Stord (island)
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Stord (island)
Stord is an island in Vestland county, Norway. Located in the traditional district of Sunnhordland, the island is part of the municipalities of Stord (southern part) and Fitjar (northern part). The largest settlements on the island are the town of Leirvik (granted town status in 1997) and the villages of Sagvåg and Fitjar. Geography Stord has an area of and the highest point is the tall mountain Mehammarsåto. The island lies on the northern side of the mouth of the great Hardangerfjorden. The Selbjørnsfjorden lies on the north end of the island. On the east side of the island, the Langenuen strait separates Stord from the neighboring island of Tysnesøya. On the west side of the island, the Stokksundet strait separates Stord from the neighboring island of Bømlo. There are over 350 small islands and skerries lying off the northeastern coast. Most of the central part of the island is mountainous, leaving the islands population living mostly along the coasts ...
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Fitjar (village)
is the administrative centre of Fitjar municipality in Vestland county, Norway. The village is located on the northwestern shore of the island of Stord. It sits at the southern end of the Fitjarvika bay, a small arm off the main Selbjørnsfjorden. A large group of small islands lie just off the coast to the west. Fitjar Church is located in this central part of this village. The historic Battle of Fitjar took place in this area in the year 961. The village has a population (2019) of 1,751 and a population density of . Name The village (and municipality) is named after the old ''Fitjar'' farm, since the first Fitjar Church Fitjar Church ( no, Fitjar kyrkje) is a parish church of the Church of Norway in Fitjar Municipality in Vestland county, Norway. It is located in the village of Fitjar. It is the church for the Fitjar parish which is part of the Sunnhordland pr ... was built there. The name is the plural form of ''fit'' which means "vigorous meadow". Before 1900, th ...
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Pyrite
The mineral pyrite (), or iron pyrite, also known as fool's gold, is an iron sulfide with the chemical formula Fe S2 (iron (II) disulfide). Pyrite is the most abundant sulfide mineral. Pyrite's metallic luster and pale brass-yellow hue give it a superficial resemblance to gold, hence the well-known nickname of ''fool's gold''. The color has also led to the nicknames ''brass'', ''brazzle'', and ''Brazil'', primarily used to refer to pyrite found in coal. The name ''pyrite'' is derived from the Greek (), 'stone or mineral which strikes fire', in turn from (), 'fire'. In ancient Roman times, this name was applied to several types of stone that would create sparks when struck against steel; Pliny the Elder described one of them as being brassy, almost certainly a reference to what we now call pyrite. By Georgius Agricola's time, , the term had become a generic term for all of the sulfide minerals. Pyrite is usually found associated with other sulfides or oxides in quartz v ...
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Battle Of Fitjar
The Battle of Fitjar (''Slaget ved Fitjar på Stord'') took place in 961 in Fitjar at Stord in the county of Hordaland, Norway. Battle and aftermath The Battle of Fitjar at Stord was the last battle in a war between the sons of Eric Bloodaxe and their uncle King Haakon the Good for power over Norway. It also formed part of a contest between Norway and Denmark to control the area of Oslofjord. Erling Eiriksson, Sigurd Sleva and Harald Greycloak, three of the sons of Eric Bloodaxe (''Eirikssønnene'') landed unnoticed on Hordaland in 961 and surprised the king at Fitjar. The battle was won by the forces of King Haakon, but he was wounded and eventually died. According to Snorri Sturluson, the king wanted the Norwegians to accept the sons of Eric Bloodaxe to succeed him as king and thus end the war. After Haakon's death, Harald Greycloak and his brothers became kings of Norway, but they had little authority outside western Norway. The third son of Eric Bloodaxe, Harald was the mo ...
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Håkon The Good
Haakon Haraldsson (c. 920–961), also Haakon the Good (Old Norse: ''Hákon góði'', Norwegian: ''Håkon den gode'') and Haakon Adalsteinfostre (Old Norse: ''Hákon Aðalsteinsfóstri'', Norwegian: ''Håkon Adalsteinsfostre''), was the king of Norway from 934 to 961. He was noted for his attempts to introduce Christianity into Norway. Early life Haakon is not mentioned in any narrative sources earlier than the late 12th century. According to this late saga tradition, Haakon was the youngest son of King Harald Fairhair and Thora Mosterstang. He was born on the Håkonshella peninsula in Hordaland. King Harald determined to remove his youngest son out of harm's way and accordingly sent him to the court of King Athelstan of England. Haakon was fostered by King Athelstan, as part of an agreement made by his father, for which reason Haakon was nicknamed ''Adalsteinfostre''. According to the Sagas, Athelstan was tricked into fostering Haakon when Harald's envoy used the custom of kn ...
