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Haldórsvík
Haldórsvík ( da, Haldersvig), also Haldarsvík, is a village located on the north-east coast of Streymoy in the Sunda Kommuna municipality. In the centre of the village there is a small waterfall. The stone church in the village is from 1856. It is the only octagonal church on the Faroe Islands. The altarpiece is also distinctive. It represents the Last Supper, with the Apostles' faces replaced by the faces of living public figures from the Faroe Islands. Gallery File:Haldarsvíkar Kirkja mai 2013.JPG, The octagonal church in Haldórsvík Haldarsvík, Faroe Islands (2).JPG, Haldórsvík File:Haldarsvík Faroe Islands 2013.JPG, A river and a bridge in Haldórsvík File:Haldarsvík, Faroe Islands (3).JPG, A house in Haldórsvík with turf roof File:Haldarsvík May 2013.JPG, A view of Haldórsvík,with the church at centre See also * List of towns in the Faroe Islands This is a list of villages (and towns) of the Faroe Islands. :fo:Býir í Føroyum :de:Liste d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sunda Kommuna
Sunda is a municipality in the Faroe Islands, loosely centered around the Sundini sound between the islands of Streymoy and Eysturoy. History Sunda is an amalgamation of the former municipalities of Hósvíkar, Hvalvíkar, Saksunar, Haldarsvíkar, (former) Sunda and Gjáar kommuna, which merged in 2005. The mayor as of 2020 is Heðin Zachariasen, who was also the first mayor, from 2005 to 2009. Geography The region in which Sunda kommuna is situated is referred to as Sundalagið, centered around the Sundini (''The Narrows'') between the islands of Streymoy and Eysturoy. The region also includes Eiðis kommuna, while strictly speaking Gjógv does not belong to Sundalagið, though is part of Sunda kommuna. The villages Selatrað, Morskranes and Kolbeinagjógv are also situated on the Sundini but not considered part of Sundalagið region. Sunda kommuna contains the following villages: *Hósvík *Norðskáli *Hvalvík *Streymnes *Haldórsvík *Oyri *Oyrarbakki *Tjørnuvík *Gjógv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Faroe Islands
The Faroe Islands ( ), or simply the Faroes ( fo, Føroyar ; da, Færøerne ), are a North Atlantic island group and an autonomous territory of the Kingdom of Denmark. They are located north-northwest of Scotland, and about halfway between Norway ( away) and Iceland ( away). The islands form part of the Kingdom of Denmark, along with mainland Denmark and Greenland. The islands have a total area of about with a population of 54,000 as of June 2022. The terrain is rugged, and the subpolar oceanic climate (Cfc) is windy, wet, cloudy, and cool. Temperatures for such a northerly climate are moderated by the Gulf Stream, averaging above freezing throughout the year, and hovering around in summer and 5 °C (41 °F) in winter. The northerly latitude also results in perpetual civil twilight during summer nights and very short winter days. Between 1035 and 1814, the Faroe Islands were part of the Kingdom of Norway, which was in a personal union with Denmark from 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Streymoy
Streymoy ( da, Strømø) is the largest and most populated island of the Faroe Islands. The capital, Tórshavn, is located on its southeast coast. The name means "island of currents". It also refers to the largest region of the country that also includes the islands of Hestur, Koltur and Nólsoy. Geography The island is oblong in shape and stretches roughly in northwest–southeast direction with a length of and a width of around . There are two deeply-indented fjords in the southeast: Kollafjørður and Kaldbaksfjørður. The island is mountainous (average height is 337 meter ), especially in the northwest, with the highest peak being Kopsenni (). That area is dominated by over cliffs. The area is known as Vestmannabjørgini, which means Cliffs of Vestmanna. The beaches of Tórshavn, Vestmanna, Leynar, Kollafjørður, Hvalvík (meaning Whale Bay) and Tjørnuvík are officially approved ''grind'' beaches for whaling. Like the rest of the Faroe Islands there are numerous shor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenwich Mean Time
Greenwich Mean Time (GMT) is the Local mean time, mean solar time at the Royal Observatory, Greenwich, Royal Observatory in Greenwich, London, counted from midnight. At different times in the past, it has been calculated in different ways, including being calculated from noon; as a consequence, it cannot be used to specify a particular time unless a context is given. The term 'GMT' is also used as Western European Time, one of the names for the time zone UTC+00:00 and, in UK law, is the basis for civil time in the United Kingdom. English speakers often use GMT as a synonym for Coordinated Universal Time (UTC). For navigation, it is considered equivalent to UT1 (the modern form of mean solar time at 0° longitude); but this meaning can differ from UTC by up to 0.9s. The term GMT should thus not be used for purposes that require precision. Because of Earth's uneven angular velocity in its elliptical orbit and its axial tilt, noon (12:00:00) GMT is rarely the exact moment the S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European Summer Time
