1.
Tinganes
–
Tinganes is the historic location of the Faroese landsstýri, and is a part of Tórshavn. The name means parliament jetty or parliament point in Faroese, the parliament met there for the first time in the Viking ages when Norwegian colonists placed their Ting on the location in 825. It is one of the oldest parliamentary meeting places in the world, along with Tynwald hill in the Isle of Man, the Løgting has since moved to the north of the city, but the home-rule government still sits here. The building on the outermost point on the small peninsula Skansapakkhusið, the small main street on the peninsula is called Gongin and is home to the oldest parts of the city. Many of the houses on Tinganes were built in the 16th and 17th centuries and are still in use today, the peninsula divides the Tórshavn harbour in two parts, Eystaravág and Vesteravág
Tinganes
–
Tinganes showing government buildings
2.
Faroe Islands
–
The Faroe Islands, also spelled the Faeroes, is an archipelago between the Norwegian Sea and the North Atlantic, about halfway between Norway and Iceland,320 kilometres north-northwest of Scotland. Its area is about 1,400 square kilometres with a population of 49,188 in 2016, the Faeroe Islands is an autonomous country within the Danish Realm. The land of the Faeroes is rugged, and these islands have an oceanic climate, windy, wet, cloudy. Despite this island groups northerly latitude, temperatures average above freezing throughout the year because of the Gulf Stream, between 1035 and 1814, the Faeroes were part of the Hereditary Kingdom of Norway. In 1814, the Treaty of Kiel granted Denmark control over the islands, the Faroe Islands have been a self-governing country within the Kingdom of Denmark since 1948. The Faroese have control of most domestic matters, areas that remain the responsibility of Denmark include military defence, the police department, the justice department, currency, and foreign affairs. However, as they are not part of the customs area as Denmark, the Faroe Islands have an independent trade policy. The islands also have representation in the Nordic Council as members of the Danish delegation, the people of the Faroe Islands also compete as national team in certain sports. In Danish, the name Færøerne may reflect an Old Norse word fær, the morpheme øerne represents a plural of ø in Danish. The Danish name thus translates as the islands of sheep, in Faroese, the name appears as Føroyar. Oyar represents the plural of oy, older Faroese for island, the modern Faeroese word for island is oyggj. In the English language, their name is sometimes spelled Faeroe, archaeological evidence shows settlers living on the Faroe Islands in two successive periods prior to the arrival of the Norse, the first between 400 and 600 and the second between 600 and 800. Scientists from the University of Aberdeen have also found early cereal pollen from domesticated plants, archaeologist Mike Church noted that Dicuil mentioned what may have been the Faroes. He also suggested that the living there might have been from Ireland, Scotland or Scandinavia. A Latin account of a made by Brendan, an Irish monastic saint who lived around 484–578. This association, however, is far from conclusive in its description, Dicuil, an Irish monk of the early 9th century, wrote a more definite account. 800, bringing Old West Norse, which evolved into the modern Faroese language, according to Icelandic sagas such as Færeyjar Saga, one of the best known men in the island was Tróndur í Gøtu, a descendant of Scandinavian chiefs who had settled in Dublin, Ireland. Tróndur led the battle against Sigmund Brestursson, the Norwegian monarchy, a traditional name for the islands in Irish, Na Scigirí, possibly refers to the Skeggjar Beards, a nickname given to island dwellers
Faroe Islands
–
Tinganes in
Tórshavn, seat of a part of the Faroese government.
Faroe Islands
–
Flag
Faroe Islands
–
Queen
Margrethe II, monarch of the
Unity of the Realm, during a visit to
Vágur in 2005.
Faroe Islands
–
NASA satellite image of the Faroe Islands.
3.
Geographic coordinate system
–
A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
Geographic coordinate system
–
Longitude lines are perpendicular and latitude lines are parallel to the equator.
4.
