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Kúðafljót
The Kúðafljót () is a river in the south of Iceland. It is one of the largest glacier rivers in the country. Name The ''Landnámabók'' reports that the name is from the ship of Vilbald, one of the first settlers in Skaftátunga. The name of the ships was ''Kúði''. Location and tributaries It flows east of the Mýrdalsjökull through the ''Skaftátunga'' district and flows into the Atlantic Ocean through the Mýrdalssandur from numerous tributaries, the most important of which are Hólmsá, Tungufljót and Eldvatn. An arm of the Skaftá also flows into the Kúðafljót.cf. Water quantity The mean water volume is 230 m³/s. The lowest measured value was 110 m³/s and the maximum measured value 2000 m³/s. The Kúðafljót is one of the rivers whose water level may indicate volcanic activity of Katla under the Mýrdalsjökull. Therefore, it is monitored closely. The Icelandic Meteorological Office monitors the Hólmsá, Eldvatn and Skálm tributaries. Eruptions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mýrdalssandur
Mýrdalssandur () is an outwash plain on the south coast of Iceland. Location and description The outwash plain is located between the rivers of Kúðafljót in the east and Múlakvísl in the west. Both rivers carry water from the Mýrdalsjökull glacier to the sea. Mýrdalssandur has a -long coast line, including Kötlutangi , the southernmost point of the island of Iceland. The Ring Road crosses this flat surface on . Development The outwash plain was built by the numerous jökulhlaups of the Mýrdalsjökull. The last large jökulhlaup was due to an explosive eruption of the Katla volcano under the glacier in 1918, and the water volume at the peak of the jökulhlaup was estimated to be around 200,000 - 300,000 m³/s. History of settlements South of the road rises Hjörleifshöfði to a height of . The mountain is named after Hjörleifr Hróðmarsson. He was the first settler to come to Iceland with Ingólfr Arnarson. In the Middle Ages there was a fishing lake called ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Iceland
On an island like Iceland, the rivers are short in length. None of the rivers are important as a means of navigation due to the impracticality of settlements in the Highlands of Iceland where they originate. South * Hvítá * Krossá *Kúðafljót * Markarfljót * Mustafl *Ölfusá (the Icelandic river with the greatest flow) * Rangá *Skaftá *Skeiðará * Skógá * Sog *Þjórsá (the longest river in Iceland, 230 km) *Tungnaá West *Fossá * Hvítá * Kjarrá–Thervá * Norðurá Westfjords * Dynjandi * Kolbeinsá * Staðará North *Blanda * Eyjafjarðará * Eystri Jökulsá * Fnjóská * Glerá * Grafará * Gönguskarðsá * Heiðará *Héraðsvötn * Hjaltadalsá * Hofsá (Skagafjörður) * Hofsá (Vesturdalur) * Hörgá *Jökulsá á Fjöllum * Kolka (Kolbeinsdalsá) * Laxá * Norðurá * Sauðá *Skjálfandafljót * Svartá * Sæmundará * Vatnsdalsá East * Hamarsá * Hofsá *Jökulsá á Dal * Jökulsá í Fljótsdal *Jökulsá í Lóni *Lagarflj� ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skaftá
The Skaftá () is a river in South Iceland. It is primarily glacial in origin and has had its course modified by volcanic activity; as a result of both, it often floods because of glacial melting. Course The river's primary source is two subglacial "cauldrons" beneath Skaftájökull, part of the Vatnajökull glacier in the interior of Iceland. It also receives spring-fed water from Langisjór, a lake a short distance to the west from which a tributary called the Útfall runs into the Skaftá. Other tributaries include the North and South Ófaerá, the Grjótá, and the Hellisá. West of Skaftárdalur, a farm named for the river valley, the Skaftá runs over a lava field in many channels, which recombine into three for the remainder of its course to the Atlantic The Atlantic Ocean is the second largest of the world's five oceanic divisions, with an area of about . It covers approximately 17% of Earth's surface and about 24% of its water surface area. During the Age of D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iceland
Iceland is a Nordic countries, Nordic island country between the Atlantic Ocean, North Atlantic and Arctic Oceans, on the Mid-Atlantic Ridge between North America and Europe. It is culturally and politically linked with Europe and is the region's westernmost and most list of countries and dependencies by population density, sparsely populated country. Its Capital city, capital and largest city is Reykjavík, which is home to about 36% of the country's roughly 380,000 residents (excluding nearby towns/suburbs, which are separate municipalities). The official language of the country is Icelandic language, Icelandic. Iceland is on a rift between Plate tectonics, tectonic plates, and its geologic activity includes geysers and frequent Types of volcanic eruptions, volcanic eruptions. The interior consists of a volcanic plateau with sand and lava fields, mountains and glaciers, and many Glacial stream, glacial rivers flow to the sea through the Upland and lowland, lowlands. Iceland i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Route 1 (Iceland)
Route 1 or the Ring Road ( or ) is a National road (Iceland), national road in Iceland that circles the entire country. As a major Trunk road, trunk route, it is considered to be the most important piece of transport infrastructure in Iceland as it connects the majority of towns together in the most densely populated areas of the country. Economically, it carries a large proportion of goods traffic as well as Tourism, tourist traffic. The total length of the road is , making it the longest ring road in Europe. The road was completed in 1974, coinciding with the 1,100th anniversary of Settlement of Iceland, the country's settlement when the longest bridge in Iceland, crossing the Skeiðará river in the southeast, was opened. Previously, vehicles intending to travel between southern settlements, e.g. Vík to Höfn, had to travel north of the country through Akureyri, making the opening a major transport improvement to the country. Many popular tourist attractions in Iceland, su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Iceland
