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Norse Settlement In The Faroe Islands
Norse settlement in the Faroe Islands can be traced back to sometime between the 9th and 10th centuries, with the first Norsemen on the islands arguably around the late 8th century. Accounts from Irish priests such as Dicuil claim monks were there hundreds of years beforehand. Settlement The history of Viking Age settlement of the Faroe Islands comes from the ''Færeyinga saga'', a manuscript that is now lost. Portions of the tale were inscribed in three other sagas, such as ''Flateyjarbók'' and '' Saga of Óláfr Tryggvason''. Similar to other sagas, the historical credibility of the Færeyinga saga is often questioned. Both the ''Saga of Ólafr Tryggvason'' and ''Flateyjarbók'' claim a man named Grímur Kamban was the first man to discover the Faroe Islands. However, the two sources disagree on the year in which he left and the cause of his departure. ''Flateyjarbók'' details the emigration of Grímur Kamban as sometime during the reign of King Harald Hårfagre, between 872 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norsemen
The Norsemen (or Norse people) were a North Germanic ethnolinguistic group of the Early Middle Ages, during which they spoke the Old Norse language. The language belongs to the North Germanic branch of the Indo-European languages and is the predecessor of the modern Germanic languages of Scandinavia. During the late eighth century, Scandinavians embarked on a large-scale expansion in all directions, giving rise to the Viking Age. In English-language scholarship since the 19th century, Norse seafaring traders, settlers and warriors have commonly been referred to as Vikings. Historians of Anglo-Saxon England distinguish between Norse Vikings (Norsemen) from Norway who mainly invaded and occupied the islands north and north-west of Britain, Ireland and western Britain, and Danish Vikings, who principally invaded and occupied eastern Britain. Modern descendants of Norsemen are the Danes, Icelanders, Faroe Islanders, Norwegians, and Swedes, who are now generally referred to as "Sc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandavágur Stone
The Sandavágur stone (FR 2 M) is a runestone that was discovered in the town of Sandavágur on the Faroe Islands in 1917. The stone can today be seen in the Sandavágur Church. The inscription describes Þorkell, a man from Rogaland, Norway Norway, officially the Kingdom of Norway, is a Nordic country in Northern Europe, the mainland territory of which comprises the western and northernmost portion of the Scandinavian Peninsula. The remote Arctic island of Jan Mayen and the ... who claims to have lived in the Sandavágur area first. He is presumably one of the first settlers, if not the very first one. In both runes and language the Sandavágur stone corresponds to what is known from Rogaland around the 13th century. See also * Fámjin stone * Kirkjubøur stone References {{DEFAULTSORT:Sandavagur stone Runestones on the Faroe Islands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandur, Faroe Islands
Sandur (meaning ''sandy beach''; da, Sand) is a village on the south coast of the island of Sandoy in the Faroe Islands. The Sandur hoard of silver coins, dating to the end of the 11th century, attests to the long history of the village. In January 2020 the population stood at 532. The Municipality of Sandur consists of the village of Sandur only. It is the most populous place on the "Sand Island", and is situated on a peninsula between the lakes of Gróthúsvatn in the northwest and Sandsvatn in the northeast, facing the inlets of Grótvík and Sandsvágur in the south. History Sandur is an old site of the thing where every year the local Várting was held. Excavations here have unearthed a stave church from the 11th century, where today there is a typical Faroese wooden church with grass roof. In 1988 the modern church suffered a devastating fire in which all of the church's silver melted. The fire turned out to be arson. In the following year the church was restored, just in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steatite
Soapstone (also known as steatite or soaprock) is a talc-schist, which is a type of metamorphic rock. It is composed largely of the magnesium rich mineral talc. It is produced by dynamothermal metamorphism and metasomatism, which occur in the zones where tectonic plates are subducted, changing rocks by heat and pressure, with influx of fluids, but without melting. It has been a medium for carving for thousands of years. Terminology The definitions of the terms "steatite" and "soapstone" vary with the field of study. In geology, steatite is a rock that is to a very large extent composed of talc. The mining industry will define steatite as a high-purity talc rock that is suitable for manufacturing of, for example, insulators, the lesser grades of the mineral can be called simply "talc rock". Steatite can be used both in lumps ("block steatite", "lava steatite", "lava grade talc"), and in the ground form. While the geologists logically will use "steatite" to designate both forms, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puffin