Kingdom of Denmark
–
The term Danish Realm refers to the relationship between Denmark proper, the Faroe Islands and Greenland—three countries constituting the Kingdom of Denmark. The legal nature of the Kingdom of Denmark is fundamentally one of a sovereign state. The Faroe Islands and Greenland have been part of the Crown of Denmark since 1397 when the Kalmar Union was ratified, legal matters in The Danish Realm are subject to the Danish Constitution. Beginning in 1953, state law issues within The Danish Realm has been governed by The Unity of the Realm, a less formal name for The Unity of the Realm is the Commonwealth of the Realm. In 1978, The Unity of The Realm was for the first time referred to as rigsfællesskabet. The name caught on and since the 1990s, both The Unity of The Realm and The Danish Realm itself has increasingly been referred to as simply rigsfællesskabet in daily parlance. The Danish Constitution stipulates that the foreign and security interests for all parts of the Danish Realm are the responsibility of the Danish government, the Faroes received home rule in 1948 and Greenland did so in 1979. In 2005, the Faroes received a self-government arrangement, and in 2009 Greenland received self rule, the Danish Realms unique state of internal affairs is acted out in the principle of The Unity of the Realm. This principle is derived from Article 1 of the Danish Constitution which specifies that constitutional law applies equally to all areas of the Danish Realm, the Constitutional Act specifies that sovereignty is to continue to be exclusively with the authorities of the Realm. The language of Denmark is Danish, and the Danish state authorities are based in Denmark, the Kingdom of Denmarks parliament, with its 179 members, is located in the capital, Copenhagen. Two of the members are elected in each of Greenland and the Faroe Islands. The Government ministries are located in Copenhagen, as is the highest court, in principle, the Danish Realm constitutes a unified sovereign state, with equal status between its constituent parts. Devolution differs from federalism in that the powers of the subnational authority ultimately reside in central government. The Self-Government Arrangements devolves political competence and responsibility from the Danish political authorities to the Faroese, the Faroese and Greenlandic authorities administer the tasks taken over from the state, enact legislation in these specific fields and have the economic responsibility for solving these tasks. The Danish government provides a grant to the Faroese and the Greenlandic authorities to cover the costs of these devolved areas. The 1948 Home Rule Act of the Faroe Islands sets out the terms of Faroese home rule, the Act states. the Faroe Islands shall constitute a self-governing community within the State of Denmark. It establishes the government of the Faroe Islands and the Faroese parliament. The Faroe Islands were previously administered as a Danish county, the Home Rule Act abolished the post of Amtmand and these powers were expanded in a 2005 Act, which named the Faroese home government as an equal partner with the Danish government
Kingdom of Denmark
–
The gilded side of the
Trundholm sun chariot dating from the Nordic Bronze Age.
Kingdom of Denmark
–
Flag
Kingdom of Denmark
–
The
Ladby ship, the largest ship burial found in Denmark.
Kingdom of Denmark
–
Larger of the two Jelling stones, raised by
Harald Bluetooth.
5.
Annika Olsen
–
Annika Olsen and is a Faroese politician, high school teacher and former swimmer. She was Deputy Prime Minister and Minister of Social Affairs in the Faroe Islands, before that she was a member of the City Council of Tórshavn from 2004 to 2008. Annika Olsen has an MA in Nordic languages and literature with a subject in religion. She is the daughter of Jákup Olsen, a businessman, former politician and former headmaster of Vágurs School and Marna Olsen, born Holm, a retired teacher. At the general election 2015, the Peoples Party lost two seats in the Faroese parliament, they got 18. 9% of the votes and 6 members, Annika Olsen got second most votes of the parties candidates. Eight days after the election, Olsen who had received 961 personal votes, left the Peoples Party, on 17 September she joined the Liberal party Progress, which is part of the governing coalition. She was subsequently elected as chairman of the Fiscal committee, three days later, she regret her decision and left Progress and also said she would not be the chairman of the Fiscal committee. She needed some time alone with her family and took leave from the parliament and she asked the people who elected her to forgive her, she had had too little time to think before she joined another party. On 4 February 2016 she became a member of the Peoples Party again, between 1988 and 1995 Annika Olsen was a member of the Faroese national swimming team. She attended the Island Games in 1991 and won a medal in 200 m breast, bronze in 4x50 m free, bronze in 4x100 m free. She also attended the Island Games 1989 in the Faroe Islands
Annika Olsen
–
Annika Olsen
6.
Metropolitan area
–
As social, economic and political institutions have changed, metropolitan areas have become key economic and political regions. The Greater São Paulo is a term for one of the multiple definitions the large metropolitan area located in the São Paulo state in Brazil. A metropolitan area combines an urban agglomeration with zones not necessarily urban in character and these outlying zones are sometimes known as a commuter belt, and may extend well beyond the urban zone, to other political entities. For example, El Monte, California is considered part of the Los Angeles metro area in the United States, in practice, the parameters of metropolitan areas, in both official and unofficial usage, are not consistent. Population figures given for one area can vary by millions. A polycentric metropolitan area is one not connected by continuous development or conurbation, in defining a metropolitan area, it is sufficient that a city or cities form a nucleus that other areas have a high degree of integration with. The Australian Bureau of Statistics defines statistical divisions as areas under the influence of one or more major towns or a major city. However, this definition has become obsolete with the conurbation of several statistical divisions into a larger metropolitan areas. In Brazil, metropolitan areas are called metropolitan regions, each State defines its own legislation for the creation, definition and organization of a metropolitan region. The creation of a region is not intended for any statistical purpose, although the Brazilian Institute of Geography. Their main purpose is to allow for a management of public policies of common interest to all cities involved. They dont have political, electoral or jurisdictional power whatsoever, so living in a metropolitan region do not elect representatives for them. Statistics Canada defines a metropolitan area as an area consisting of one or more adjacent municipalities situated around a major urban core. To form a CMA, the area must have a population of at least 100,000. To be included in the CMA, adjacent municipalities must have a degree of integration with the core. As of the Canada 2011 Census, there were 33 CMAs in Canada, including six with a population over one million—Toronto, Montreal, Vancouver, Ottawa, Calgary and Edmonton. In Denmark the only area is Greater Copenhagen, consisting of the Capital Region of Denmark along with the neighboring regions Region Zealand. Greater Copenhagen has an population of 1.25 million people
Metropolitan area
–
Greater Buenos Aires,
Argentina
Metropolitan area
–
Paris (
France), one of Europe's major centres
Metropolitan area
–
Tel Aviv Metropolitan Area,
Israel
Metropolitan area
–
Perth, Western Australia, an isolated metropolitan area
7.