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Harald I Hårfagre
Harald Fairhair no, Harald hårfagre Modern Icelandic: ( – ) was a Norwegian king. According to traditions current in Norway and Iceland in the eleventh and twelfth centuries, he reigned from  872 to 930 and was the first King of Norway. Supposedly, two of his sons, Eric Bloodaxe and Haakon the Good, succeeded Harald to become kings after his death. Much of Harald's biography is uncertain. A couple of praise poems by his court poet Þorbjörn Hornklofi survive in fragments, but the extant accounts of his life come from sagas set down in writing around three centuries after his lifetime. His life is described in several of the Kings' sagas, none of them older than the twelfth century. Their accounts of Harald and his life differ on many points, but it is clear that in the twelfth and thirteenth centuries Harald was regarded as having unified Norway into one kingdom. Since the nineteenth century, when Norway was in a personal union with Sweden, Harald has become a na ...
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Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end of ...
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Tilia
''Tilia'' is a genus of about 30 species of trees or bushes, native throughout most of the temperate Northern Hemisphere. The tree is known as linden for the European species, and basswood for North American species. In Britain and Ireland they are commonly called lime trees, although they are not related to the citrus lime. The genus occurs in Europe and eastern North America, but the greatest species diversity is found in Asia. Under the Cronquist classification system, this genus was placed in the family Tiliaceae, but genetic research summarised by the Angiosperm Phylogeny Group has resulted in the incorporation of this genus, and of most of the previous family, into the Malvaceae. ''Tilia'' species are mostly large, deciduous trees, reaching typically tall, with oblique-cordate (heart-shaped) leaves across. As with elms, the exact number of species is uncertain, as many of the species can hybridise readily, both in the wild and in cultivation. They are hermaphroditi ...
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Ash Trees
''Fraxinus'' (), commonly called ash, is a genus of flowering plants in the olive and lilac family, Oleaceae. It contains 45–65 species of usually medium to large trees, mostly deciduous, though a number of subtropical species are evergreen. The genus is widespread across much of Europe, Asia, and North America. The leaves are opposite (rarely in whorls of three), and mostly pinnately compound, though simple in a few species. The seeds, popularly known as "keys" or "helicopter seeds", are a type of fruit known as a samara. Some ''Fraxinus'' species are dioecious, having male and female flowers on separate plants but sex in ash is expressed as a continuum between male and female individuals, dominated by unisexual trees. With age, ash may change their sexual function from predominantly male and hermaphrodite towards femaleness ; if grown as an ornamental and both sexes are present, ashes can cause a considerable litter problem with their seeds. Rowans or mounta ...
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Oak Tree
An oak is a tree or shrub in the genus ''Quercus'' (; Latin "oak tree") of the beech family, Fagaceae. There are approximately 500 extant species of oaks. The common name "oak" also appears in the names of species in related genera, notably ''Lithocarpus'' (stone oaks), as well as in those of unrelated species such as '' Grevillea robusta'' (silky oaks) and the Casuarinaceae (she-oaks). The genus ''Quercus'' is native to the Northern Hemisphere, and includes deciduous and evergreen species extending from cool temperate to tropical latitudes in the Americas, Asia, Europe, and North Africa. North America has the largest number of oak species, with approximately 160 species in Mexico of which 109 are endemic and about 90 in the United States. The second greatest area of oak diversity is China, with approximately 100 species. Description Oaks have spirally arranged leaves, with lobate margins in many species; some have serrated leaves or entire leaves with smooth margins. M ...
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Stone Age
The Stone Age was a broad prehistoric period during which stone was widely used to make tools with an edge, a point, or a percussion surface. The period lasted for roughly 3.4 million years, and ended between 4,000 BC and 2,000 BC, with the advent of metalworking. Though some simple metalworking of malleable metals, particularly the use of gold and copper for purposes of ornamentation, was known in the Stone Age, it is the melting and smelting of copper that marks the end of the Stone Age. In Western Asia, this occurred by about 3,000 BC, when bronze became widespread. The term Bronze Age is used to describe the period that followed the Stone Age, as well as to describe cultures that had developed techniques and technologies for working copper alloys (bronze: originally copper and arsenic, later copper and tin) into tools, supplanting stone in many uses. Stone Age artifacts that have been discovered include tools used by modern humans, by their predecessor species in the ...
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Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is near ...
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Gabbro
Gabbro () is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt. Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term ''gabbro'' may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic". By rough analogy, gabbro is to basalt as granite is to rhyolite. Etymology The term "gabbro" was used in the 1760s to name a set of rock types that were found in the ophiolites of the Apennine Mountains in Italy. It was named after Gabbro, a hamlet near Rosignano Marittimo in Tuscany. Then, in 1809, the German geologist Christian Leopold von Buch used the term more restrictively in his ...
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