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Skaftafell
Skaftafell () is a preservation area in Öræfi, southeast Iceland. It was once a major farm, later being named a national park. Originally known as Skaftafell National Park, it was subsequently joined together with other nearby regions to form the larger Vatnajökull National Park. Skaftafell National Park Skaftafell National Park was a national park, situated between Kirkjubæjarklaustur, typically referred to as Klaustur, and Höfn in the south of Iceland. On 7 June 2008, it became a part of the larger Vatnajökull National Park. It was founded on September 15, 1967, and enlarged twice afterwards. Before its inclusion into Vatnajökull National Park, it measured about 4807 km2 (2884 mi2), making it Iceland's second largest national park. It contains the valley ''Morsárdalur'' , the mountain ''KristÃnartindar'' and the glacier ''Skaftafellsjökull'' (a spur of the Vatnajökull ice cap). The landscape is very similar to some of the Alps, but it has been formed o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skaftafell View
Skaftafell () is a preservation area in Öræfi, southeast Iceland. It was once a major farm, later being named a national park. Originally known as Skaftafell National Park, it was subsequently joined together with other nearby regions to form the larger Vatnajökull National Park. Skaftafell National Park Skaftafell National Park was a national park, situated between Kirkjubæjarklaustur, typically referred to as Klaustur, and Höfn in the south of Iceland. On 7 June 2008, it became a part of the larger Vatnajökull National Park. It was founded on September 15, 1967, and enlarged twice afterwards. Before its inclusion into Vatnajökull National Park, it measured about 4807 km2 (2884 mi2), making it Iceland's second largest national park. It contains the valley ''Morsárdalur'' , the mountain ''KristÃnartindar'' and the glacier ''Skaftafellsjökull'' (a spur of the Vatnajökull ice cap). The landscape is very similar to some of the Alps, but it has been formed o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vatnajökull National Park
Vatnajökull National Park ( is, Vatnajökulsþjóðgarður ) is one of three national parks in Iceland. It encompasses all of Vatnajökull glacier and extensive surrounding areas. These include the national parks previously existing at Skaftafell in the southwest and Jökulsárgljúfur in the north. The unique qualities of Vatnajökull National Park are primarily its great variety of landscape features, created by the combined forces of rivers, glacial ice, and volcanic and geothermal activity. On 5 July 2019, Vatnajökull National Park was inscribed as a World Heritage Site. History Vatnajökull National Park was established on 7 June 2008. When established, the park covered an area of 12,000 km2, but with recent additions of LakagÃgar, Langisjór, Krepputunga and Jökulsárlón (including its surrounding areas) it now covers 14,141 km2 or approximately 14% of Iceland, making it Europe's second largest national park in terms of area after Yugyd Va in Russia. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Lake Outburst Flood
A glacial lake outburst flood (GLOF) is a type of outburst flood caused by the failure of a dam containing a glacial lake. An event similar to a GLOF, where a body of water contained by a glacier melts or overflows the glacier, is called a jökulhlaup. The dam can consist of glacier ice or a terminal moraine. Failure can happen due to erosion, a buildup of water pressure, an avalanche of rock or heavy snow, an earthquake or cryoseism, volcanic eruptions under the ice, or massive displacement of water in a glacial lake when a large portion of an adjacent glacier collapses into it. Increasing glacial melting because of climate change, alongside other environmental effects of climate change (i.e permafrost melting) mean that regions with glaciers are likely to see increased flooding risks from GLOFs. This is especially true in the Himalayas where geologies are more active. Definition A glacial lake outburst flood is a type of outburst flood occurring when water dammed by a glac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skeiðará
Skeiðará () is a relatively short glacier river (about 30 km long). It has its source on the glacier Skeiðarárjökull, one of the southern arms of the Vatnajökull in the south of Iceland. In spite of its short length, this river has a bad reputation. It is especially feared because of the frequent glacier runs that can be fatal. In front of Skaftafell and Skeiðarárjökull, Skeiðará has formed the Skeiðarársandur, a black plain of lava sand and ashes crossed by a lot of small rivulets which covers the whole area between the park and the sea (about 40 km long and 5 to 10 km wide). In 1996, the latest of these glacier runs took place. It destroyed parts of Route 1 (the Ring Road). The bridge was damaged by floating ice boulders the size of houses. At the peak of this glacier run, 45,000 m3/s of water were coming down. No one was harmed, scientists having very carefully monitored the volcano GrÃmsvötn on Vatnajökull which caused the glacier run by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Höfn
Höfn () or Höfn à Hornafirði () is an Icelandic fishing town in the southeastern part of the country. It lies near Hornafjörður fjord. The town, the second largest in the southeastern part of Iceland, offers scenic views of Vatnajökull (the largest ice cap in Europe by volume). The community was formerly known as Hornafjarðarbær between 1994 and 1998. Geography Höfn is located on a peninsula in the southeast of Iceland. The name Höfn means harbour and it is a fishing port surrounded on three sides by the sea, with beaches on a long shoreline to the southeast. Shoals and glacial rivers traverse this area with many shifting lagoons and sand reefs being formed. Höfn is surrounded by several small islands to the east of the town, the largest of which is Mikley , followed by Krókalátur and Hellir . Nearby areas include Suðursveit (the birthplace of Þórbergur Þórðarson), Öræfasveit, Lón , Mýrar and Nes . In Nes there is a small village called Nesjahv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vatnajökull
