Landmannalaugar Iceland 2005 3
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Landmannalaugar Iceland 2005 3
Landmannalaugar () is a location in Iceland's Fjallabak Nature Reserve in the Highlands. It is at the edge of the Laugahraun lava field, formed in an eruption in approximately 1477. It is known for its natural geothermal hot springs and surrounding landscape. Landmannalaugar is at the northern end of the Laugavegur hiking trail, and the Iceland Touring Association operates a mountain hut accommodating hikers. During the high tourist season, a small shop and a horse tour agency operate there, as well as the ICE-SAR highland patrol in Fjallabak. Several bus companies have regular trips to and from Landmannalaugar during the tourist season. Routes Four routes lead to Landmannalaugar, including one accessible by car, though the road is rough, with large stones on the road and washboard sections. Rented cars are not allowed on either road, as F roads are usually only for four-wheel-drive vehicles. The most accessible route to Landmannalaugar is via Road 30 from the main r ...
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Landmannalaugar Campsite
Landmannalaugar () is a location in Iceland's Fjallabak Nature Reserve in the Highlands. It is at the edge of the Laugahraun lava field, formed in an eruption in approximately 1477. It is known for its natural geothermal hot springs and surrounding landscape. Landmannalaugar is at the northern end of the Laugavegur hiking trail, and the Iceland Touring Association operates a mountain hut accommodating hikers. During the high tourist season, a small shop and a horse tour agency operate there, as well as the ICE-SAR highland patrol in Fjallabak. Several bus companies have regular trips to and from Landmannalaugar during the tourist season. Routes Four routes lead to Landmannalaugar, including one accessible by car, though the road is rough, with large stones on the road and washboard sections. Rented cars are not allowed on either road, as F roads are usually only for four-wheel-drive vehicles. The most accessible route to Landmannalaugar is via Road 30 from the main ...
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Sprengisandur
Sprengisandur () is a highland plateau in Iceland, defined roughly as the area between the Hofsjökull and Vatnajökull glaciers. History and etymology Like Kjölur and Kaldidalur, Sprengisandur is an ancient pass - during the time of the Icelandic Free State (ca. 930–1265) it was one of the several important north–south routes that connected remote regions of the island to the Plains of the Parliament, Þingvellir, where the yearly parliament, Alþingi, was held each year at midsummer. In the sagas of Icelanders it is often called simply ''Sandr'' "Sand" or ''Sandleið'', "Sand trail". At its southern end, it was joined with another such route, Fjallabaksvegur nyrðri, running west from Landmannalaugar mountain hot springs area. Sprengisandur is only accessible during summer - like other parts of the inner desert, it is impassable in winter because of the snow, and in spring because of floods. While being the shortest way to the Alþingi for some Icelanders, for example ...
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Mýrdalsjökull
Mýrdalsjökull (pronounced , Icelandic for "(the) mire dale glacier" or "(the) mire valley glacier") is an ice cap in the south of Iceland. It is to the north of Vík í Mýrdal and to the east of the smaller ice cap Eyjafjallajökull. Between these two glaciers is Fimmvörðuháls pass. Its peak reaches in height and in the year 1980 it covered an area of approximately . The icecap of the glacier covers an active volcano called Katla. The caldera of the volcano has a diameter of and the volcano erupts usually every 40–80 years. The last eruption took place in 1918. Scientists are actively monitoring the volcano, particularly after the eruption of nearby Eyjafjallajökull began in April 2010. Since the year 930, 16 eruptions have been documented. The Eldgjá, a volcanic eruption fissure about long, which erupted in the year 936, is part of the same volcanic system. Before the Hringvegur (the main ring road round the island) was built, people feared traversing the pl ...
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Eyjafjallajökull
Eyjafjallajökull (; ), sometimes referred to by the numeronym E15, is one of the smaller ice caps of Iceland, north of Skógar and west of Mýrdalsjökull. The ice cap covers the caldera of a volcano with a summit elevation of . The volcano has erupted relatively frequently since the Last Glacial Period, most recently in 2010, when, although relatively small for a volcanic eruption, it caused enormous disruption to air travel across northern and western Europe for a week. Geography Eyjafjallajökull consists of a volcano completely covered by an ice cap. The ice cap covers an area of about , feeding many outlet glaciers. The main outlet glaciers are to the north: Gígjökull , flowing into Lónið , and Steinholtsjökull , flowing into Steinholtslón . In 1967, there was a massive landslide on the Steinholtsjökull glacial tongue. On 16 January 1967 at 13:47:55 there was an explosion on the glacier. It can be timed because the seismometers at Kirkjubæjarklaustur monitor ...
