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Bláfjöll From Plane
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] |
Bláfjöll From Plane
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] |
Tow Lift
A surface lift is a type of cable transport for snow sports in which skiers and snowboarders remain on the ground as they are pulled uphill. While they were once prevalent, they have been overtaken in popularity by higher-capacity and higher-comfort aerial lifts, such as chairlifts and gondola lifts. Today, surface lifts are most often found on beginner slopes, small ski areas, and peripheral slopes. They are also often used to access glacier ski slopes because their supports can be anchored in glacier ice due to the lower forces and realigned due to glacier movement. Surface lifts have some disadvantages compared to aerial lifts: they require more passenger skill and may be difficult for some beginners (especially snowboarders, whose boards point at an angle different than the direction of travel) and children; sometimes they lack a suitable route back to the piste; the snow surface must be continuous; they can get in the way of skiable terrain; they are relatively slow in spee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reykjanes Volcanic Belt
The Reykjanes Peninsula ( is, Reykjanesskagi ) in southwest Iceland is the continuation of the mostly submarine Reykjanes Ridge, a part of the Mid-Atlantic Ridge, on land and reaching from Esja in the north and Hengill in the east to Reykjanestá in the west.G.B.M. Pedersen, P. Grosse: ''Morphometry of subaerial shield volcanoes and glaciovolcanoes from Reykjanes Peninsula, Iceland: Effects of eruption environment. Journal of Volcanology and Geothermal Research 282'', (2014), 115-133. Retrieved 21 August 2020. Suðurnes (transl. |
Mountains Of Iceland
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sport In Iceland
Sports in Iceland are very popular. Popular sports include association football, football, handball, sport of athletics, athletics, basketball, :Chess in Iceland, chess, golf, volleyball, tennis, skiing, snowboarding, ice hockey, swimming (sport), swimming, rock climbing and mountain climbing; horseback riding on Icelandic horses is also popular and also archery. In some of those sports, namely football, handball, and basketball, Iceland is extremely successful, considering its population. It manages to compete at comparable level with countries that have 10-200 times its population. Iceland's most famous athlete comes from the world of football. Eiður Guðjohnsen has played in England's Premier League for Chelsea F.C. winning the league title and the Community Shield twice, as well as the League Cup once. He also played in La Liga for FC Barcelona, where he was part of the team that won the Treble (association football), Treble of the league, Copa del Rey and the UEFA Champions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heiðin Há
Heiðin há () is a shield volcano up on Hellisheiði at about 35 km to the south of Reykjavík in Iceland. The mountain has a height of 626 m.Björn Hróarsson: Hellahandbókin. Leiðsögn um 77 íslenska hraunhella. Reykjavík 2008, p. 103 Shield volcano The volcano dates from the Mid-Holocene, is - following B. Hróarsson - about 6,000 years old, slightly younger than the Selvogsheiði, another shield volcano on Reykjanes peninsula, whereas Sinton defines its age as “finiglacial”, i.e., from the beginning of Holocene. It covers about 160km2, and its volume is about 10km3. The volcano is part of the Brennisteinsfjöll volcanic system. The top crater is located south of Bláfjöll. It has a diameter of ca. 400m, but is mostly filled by lava up to the rim. The lava flows from Heiðin há went in all directions on Hellisheiði: They covered the highland up to the Bláfjöll and up to the tuya Geitafell in eastern direction, and enclosed the older shield volcano ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eldborg í Bláfjöllum
The volcanic cone of Eldborg í Bláfjöllum () is to be found at about 2 km from the skiing area in Bláfjöll, i.e. at about 25 km from Reykjavík, in Iceland.Ísland Vegaatlas. Reykjavík 2006, p.1 Scoria cones Eldborg í Bláfjöllum is a scoria cone, part of a group of three such small volcanoes. The crater group as well as the impressive lava channels and tubes nearby are products of eruptions within the Brennisteinsfjöll volcanic system around the year 1000.Ari Trausti Guðmundsson, Pétur Þorleifsson: Íslensk Fjöll. Gönguleiðir á 151 tind. Reykjavík 2004, p. 260 Accessibility Route 407 (Iceland), Route 407 to the skiing area in Bláfjöll passes by the crater. Some marked hiking trails connect the cone group of Eldborgir with the bigger mountains in the vicinity and other trails, e.g. the Reykjavegur Hiking Trail. In the wintertime, cross country skiing is possible on cross-country ski-tracks in the area. Natural monument Eldborg and its surroundi ... [...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, on the southwest coast of the country. At about 30,000 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 each summer. Local industry Just two kilometres () outside of Hafnarfjörður is an aluminium smelter, run by Alcan. The smelter was originally built in 1969, and it has improved its cleaning process since then, especially regarding fluoride. Local elections were held in May 2006, where ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Route 417
The following highways are numbered 417: Canada * Manitoba Provincial Road 417 * Newfoundland and Labrador Route 417 * Ontario Highway 417 Costa Rica * National Route 417 Iceland * Route 417 Japan * Japan National Route 417 United States * Florida State Road 417 * Georgia State Route 417 (unsigned designation for Interstate 575) * Maryland Route 417 (former) * North Carolina Highway 417 (future) * New York: ** New York State Route 417 ** New York State Route 417 New York State Route 417 (NY 417) is an east–west state highway located in the Southern Tier of New York in the United States. It begins at exit 20 of the Southern Tier Expressway ( Interstate 86 or I-86 and NY 17) i ... (former) * Pennsylvania Route 417 * Puerto Rico Highway 417 * South Carolina Highway 417 * Tennessee State Route 417 {{Road index, 417 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandskeið
Sandskeið () is the main gliding center in Iceland and home of the Icelandic gliding club ( Svifflugfélag Íslands) since 1936. It is situated 20 km to the east of Reykjavík, the Icelandic capital, by Route 1 The following highways are numbered 1. For roads numbered A1, see list of A1 roads. For roads numbered B1, see list of B1 roads. For roads numbered M1, see List of M1 roads. For roads numbered N1, see list of N1 roads. For roads numbered .... It is a big grass airfield, the main runway is running 150/330 and is 200 x 1.300 meters with the new extension to the east which is 50 x 300 m to allow for greater height when winch launching. There is also a north/south runway 60 x 800 m. On the north side there is an 18 x 800 m paved runway running 150/330. Height above sea level is 180 m (600 ft). The radio frequency used is 119,90 MHz and there is an ATZ open when gliding activity is present which goes from gnd to 3000 ft msl and covers the airfield ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hringvegur
Route 1 or the Ring Road ( or ) is a national road in Iceland that circles the entire country. As a major 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 tourist traffic. The total length of the road is . The road was completed in 1974, coinciding with the 1,100th anniversary of 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, such as the Seljalandsfoss and Skógafoss waterfalls, Dyrhólaey cliffs, Jökulsárlón glacier lagoon, as well ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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