|
Highlands Of Iceland
The Highlands of Iceland ( is, hálendið ) are a sparsely inhabited plateau that covers most of the interior of Iceland. They are situated above 400–500 metres (1300–1600 feet) and are mostly an uninhabitable volcanic desert, because the water precipitating as rain or snow infiltrates so quickly into the ground that it is unavailable for plant growth. This results largely in a surface of grey, black or brown earth, lava and volcanic ashes. A few oasis-like areas, such as Herðubreiðarlindir near Askja, are found only in proximity to rivers. Icelanders categorise the Highlands as: * "Háls", meaning a broad mountain ridge between valleys, such as the one near Langavatn north of Borgarnes; or * "Heiði", meaning the real highlands, such as those alongside the Sprengisandur road. Most of the numerous glaciers, such as Vatnajökull, Langjökull and Hofsjökull, are also part of the Icelandic Highlands. Vegetation is only found on the shores of the glacier rivers. There is al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Map Of Iceland Highlands-en
A map is a symbolic depiction emphasizing relationships between elements of some space, such as objects, regions, or themes. Many maps are static, fixed to paper or some other durable medium, while others are dynamic or interactive. Although most commonly used to depict geography, maps may represent any space, real or fictional, without regard to context or scale, such as in brain mapping, DNA mapping, or computer network topology mapping. The space being mapped may be two dimensional, such as the surface of the earth, three dimensional, such as the interior of the earth, or even more abstract spaces of any dimension, such as arise in modeling phenomena having many independent variables. Although the earliest maps known are of the heavens, geographic maps of territory have a very long tradition and exist from ancient times. The word "map" comes from the , wherein ''mappa'' meant 'napkin' or 'cloth' and ''mundi'' 'the world'. Thus, "map" became a shortened term referring to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hofsjökull
__NOTOC__ Hofsjökull ( Icelandic: "temple glacier", ) is the third largest ice cap in Iceland after Vatnajökull and Langjökull and the largest active volcano in the country. It is situated in the west of the Highlands of Iceland and north of the mountain range Kerlingarfjöll, between the two largest glaciers of Iceland. It covers an area of 925 km2, reaching at its summit. The subglacial volcano is a shield type with caldera. Hofsjökull is the source of several rivers including the Þjórsá, Iceland's longest river. In the southeast of Iceland, between the easternmost glacier tongue of Vatnajökull (Axajökull) and Þrándarjökull, there is a smaller glacier (area about 4 km2), which is also called Hofsjökull. In 2015, Hofsjökull increased in mass, the first time in 20 years this had happened. See also * Glaciers of Iceland * Iceland plume * List of volcanoes in Iceland Notes References * External links Hofsjökullin the Catalogue of Icelandic Volcano ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deserts Of Europe
A desert is a barren area of landscape where little precipitation occurs and, consequently, living conditions are hostile for plant and animal life. The lack of vegetation exposes the unprotected surface of the ground to denudation. About one-third of the land surface of the Earth is arid or semi-arid. This includes much of the polar regions, where little precipitation occurs, and which are sometimes called polar deserts or "cold deserts". Deserts can be classified by the amount of precipitation that falls, by the temperature that prevails, by the causes of desertification or by their geographical location. Deserts are formed by weathering processes as large variations in temperature between day and night put strains on the rocks, which consequently break in pieces. Although rain seldom occurs in deserts, there are occasional downpours that can result in flash floods. Rain falling on hot rocks can cause them to shatter, and the resulting fragments and rubble strewn over the d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highlands Of Iceland
The Highlands of Iceland ( is, hálendið ) are a sparsely inhabited plateau that covers most of the interior of Iceland. They are situated above 400–500 metres (1300–1600 feet) and are mostly an uninhabitable volcanic desert, because the water precipitating as rain or snow infiltrates so quickly into the ground that it is unavailable for plant growth. This results largely in a surface of grey, black or brown earth, lava and volcanic ashes. A few oasis-like areas, such as Herðubreiðarlindir near Askja, are found only in proximity to rivers. Icelanders categorise the Highlands as: * "Háls", meaning a broad mountain ridge between valleys, such as the one near Langavatn north of Borgarnes; or * "Heiði", meaning the real highlands, such as those alongside the Sprengisandur road. Most of the numerous glaciers, such as Vatnajökull, Langjökull and Hofsjökull, are also part of the Icelandic Highlands. Vegetation is only found on the shores of the glacier rivers. There is al ... [...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 Lakagígar, 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] |
Volcanism Of Iceland
