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Reykjanes Fólkvangur
Reykjanes () is a small headland on the southwestern tip of the Reykjanes Peninsula in Iceland, giving the main peninsula its name. The region is about from Iceland's international airport. As the name means "smoking peninsula" connected to volcanic activity, there are also other peninsulas by this name in Iceland, e.g. the peninsula of Reykjanes in Ísafjarðardjúp Ísafjarðardjúp () is a large fjord in the Westfjords region of Iceland. Its name translates to ''Depth of the fjord of sea ice''. Ísafjörður, capital of the Westfjords region, is situated close to the mouth of Ísafjarðardjúp in Sk .... References External links Catalogue of Icelandic Volcanoes - Reykjanes Headlands of Iceland Black sand beaches {{Iceland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reykjanesvirkjun
The Reykjanes Power Station (known as ''Reykjanesvirkjun'' ) is a geothermal power station located in Reykjanes at the southwestern tip of Iceland. As of 2012, the power plant generates 100MWe from two 50MWe turbines, using steam and brine from a reservoir at 290 °C to 320 °C, which is extracted from 12 wells that are 2700m deep. This is the first time that geothermal steam of such high temperature has been used for electrical generation. The power plant is open to the public and houses the ''Power Plant Earth'' interpretative exhibition. See also * Geothermal power in Iceland * List of largest power stations in the world * List of power stations in Iceland * Renewable energy in Iceland References External links Photo Gallery from islandsmyndir.is Geothermal power stations in Iceland {{powerstation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reykjanes Peninsula
Southern Peninsula ( is, Suðurnes ) 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 27,829 (2020) 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 peninsul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iceland
Iceland ( is, Ísland; ) is a Nordic island country in the North Atlantic Ocean and in the Arctic Ocean. Iceland is the most sparsely populated country in Europe. Iceland's capital and largest city is Reykjavík, which (along with its surrounding areas) is home to over 65% of the population. Iceland is the biggest part of the Mid-Atlantic Ridge that rises above sea level, and its central volcanic plateau is erupting almost constantly. The interior consists of a plateau characterised by sand and lava fields, mountains, and glaciers, and many glacial rivers flow to the sea through the lowlands. Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Circle. Its high latitude and marine influence keep summers chilly, and most of its islands have a polar climate. According to the ancient manuscript , the settlement of Iceland began in 874 AD when the Norwegian chieftain Ingólfr Arnarson became the first p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keflavík International Airport
Keflavík Airport ( is, Keflavíkurflugvöllur ) , also known as Reykjavík–Keflavík Airport, is the largest airport in Iceland and the country's main hub for international transportation. The airport is west of Keflavík and southwest of Reykjavík. The airport has three runways, two of which are in use, and the airport area is about . Most international journeys to or from Iceland pass through this airport. The main carrier at Keflavík is Icelandair, which has the airport as its main hub. The airport is only used for international flights; all domestic flights use the much smaller Reykjavík Airport, which lies from Reykjavík's city centre. Keflavík Airport is operated by Isavia, a government enterprise. History Early years Originally, the airport was built by the United States military during World War II, as a replacement for a small British landing strip at Garður to the north. It consisted of two separate two-runway airfields, built simultaneously just 4 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ísafjarðardjúp
Ísafjarðardjúp () is a large fjord in the Westfjords region of Iceland. Its name translates to ''Depth of the fjord of sea ice''. Ísafjörður, capital of the Westfjords region, is situated close to the mouth of Ísafjarðardjúp in Skutulsfjörður. The north-eastern coast is fairly straight with the only inlet being Kaldalón, but the southern side has fjords extending well into the land: Skutulsfjörður, Álftafjörður, Seyðisfjörður, Hestfjörður, Skötufjörður, Mjóifjörður, Reykjafjörður and Ísafjörður. Three islands lie in Ísafjarðardjúp: Borgarey, Æðey and Vigur. Borgarey is the smallest with no inhabitants and Æðey the largest. On both Æðey and Vigur there is one farmstead. On the peninsula of Reykjanes, there are hot springs A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by sh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reykjanes
Reykjanes () is a small headland on the southwestern tip of the Reykjanes Peninsula in Iceland, giving the main peninsula its name. The region is about from Iceland's international airport. As the name means "smoking peninsula" connected to volcanic activity, there are also other peninsulas by this name in Iceland, e.g. the peninsula of Reykjanes in Ísafjarðardjúp Ísafjarðardjúp () is a large fjord in the Westfjords region of Iceland. Its name translates to ''Depth of the fjord of sea ice''. Ísafjörður, capital of the Westfjords region, is situated close to the mouth of Ísafjarðardjúp in Skutul .... References External links Catalogue of Icelandic Volcanoes - Reykjanes Headlands of Iceland Black sand beaches {{Iceland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of Iceland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the ero ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