Puffins are any of three species of small alcids (auks) in the bird genus ''Fratercula''. These are pelagic seabirds that feed primarily by diving in the water. They breed in large colonies on coastal cliffs or offshore islands, nesting in crevices among rocks or in burrows in the soil. Two species, the tufted puffin and horned puffin, are found in the North Pacific Ocean, while the Atlantic puffin is found in the North Atlantic Ocean. All puffin species have predominantly black or black and white plumage, a stocky build, and large beaks that get brightly colored during the breeding season. They shed the colorful outer parts of their bills after the breeding season, leaving a smaller and duller beak. Their short wings are adapted for swimming with a flying technique underwater. In the air, they beat their wings rapidly (up to 400 times per minute) in swift flight, often flying low over the ocean's surface. Etymology The English name "puffin" – puffed in the sense of swollen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tufa
Tufa is a variety of limestone formed when carbonate minerals precipitate out of water in unheated rivers or lakes. Geothermally heated hot springs sometimes produce similar (but less porous) carbonate deposits, which are known as travertine. Tufa is sometimes referred to as (meteogene) travertine. It should not be confused with hot spring (thermogene) travertine. Tufa, which is calcareous, should also not be confused with tuff, a porous volcanic rock with a similar etymology that is sometimes also called "tufa". Classification and features Modern and fossil tufa deposits abound with wetland plants; as such, many tufa deposits are characterised by their large macrobiological component, and are highly porous. Tufa forms either in fluvial channels or in lacustrine environments. Ford and Pedley (1996) provide a review of tufa systems worldwide. Fluvial deposits Deposits can be classified by their depositional environment (or otherwise by vegetation or petrographically). Pedle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoyvík
Hoyvík is a town in the Faroe Islands. It is part of the Tórshavn Municipality, and de facto is merged as a northern suburb of Tórshavn, the Faroese capital. History Hoyvík is believed to be a very old settlement. An early source is the ''Færeyinga saga'', a 13th-century recollection of earlier Viking oral recounts. Before the late 20th century the population was very low. Until the mid 19th century the entire population comprised one farm. A few more houses were built close to the farmland after the Second World War. A real development boom has been in Hoyvík since about the early 1980s. The new houses have been built on land that was formerly considered farmer outfields. The architecture of some of these newer houses include detached and terraced housing. Notable facts A 17th-century farmhouse functions today as an open-air museum, part of the National Museum of the Faroe Islands. Important institutions in Hoyvík are the gymnasium and the Faroese Historical Muse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Akraberg
Akraberg is the southern tip of Suðuroy, 5 km south from the village of Sumba, in the Faroe Islands. The name Akraberg derives from ''akur'' (cereal field). Five kilometres south of Akraberg is the southernmost point of The Faroe Islands, a rock called the Munkurin (The Monk), also called Sumbiarsteinur, which is one of a group of six rocks. This group of rocks are called Flesjarnar. The sound between Suðuroy and Munkurin is notorious for its strong current, it is called Røstin; the poet Poul F. Joensen (born 1898, died 1970) mentioned it in one of his poems "...Røstin rísin rann...". The waters south of Sumba are notorious for their unpredictability. Here lies a series of rocky skerries below and above sea level, and the meeting of currents, together with wind and weather, create dangerous conditions for boats and ships. The situation became more hazardous in 1884 when much of the high rock Munkurin on the southernmost rock, Sumbiarsteinur, crashed into the sea, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandavágur Church
Sandavágur Church is a distinctive red-roofed church in the town of Sandavágur in the Faroe Islands. History The church of Sandavá was consecrated on April 29, 1917. It was the fifth in a series of churches built in the last 300 years. A memorial was erected outside the church to one of the many ships that were sunk during the Second World War World War II or the Second World War, often abbreviated as WWII or WW2, was a world war that lasted from 1939 to 1945. It involved the vast majority of the world's countries—including all of the great powers—forming two opposi .... References External linksSandavagur at Faroeislands.dk Churches in the Faroe Islands {{faroes-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rogaland
Rogaland () is a Counties of Norway, county in Western Norway, bordering the North Sea to the west and the counties of Vestland to the north, Vestfold og Telemark to the east and Agder to the east and southeast. In 2020, it had a population of 479,892. The administrative centre of the county is the Stavanger (city), city of Stavanger, which is one of the largest cities in Norway. Rogaland is the centre of the Norwegian petroleum industry. In 2016, Rogaland had an unemployment rate of 4.9%, one of the highest in Norway. In 2015, Rogaland had a fertility rate of 1.78 children per woman, which is the highest in the country. The Diocese of Stavanger for the Church of Norway includes all of Rogaland county. Etymology ''Rogaland'' is the region's Old Norse name, which was revived in modern times. During Denmark's rule of Norway until the year 1814, the county was named ''Stavanger amt (subnational entity), amt'', after the large city of Stavanger. The first element is the plural ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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