Bláfjöll are Pleistocene subglacial volcanoes and part of the Brennisteinsfjöll volcanic system. Winter sports The area is the most popular ski resort for the inhabitants of Iceland's Höfuðborgarsvæði, Capital City Area. The winter sports area is situated at elevations between 460 and 700 m.https://www.skiresort.info/ski-resort/blafjoell/ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jósepsdalur
Jósepsdalur (), also Josefsdalur , is a small valley, about 2 km long in southwestern direction, and to the east of the volcano Vífilsfell up on Hellisheiði at a distance of about 25 km from Reykjavík within Selvogshreppur municipality.Ari Trausti Guðmundsson, Pétur Þorleifsson: Íslensk Fjöll. Gönguleiðir á 151 tind. Reykjavík 2004, p. 300 The Bláfjöll mountains surround the U-shaped valley.Þór Vigfússon: Í Árnesþingi vestanverðu. Ferðafélag Íslands Árbók 2003. Reykjavík 2003, p. 83 The valley is situated next to an old trail over the pass ''Ölfusskarð'' from Ölfus, the region in the south of Iceland around Hveragerði, to Reykjavík.Íslandshandbókin. Náttúra, saga og sérkenni. Reykjavík 1989, v.2, p.806 Folk tales Acc. to an old folk tale, a troll woman shall have lived in a cave in Jósepsdalur. Another folk tale explains the name of the valley: A man named Jósep lived in this valley once. He had a bad reputation for swearing and blasphemy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brennisteinsfjöll
Brennisteinsfjöll (, "Sulfur mountains" Brennisteinsfjöll. Detailed description. In: Catalogue of Icelandic Volcanoes. Retrieved 27 July 2020) is a minor Volcanism of Iceland, volcanic system, with Crater Row, crater rows and small shield volcanoes on the Reykjanes Peninsula in southwest Iceland. Geography The mountain range is located at about from Reykjavík as well as Hafnarfjörður and to the south of the cities on the Reykjanes peninsula of Southwest Iceland. Brennisteinfjöll is not high. The highest mountain is Vífilsfell with 655 m.Geology Position within Iceland’s volcano-tectonic environment In Iceland there are about 32 volcanic systems. Volcanic system means a volcano-tectonic fissure system and – very often a bigger volcano, a so-called central vo ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reykjanes Peninsula
Southern Peninsula (, ) is an administrative unit and part of Reykjanesskagi (pronounced ), or Reykjanes Peninsula, a region in southwest Iceland. It was named after Reykjanes, the southwestern tip of Reykjanesskagi. The region has a population of 30,933 (2024) and is one of the more densely populated parts of the island. The administrative centre is Keflavík, which had 7,000 residents when it merged with the nearby town of Njarðvík and Hafnir in 1995 to create Reykjanesbær, which is the largest settlement outside the Greater Reykjavík area; in 2018, the region had a population of 17,805. The region is the location of Keflavík International Airport, the major point of entry for Iceland. Some fishing towns, such as Grindavík, Njarðvík and Sandgerði, are situated on the peninsula. The peninsula is marked by active volcanism under its surface and large lava fields, allowing little vegetation. There are numerous hot springs in the southern half of the peninsula, around t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hafnarfjörður
Hafnarfjörður, officially Hafnarfjarðarkaupstaður, is a port town and municipality in Iceland, located about south of Reykjavík. The municipality consists of two non-contiguous areas in the Capital Region (Iceland), Capital Region, on the southwest coast of the country. At about 31,500 inhabitants, Hafnarfjörður is the third-most populous city in Iceland after Reykjavík and Kópavogur. It has established local industry and a variety of urban activities, with annual festival events. Activities The town is the site of an annual Viking festival, where Viking culture enthusiasts from around the world display reconstructions of Viking garb, handicraft, sword-fighting and longbow shooting. It takes place in June. Local industry Just two kilometres () outside of Hafnarfjörður is an aluminium smelter, run by Alcan. The smelter was originally built in 1969. Local elections were held in April 2007, where the people of the town voted against extension of the smelter. History ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landnámabók
(, "Book of Settlements"), often shortened to , is a medieval Icelandic written work which describes in considerable detail the settlement () of Iceland by the Norse in the 9th and 10th centuries CE. is divided into five parts and over 100 chapters. The first part tells of how the island was found. The latter parts count settlers quarter by quarter, beginning with west and ending with south. It traces important events and family history into the 12th century. More than 3,000 people and 1,400 settlements are described. It tells where each settler settled and provides a brief genealogy of his or her descendants. Sometimes short anecdote-like stories are also included. lists 435 people (', which includes men and women) as the initial settlers, the majority of them settling in the northern and southwestern parts of the island. It remains an invaluable source on both the history and genealogy of the Icelandic people. Some have suggested a single author, while others have ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seltjarnarnes
Seltjarnarnes () is a town and municipality in the Capital Region of Iceland. The municipality is located on a peninsula, bordered only by Reykjavík to the east. It is also the most densely populated municipality in Iceland. It took on its current political form shortly after the Second World War and was formally created as a township in 1947. It is the smallest Icelandic township by land. The municipality's small land size relative to its population makes it Iceland's most densely populated municipality. Overview There are two schools in Seltjarnarnes, Mýrarhúsaskóli and Valhúsaskóli. The Independence Party has had an overall control in the town's council since proper elections started in 1962. First Lady of Iceland Guðrún Katrín Þorbergsdóttir held a position in the city council for 16 years. In the last elections in 2014, the party received 52,6% of the votes and 4 out of 7 members of the council. Other parties represented in the town council are Samfylkingin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svínahraun
Leitin () is a small shield volcano in the southwest of Iceland. Name Leitin ("the hills") is sometimes also called Leiti ("hills") or Leitahraun after its eruption products (“the lava of Leiti”). Geography The lava shield is located on the big Reykjanes peninsula some 25 km south of Reykjavík. When travelling on the hringvegur and looking to the west, the volcano is to be seen in a broad valley between the palagonite ridges of ''Lambafell'' with its quarries and ''Sauðadalahnúkar'' and behind some small cones, the ''Nyrðri'' and ''Syðri Eldborg'' , eruptive vents of the Brennisteinsfjöll volcanic system. Geology and volcanism The Holocene shield volcano Leitin is itself also part of the Brennisteinsfjöll volcanic system and therefore of the Reykjanes Volcanic Belt.Thor Thordarson, Armann Hoskuldsson: Iceland. Classic geology of Europe 3. Harpenden 2002, p.56 It originated in a probably long drawn, mostly effusive eruption, ca. 5000 years ago. This sm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
ʻaʻā
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is often also called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. Etymology The word ''lava'' comes from Italian and is probably derived from the Latin wor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subglacial Eruption
Subglacial eruptions, those of ice-covered volcanoes, result in the interaction of magma with ice and snow, leading to meltwater formation, jökulhlaups, and lahars. Flooding associated with meltwater is a significant hazard in some volcanic areas, including Iceland, Alaska, and parts of the Andes. Jökulhlaups (glacial outburst floods) have been identified as the most frequently occurring volcanic hazard in Iceland, with major events where peak discharges of meltwater can reach 10,000 – 100,000 m3/s occurring when there are large eruptions beneath glaciers. It is important to explore volcano-ice interactions to improve the effectiveness of monitoring these events and to undertake hazard assessments. This is particularly relevant given that subglacial eruptions have demonstrated their ability to cause widespread impact, with the ash cloud associated with Iceland's Eyjafjallajökull eruption in 2010 resulting in significant impacts to aviation across Europe. Examples Dec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