:''The volcano system in Iceland that started activity on August 17, 2014, and ended on February 27, 2015, is Bárðarbunga.'' :''The volcano in Iceland that erupted in May 2011 is Grímsvötn.'' Iceland experiences frequent volcanic activity, due to its location both on the Mid-Atlantic Ridge, a divergent tectonic plate boundary, and over a hot spot. Nearly thirty volcanoes are known to have erupted in the Holocene epoch; these include Eldgjá, source of the largest lava eruption in human history. Volcanic systems and volcanic zones of Iceland Holocene volcanism in Iceland is mostly to be found in the ''Neovolcanic Zone'', comprising the Reykjanes Volcanic Belt (RVB), the West Volcanic Zone (WVZ), the Mid-Iceland Belt (MIB), the East Volcanic Zone (EVZ) and the North Volcanic Zone (NVZ). Two lateral volcanic zones play a minor role: Öræfi Volcanic Belt (ÖVB) and Snæfellsnes Volcanic Belt (SVB). Outside of the main island are the Reykjanes Ridge (RR), as part of the Mid-At ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Four-wheel Drive
Four-wheel drive, also called 4×4 ("four by four") or 4WD, refers to a two-axled vehicle drivetrain capable of providing torque to all of its wheels simultaneously. It may be full-time or on-demand, and is typically linked via a transfer case providing an additional output drive shaft and, in many instances, additional gear ranges. A four-wheel drive vehicle with torque supplied to both axles is described as "all-wheel drive" (AWD). However, "four-wheel drive" typically refers to a set of specific components and functions, and intended off-road application, which generally complies with modern use of the terminology. Definitions Four-wheel-drive systems were developed in many different markets and used in many different vehicle platforms. There is no universally accepted set of terminology that describes the various architectures and functions. The terms used by various manufacturers often reflect marketing rather than engineering considerations or significant technical diff ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kjölur
Kjölur () is a plateau in the highlands of Iceland, roughly defined as the area between the Langjökull and Hofsjökull glaciers. It lies at an elevation of about 600–700 metres. Geography At the northern end of the Kjölur road, near the headwaters of the Blanda river, the hot springs of Hveravellir provide a warm oasis. Not far from Hveravellir, the Kerlingarfjöll, a volcanic mountain range, is situated to the north-east of the Kjölur road. History Like Sprengisandur highland road, the area was probably known since the first times of Icelandic settlement and is mentioned in the Icelandic sagas. A track along Langjökull was used as a shortcut between regions during summer. This is today known as ''Kjalvegur hinn forni'' (Old Kjalvegur) and is still in use for trekking and horse-riding. Piles of stones mark the track through the highland desert. After some people had perished in a snowstorm by the end of the 18th century, the Kjölur road was forgotten for about 100 ye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaldidalur
The Kaldadalsvegur () is the shortest of the highland tracks traversing the Highlands of Iceland, therefore the nickname "highlands for beginners" . Its name derives from the valley it crosses: ''Kaldidalur'' means "cold dale/valley". Sometimes the Kaldadalsvegur is referred to as simply "the Kaldidalur". The route begins a bit to the north of Þingvellir and to the west of the volcano Skjaldbreiður, which really comes up to its name (meaning ''broad shield''). The track continues between the glaciers Þórisjökull and Ok and leads up to the north. To the east of Reykholt it comes near the ''Reykholtsdalur'' to Húsafell. Then it continues up to ''Hvammstangi'' at the ''Miðfjörður''. Signed as route 550 (formerly F550), the track is 40 kilometers long, and has no unbridged river crossings. (The Kaldadalsvegur is ''not'' an F road, and a four-wheel-drive vehicle is ''not'' legally required to traverse it, however many car rental companies forbid the use of their two-w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iceland Car Stuck In River 1972
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 permanent set ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Herðubreið
Herðubreið (, ''broad-shouldered'') is a tuya in northern part of Vatnajökull National Park, Iceland. It is situated in the Highlands of Iceland at the east side of the Ódáðahraun desert and close to Askja volcano. The desert is a large lava field originating from eruptions of Trölladyngja and other shield volcanoes in the area. Herðubreið was formed beneath the icesheet that covered Iceland during the last glacial period. Overview Due to the mountain's steep and unstable sides, the first ascent was in 1908 despite centuries of knowledge of its existence. The Mountain is often referred to as "The Queen of Icelandic Mountains" by Icelanders due to its beautiful shape. Near the mountain lies an oasis called Herðubreiðarlindir with a campground and hiking trails. In former times, outcasts who had been excluded from Icelandic society because of crimes they had committed lived at the oasis. One such outlaw was Fjalla-Eyvindur, who lived there during the winter of 177 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landmannalaugar
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