Summer time in Europe is the variation of standard clock time that is applied in most European countries (apart from Iceland, Belarus, Turkey and Russia) in the period between spring and autumn, during which clocks are advanced by one hour from the time observed in the rest of the year, with a view to making the most efficient use of seasonal daylight. It corresponds to the notion and practice of daylight saving time (DST) to be found in many other parts of the world. In all locations in Europe where summer time is observed (the EU, EFTA and associated countries), European Summer Time begins at 01:00 UTC/Western European Time, WET (02:00 Central European Time, CET, 03:00 Eastern European Time, EET) on the last Sunday in March and ends at 01:00 UTC (02:00 Western European Summer Time, WEST, 03:00 Central European Summer Time, CEST, 04:00 Eastern European Summer Time, EEST) on the last Sunday in October each year; i.e. the change is made at the same absolute time across all time zone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock (geology)
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Church (building)
A church, church building or church house is a building used for Christian worship services and other Christian religious activities. The earliest identified Christian church is a house church founded between 233 and 256. From the 11th through the 14th centuries, there was a wave of church construction in Western Europe. Sometimes, the word ''church'' is used by analogy for the buildings of other religions. ''Church'' is also used to describe the Christian religious community as a whole, or a body or an assembly of Christian believers around the world. In traditional Christian architecture, the plan view of a church often forms a Christian cross; the center aisle and seating representing the vertical beam with the Church architecture#Characteristics of the early Christian church building, bema and altar forming the horizontal. Towers or domes may inspire contemplation of the heavens. Modern churches have a variety of architectural styles and layouts. Some buildings designe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Octagon
In geometry, an octagon (from the Greek ὀκτάγωνον ''oktágōnon'', "eight angles") is an eight-sided polygon or 8-gon. A '' regular octagon'' has Schläfli symbol and can also be constructed as a quasiregular truncated square, t, which alternates two types of edges. A truncated octagon, t is a hexadecagon, . A 3D analog of the octagon can be the rhombicuboctahedron with the triangular faces on it like the replaced edges, if one considers the octagon to be a truncated square. Properties of the general octagon The sum of all the internal angles of any octagon is 1080°. As with all polygons, the external angles total 360°. If squares are constructed all internally or all externally on the sides of an octagon, then the midpoints of the segments connecting the centers of opposite squares form a quadrilateral that is both equidiagonal and orthodiagonal (that is, whose diagonals are equal in length and at right angles to each other).Dao Thanh Oai (2015), "Equilatera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Altarpiece
An altarpiece is an artwork such as a painting, sculpture or relief representing a religious subject made for placing at the back of or behind the altar of a Christian church. Though most commonly used for a single work of art such as a painting or sculpture, or a set of them, the word can also be used of the whole ensemble behind an altar, otherwise known as a reredos, including what is often an elaborate frame for the central image or images. Altarpieces were one of the most important products of Christian art especially from the late Middle Ages to the era of the Counter-Reformation. Many altarpieces have been removed from their church settings, and often from their elaborate sculpted frameworks, and are displayed as more simply framed paintings in museums and elsewhere. History Origins and early development Altarpieces seem to have begun to be used during the 11th century, with the possible exception of a few earlier examples. The reasons and forces that led to the developme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Last Supper
Image:The Last Supper - Leonardo Da Vinci - High Resolution 32x16.jpg, 400px, alt=''The Last Supper'' by Leonardo da Vinci - Clickable Image, Depictions of the Last Supper in Christian art have been undertaken by artistic masters for centuries, Leonardo da Vinci's The Last Supper (Leonardo), late-1490s mural painting in Milan, Italy, being the best-known example. ''(Clickable image—use cursor to identify.)'' poly 550 2550 750 2400 1150 2300 1150 2150 1200 2075 1500 2125 1525 2300 1350 2800 1450 3000 1700 3300 1300 3475 650 3500 550 3300 450 3000 Bartholomew the Apostle, Bartholomew poly 1575 2300 1625 2150 1900 2150 1925 2500 1875 2600 1800 2750 1600 3250 1425 3100 1400 2800 1375 2600 James, son of Alphaeus, James Minor poly 1960 2150 2200 2150 2350 2500 2450 2575 2375 2725 2375 2900 2225 3100 2225 3225 1600 3225 1825 2700 1975 2450 1925 2300 Saint Andrew, Andrew poly 2450 2575 2775 2500 2700 2650 2800 2700 2600 3000 2600 3250 2300 3250 2200 3200 2300 3000 Saint Peter, Peter p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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