HOME
*





Háifoss
Háifoss () is a waterfall situated near the volcano Hekla in southern Iceland. The waterfall Granni is next to it. The river ''Fossá'', a tributary of Þjórsá, drops here from a height of 122 m. This is the fourth highest waterfall of the island, after Morsárfoss, Glymur and Hengifoss. From the historical farm Þjóðveldisbærinn Stöng, which was destroyed by a volcanic eruption of Hekla in the Middle Ages and reconstructed, it is possible to hike to the waterfall along the Fossá (5 to 6 hours both directions). Above the waterfall, there is also a parking lot, to allow hiking to be done in the other direction. See also * Waterfalls of Iceland Iceland is unusually suited for waterfalls (Icelandic: s. ''foss,'' pl. ''fossar''). This island country has a north Atlantic climate that produces frequent rain and snow and a near-Arctic location that produces large glaciers, whose summer mel ... References External links Photo Waterfalls of Iceland {{Icelan ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Granni Waterfall
The Granni () is a waterfall that cascades into the Fossardalur right beside the Háifoss. History These two waterfalls did not have a name until the beginning of the 19th century, but ''Nágranni'' or ''granni'' is the Icelandic word for ''neighbor'' while ''Hái'' means ''tall''. The name of the waterfall is based on the proximity to the neighbouring waterfall Háifoss, which is less than 250 meters away and fed by the same river. The river Fossá í Þjórsárdal is divided into two arms some 750 meters upstream from the waterfalls. Granni has a height of 101 meters and less power than the 122 meters high Háifoss. Downstream at the bottom the two separate rivers converge again into the Fossa river. Both waterfalls can be seen from a sightseeing platform which is on the south side of the falls. The volcano Hekla is within sight in the background. See also * List of waterfalls * Waterfalls of Iceland Iceland is unusually suited for waterfalls (Icelandic: s. ''foss,'' pl ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Waterfalls Of Iceland
Iceland is unusually suited for waterfalls (Icelandic: s. ''foss,'' pl. ''fossar''). This island country has a north Atlantic climate that produces frequent rain and snow and a near-Arctic location that produces large glaciers, whose summer melts feed many rivers. As a result, it is home to a number of large and powerful waterfalls. North * Dettifoss is the most powerful waterfall in Iceland. * Gljúfursárfoss * Selfoss * Hafragilsfoss * Goðafoss * Aldeyjarfoss South * Faxi or Vatnsleysufoss in Tungufljót river * Foss á Síðu * Gluggafoss * Gljúfrafoss * Gjáin has many small waterfalls * Gullfoss (''Golden Falls'') * Háifoss (''High Falls'') * Hjálparfoss * Merkjárfoss * Ófærufoss used to be noted for the impressive natural bridge which stood above the falls, but it collapsed in 1993. * Seljalandsfoss * Skógafoss (''Forest Falls'') * Svartifoss (''Black Falls'') is one of the many waterfalls of Skaftafell National Park * Systrafoss, in Kirkju ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Þjórsá
Þjórsá () is Iceland's longest river at 230 kilometers (about 143 miles). It is in the south of the island. Þjórsá is a glacier river and has its source on the glacier Hofsjökull. It flows out through narrow gorges in the highlands of Iceland. Further downstream, another river, the Tungnaá, flows into it (see also Háifoss), before it enters the lowlands. There it passes the valley of Þjórsárdalur (Thjorsardalur) where the historical farm of Stöng is located. In the lowlands it flows along the eastern border of the Great Þjórsá Lava. In the middle of the now rather wide river, there is a big island called ''Árnes'', where there used to be a '' Þing''. The administrative unit of Árnessýsla was named after it. The ''hringvegur'' (Road No.1) traverses the river via a bridge between Selfoss and Hella. Some kilometers to the southwest the river flows into the Atlantic Ocean. 'Á' signifies river while 'þjór' means bull and is cognate to Danish - tyr, Swedish ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Iceland
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 p ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Morsárfoss
Morsárfoss () is a waterfall in Vatnajökull National Park, Iceland. Measurements showed that one of them was at least 240 meters in total height, making it the highest waterfall in Iceland. Morsárfoss became visible in 2007 when Morsárjökull, an outlet glacier of 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 ... glacier, started melting. References External links Waterfalls of Iceland {{Iceland-geo-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Glymur
Glymur () is the second-highest waterfall in Iceland, with a cascade of 198 m. It was long regarded as the tallest until being surpassed by Morsárfoss, a newly measured waterfall near Morsárjökull in 2011. It is situated at the rear end of the Hvalfjörður. Since the opening of the Hvalfjörður Tunnel under this fjord, visitor numbers have dropped. The river Botnsá runs from the Hvalvatn lake and after a short distance the water falls down alongside the Hvalfell mountain into a steep canyon. The waterfall can be accessed from a parking area at the end of the road. Hikers can view the waterfall from marked paths on the east side of the river Botnsá. Gallery Glymurschlucht.JPG, Downstream view of the canyon Rauðhöfði.jpg, Legend of Rauðhöfði Second picture is an engraving showing people trying to escape from a monster whale. It is an illustration to the Icelandic legend of Redhead (Rauðhöfði ) which is said to be the cause of formation of Glymur. See also ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Hengifoss
Hengifoss () is the third highest waterfall in Iceland, 128 meters. It is located in Hengifossá in Fljótsdalshreppur, East Iceland. It is surrounded by basaltic strata with thin, red layers of clay between the basaltic layers. Fossilized trunks of coniferous trees, sensitive to cold, and lignite, which depict warmer climates during the latter part of Tertiary. Further down the Hengifossá river is Litlanesfoss, notable for the columnar jointed volcanics around it. Hengifoss is the most popular hiking site in East Iceland with path leading from the parking lot to the falls. It takes 40–60 minutes to walk to the waterfall. See also * List of waterfalls in Iceland Iceland is unusually suited for waterfalls (Icelandic: s. ''foss,'' pl. ''fossar''). This island country has a north Atlantic climate that produces frequent rain and snow and a near-Arctic location that produces large glaciers, whose summer mel ... References Waterfalls of Iceland {{Iceland ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Þjóðveldisbærinn Stöng
Þjóðveldisbærinn Stöng (, ''Stöng Commonwealth Farm'') is a reconstructed viking-era farmstead in Iceland, located in the Þjórsárdalur valley near road 32 in Árnessýsla county. It is a historically accurate reconstruction of the three buildings, including a longhouse, which stood 7 km to the north at Stöng; the farm is believed to have been buried under volcanic ash in 1104 following the eruption of the volcano 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 .... The reconstruction was built in 1974 as a part of the national celebrations of the 1100th anniversary of the settlement of Iceland in 874. External links * Museums in Iceland Archaeological sites in Iceland Former populated places in Iceland History museums in Iceland {{Iceland-geo-stu ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Middle Ages
In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the post-classical period of global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern period. The medieval period is itself subdivided into the Early, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralized authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the 7th century, North Africa and the Middle East—most recently part of the Eastern Ro ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]