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Fimmvörðuháls
Fimmvörðuháls (; "five cairns pass") is the area between the glaciers Eyjafjallajökull and Mýrdalsjökull in southern Iceland. The route between Skógar and Thórsmörk goes through this pass and is one of the most popular walking routes in Iceland, despite being long and involving of climbing. There are two mountain huts along Fimmvörðuháls, one owned by hiking association Útivist, the other called Baldvinsskáli (). The route from Skógar has many waterfalls along the way. The route is only accessible between mid-June and late-August. On the night of 16 May 1970, three travellers died in the mountain pass in a snowstorm. Hiking the Fimmvörðuháls mountain pass takes 1–2 days. It is also possible to combine the Fimmvörðuháls route with the Laugavegur Trek between Landmannalaugar and Thórsmörk to make a trip of 4–6 days in length. 2010 eruption On 20 March 2010, an eruption of the Eyjafjallajökull volcano began in Fimmvörðuháls following mont ...
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Skógar
Skógar (pronounced ), literally "forests", is a small Icelandic village with a population of roughly 25 located at the south of the Eyjafjallajökull glacier, in the municipality of Rangárþing eystra. The area is known for its waterfall, Skógafoss, on the Skógá river, which springs from 60 metres at the top of an eroded cliff. At Skógar is a folk museum, Skógasafn , as well as a museum on transport in Iceland. Not far from Skógar is the Kvernufoss fall. Further upstream on the Skógá river there are a number of other falls. While climbing in the small forest behind the old school, some ruins of old farms can be seen. This settlement was severely affected by the 2010 eruptions of Eyjafjallajökull, eruption of the Eyjafjallajökull volcano in 2010. Gallery SkogarMuseumOutside.jpg, Museum of Skógar Skogarmuseum 2.jpg, Pétursey, ferry boat at the museum Þórður Tómasson.JPG, Þórður Tómasson (1921-2022), founder of the museum Þrasi's ring.jpg, Þrasi's ring ...
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Thórsmörk
Thórsmörk ( is, Þórsmörk, ) is a mountain ridge in Iceland that was named after the Norse god Thor (Þór). It is situated in the south of Iceland between the glaciers Tindfjallajökull and Eyjafjallajökull. The name "Thórsmörk" properly refers only to the mountain ridge between the rivers Krossá, Þröngá, and Markarfljót, but is sometimes used informally to describe a wider area that includes the region between Thórsmörk and Eyjafjallajökull. Thórsmörk is one of the most popular hiking areas in Iceland. In the valley, the river Krossá winds between the mountains. The valley is closed in between glaciers, Mýrdalsjökull being at the rear end of the valley. This leads to an especially warm climate, better than in the rest of south Iceland. In the protected valley, green vegetation of moss, fern, birchwood, and other small shrubs are found. Thórsmörk is popular amongst hikers. Many different tours are possible, from hiking on the glaciers to trekking (i.e., ...
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Hekla
Hekla (), or Hecla, is a stratovolcano in the south of Iceland with a height of . Hekla is one of Iceland's most active volcanoes; over 20 eruptions have occurred in and around the volcano since 874. During the Middle Ages, the Icelandic Norse called the volcano the "Gateway to Hell". Hekla is part of a volcanic ridge, long. The most active part of this ridge, a fissure about long named , is considered to be within Hekla proper. Hekla looks rather like an overturned boat, with its keel being a series of craters, two of which are generally the most active. The volcano's frequent large eruptions have covered much of Iceland with tephra, and these layers can be used to date eruptions of Iceland's other volcanoes. Approximately 10% of the tephra created in Iceland in the last thousand years has come from Hekla, amounting to 5 km3. Cumulatively, the volcano has produced one of the largest volumes of lava of any in the world in the last millennium, around 8 km3. Etymolo ...
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