Vatnajökull ( Icelandic pronunciation: , 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. It is in the south-east of the island, covering approximately 8% of the country. Size With an area of 7,900 km2, Vatnajökull is the second largest ice cap in Europe by volume (about 3,000 km3) and area (after the still larger Severny Island ice cap of Novaya Zemlya, Russia, which is in the extreme northeast of Europe). On 7 June 2008, it became a part of the Vatnajökull National Park. The average thickness of the ice is , with a maximum thickness of . Iceland's highest peak, Hvannadalshnúkur (), as part of the Öræfajökull, is in the southern periphery of Vatnajökull, near Skaftafell. Volcanoes Under the ice cap, as under many of the glaciers of Iceland, there are several List of volcanoes in Ice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Öræfajökull
Öræfajökull (; ' Öræfi glacier' or 'wasteland glacier') is an ice-covered volcano in south-east Iceland. The largest active volcano and the highest peak in Iceland at , it lies within the Vatnajökull National Park and is covered by part of the glacier. The original Norse settlers named the volcano KnappafellsjÇ«kull (Old Norse: ; Modern Icelandic: Hnappafellsjökull ; 'knobs mountain glacier'). The current name, ''Öræfajökull'', was eventually adopted after the 1362 eruption. Description Öræfajökull is located at the southern extremity of the Vatnajökull glacier and overlooking the Ring Road between Höfn and VÃk. It is the largest active volcano in the country, and on the summit crater's northwestern rim is Hvannadalshnúkur, the highest peak in Iceland at . Geographically, Öræfajökull is considered part of Vatnajökull, and the area covered by glacier is within the boundary of Vatnajökull National Park. Activity Öræfajökull has erupted twice in historic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
GrÃmsvötn
GrÃmsvötn (; ''vötn'' = "waters", singular: ) is a volcano with a (partially subglacial) fissure system located in Vatnajökull National Park, Iceland. The volcano itself is completely subglacial and located under the northwestern side of the Vatnajökull ice cap. The subglacial caldera is at , at an elevation of . Beneath the caldera is the magma chamber of the GrÃmsvötn volcano. GrÃmsvötn is a basaltic volcano which has the highest eruption frequency of all the volcanoes in Iceland and has a southwest-northeast-trending fissure system. The massive climate-impacting Laki fissure eruption of 1783–1784 was a part of the same fissure system. GrÃmsvötn was erupting at the same time as Laki during 1783, but continued to erupt until 1785. Because most of the volcanic system lies underneath Vatnajökull, most of its eruptions have been subglacial and the interaction of magma and meltwater from the ice causes phreatomagmatic explosive activity. Jökulhlaup Eruptions in the cal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hof, Iceland
Hof, () in Öræfi, is a cluster of farms in the municipality of Sveitarfélagið Hornafjörður in southeast Iceland, close to Vatnajökull glacier, and twenty two kilometres south of Skaftafell in Vatnajökull National Park. It is on the Route 1 southwest of Höfn, in the narrow strip between the sea coast and the glacier. It is 9.14 km WSW of the centre of Öræfajökull volcano. A notable building in Hof is a turf church, which was built in 1883 and is the youngest turf church in Iceland. Since 1951, it belongs to the National Museum of Iceland National may refer to: Common uses * Nation or country ** Nationality – a ''national'' is a person who is subject to a nation, regardless of whether the person has full rights as a citizen Places in the United States * National, Maryland, ce .... References Populated places in Eastern Region (Iceland) {{Iceland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svartifoss
Svartifoss ( Icelandic for "black waterfall", ) is a waterfall in Skaftafell in Vatnajökull National Park in Iceland, and is one of the most popular sights in the park. It is surrounded by dark lava columns, which gave rise to its name. The base of this waterfall is noteworthy for its sharp rocks. New hexagonal column sections break off faster than the falling water wears down the edges. These basalt columns have provided inspiration for Icelandic architects, most visibly in the HallgrÃmskirkja church in ReykjavÃk, and also the National Theatre. Gallery Svartifoss July 2014.JPG, Svartifoss in summer Waterfall-svartifoss.jpg, Bulb Svartifoss winter.jpg, Long exposure photograph of the Svartifoss waterfall References External links Information about hiking routes in Skaftafell, including Svartifoss. See also * List of columnar basalts in Iceland * List of waterfalls in Iceland Iceland is unusually suited for waterfalls (Icelandic: s. ''foss,'' pl. ''fossar'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kirkjubæjarklaustur
Kirkjubæjarklaustur ( Icelandic for "church farm cloister", pronounced ; often referred to locally as just Klaustur) is a village in the south of Iceland on the hringvegur (road no. 1 or Ring Road) between VÃk à Mýrdal and Höfn. It is part of the municipality of Skaftárhreppur and has about 500 inhabitants. It is surrounded by hills and plateaus to the north. Kirkjubæjarklaustur is roughly east of the capital Reykjavik. Location Kirkjubæjarklaustur's geographical location makes it better known than other villages its size. It is the only place between VÃk and Höfn which offers services, which includes a fuel station, a bank, a post office and a supermarket. Nearby tourist attractions include the Laki craters, the Eldgjá and Skaftafell, all in Vatnajökull National Park. An attraction close to the village is '' Kirkjugólf'' ("Church floor"), a natural pavement of basalt. These are basalt columns in the earth, but only the tops can be seen, and as the name suggests, t ... [...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 pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