Iceland is an island country at the confluence of the Atlantic Ocean, North Atlantic and Arctic Ocean, Arctic oceans, east of Greenland and immediately south of the Arctic Circle, atop the constructive boundary of the northern Mid-Atlantic Ridge. The island country is the world's List of islands by area#Islands, 18th largest in area and one of the most List of sovereign states and dependent territories by population density, sparsely populated. It is the westernmost European country when not including Greenland and has more land covered by glaciers than continental Europe. Its total size is and possesses an exclusive economic zone of . Statistics 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. Extent (locations outside mainland in parentheses) :North: Rifstangi, 66°32′3" N (Kolbeinsey, 67°08,9 N) :South: Kötlutangi, 63°23′6" N ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ship Graveyard
A ship graveyard, ship cemetery or breaking yard is a location where the hulls of scrapped ships are left to decay and disintegrate, or left in reserve. Such a practice is now less common due to waste regulations and so some dry docks where ships are broken (to recycle their metal and remove dangerous materials like asbestos) are also known as ship graveyards. By analogy, the phrase can also refer to an area with many shipwrecks which have not been removed by human agency, instead being left to disintegrate naturally. These can form in places where navigation is difficult or dangerous (such as the Seven Stones, off Cornwall, or Blackpool, on the Irish Sea); or where many ships have been deliberately scuttled together ( as with the German High Seas Fleet at Scapa Flow); or where many ships have been sunk in battle (such as Ironbottom Sound, in the Pacific). The majority of the ships in the world are constructed in the developed countries. Ships last about 25–30 year ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brittany (administrative Region)
The region Brittany ( ; ; Gallo: ''Bertaèyn'' ) is an administrative region of Metropolitan France, comprising the departments of Côtes-d'Armor, Finistère, Ille-et-Vilaine, and Morbihan. Its capital and largest city is Rennes. Bordered by the English Channel to the north, the Celtic Sea to the west, and the Atlantic Ocean ( Bay of Biscay) to the south, Brittany's neighboring regions are Normandy to the northeast and Pays de la Loire to the southeast. It is one of two regions in Metropolitan France where all departments have direct access to the sea, the other being Corsica. The region of Brittany is sometimes referred to as “administrative Brittany” in contrast to “historical Brittany” or “cultural Brittany”, which also includes the Loire-Atlantique and the question of its connection with the rest of the administrative region is being discussed. History Brittany, located in the west-northwest corner of France, is one of the historic province ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjarðabyggð
Fjarðabyggð () is a municipality located in eastern Iceland, in the Eastern Region. History The municipality was formed in 1998 with the union of the former municipalities of Eskifjörður, Neskaupstaður and Reyðarfjörður. Austurbyggð, Fáskrúðsfjarðarhreppur and Mjóafjarðarhreppur were merged into Fjarðabyggð in 2006, and Breiðdalshreppur merged in 2018. Geography The municipality is composed by the following villages: Twin towns – sister cities Fjarðabyggð is twinned with: * Esbjerg, Denmark * Eskilstuna, Sweden * Gravelines, France * Jyväskylä, Finland * Qeqqata, Greenland * Stavanger, Norway * Vágar Vágar (; ) is one of the 18 islands in the archipelago of the Faroe Islands and the most westerly of the ''large islands''. With a size of , it ranks third in size, behind Streymoy and Eysturoy. Vágar Regions of the Faroe Islands, region also ..., Faroe Islands References External links Official websiteVisit Fjarðabyggð Municipalit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjord
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or gla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jökulhlaup
A jökulhlaup ( ) (literally "glacial run") is a type of glacial outburst flood. It is an Icelandic term that has been adopted in glaciological terminology in many languages. It originally referred to the well-known subglacial outburst floods from Vatnajökull, Iceland, which are triggered by geothermal heating and occasionally by a volcanic subglacial eruption, but it is now used to describe any large and abrupt release of water from a subglacial or proglacial lake/reservoir. Since jökulhlaups emerge from hydrostatically sealed lakes with floating levels far above the threshold, their peak discharge can be much larger than that of a marginal or extra-marginal lake burst. The hydrograph of a jökulhlaup from Vatnajökull typically either climbs over a period of weeks with the largest flow near the end, or it climbs much faster during the course of some hours. These patterns are suggested to reflect channel melting, and sheet flow under the front, respectively. Similar p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