Oceanic climate
–
Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, and above 0 °C in the coldest month. It typically lacks a dry season, as precipitation is evenly dispersed throughout the year. Oceanic climates generally have cool summers and mild to cool winters, Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies, many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. Precipitation is both adequate and reliable throughout the year in oceanic climates, extended months of rain and cloudy conditions are common in oceanic climates. Seattle is an example of this, between October and May, Seattle experiences high rainfall and is mostly or partly cloudy six out of every seven days. In most areas with a 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, outside of Australia and parts of New Zealand, most areas with an oceanic climate experience at least one snowstorm per year. In the poleward locations of the climate zone, snowfall is more frequent. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature, summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the subpolar oceanic climate, with long and cold winters and cool. Examples of this climate include parts of coastal Iceland in the Northern Hemisphere and extreme southern Chile, Oceanic climates are not necessarily always found in coastal locations on the aforementioned parallels, however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream, which moves in a west to east direction across the middle latitudes, advancing low pressure systems, storms, in coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the adjacent to them. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Oceanic climates in Europe occur mostly in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, Germany, Norway, the north coast of Spain, examples of oceanic climates are found in London, Bergen, Dublin, Berlin, Bilbao, Donostia-San Sebastian, Biarritz, Bayonne, Zürich, Copenhagen and Paris. With decreasing distance to the Mediterranean Sea, the climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe
Oceanic climate
–
Seattle, a city with an oceanic climate
Oceanic climate
–
World map showing oceanic climate zones, as defined by the
Köppen climate types "Cfb", "Cfc", "Cwb" and "Cwc"
Oceanic climate
–
Curitiba, capital city of Brazilian
Paraná state features a subtropical highland climate
8.
Danish language
–
There are also minor Danish-speaking communities in Norway, Sweden, Spain, the United States, Canada, Brazil and Argentina. Due to immigration and language shift in urban areas, around 15–20% of the population of Greenland speak Danish as their home language. Along with the other North Germanic languages, Danish is a descendant of Old Norse, until the 16th century, Danish was a continuum of dialects spoken from Schleswig to Scania with no standard variety or spelling conventions. With the Protestant Reformation and the introduction of printing, a language was developed which was based on the educated Copenhagen dialect. It spread through use in the system and administration though German. Today, traditional Danish dialects have all but disappeared, though there are variants of the standard language. The main differences in language are between generations, with youth language being particularly innovative, Danish has a very large vowel inventory comprising 27 phonemically distinctive vowels, and its prosody is characterized by the distinctive phenomenon stød, a kind of laryngeal phonation type. The grammar is moderately inflective with strong and weak conjugations and inflections, nouns and demonstrative pronouns distinguish common and neutral gender. As in English, Danish only has remnants of a case system, particularly in the pronouns. Its syntax is V2, with the verb always occupying the second slot in the sentence. Danish is a Germanic language of the North Germanic branch, other names for this group are the Nordic or Scandinavian languages. Along with Swedish, Danish descends from the Eastern dialects of the Old Norse language, Scandinavian languages are often considered a dialect continuum, where there are no sharp dividing lines between the different vernacular languages. Like Norwegian and Swedish, Danish was significantly influenced by Low German in the Middle Ages, Danish itself can be divided into three main dialect areas, West Danish, Insular Danish, and East Danish. Danish is largely mutually intelligible with Norwegian and Swedish, both Swedes and Danes also understand Norwegian better than they understand each others languages. By the 8th century, the common Germanic language of Scandinavia, Proto-Norse, had some changes. This language was called the Danish tongue, or Norse language. Norse was written in the alphabet, first with the elder futhark. From the 7th century the common Norse language began to undergo changes that did not spread to all of Scandinavia, most of the changes separating East Norse from West Norse started as innovations in Denmark, that spread through Scania into Sweden and by maritime contact to southern Norway
Danish language
–
The first page of the Jutlandic Law originally from 1241 in Codex Holmiensis, copied in 1350. The first sentence is: " Mædh logh skal land byggas " "With law the land shall be built".
Danish language
–
Learn Danish banner in
Flensburg,
Germany where it is an officially recognized
regional language
Danish language
–
Danish label reading militærpoliti, "military police", on police vehicle
Danish language
–
Danish keyboard with keys for Æ, Ø, and Å.
9.
Capital (political)
–
A capital city is the municipality exercising primary status in a country, state, province, or other region, usually as its seat of government. A capital is typically a city that encompasses the offices and meeting places of its respective government. In some jurisdictions, including countries, the different branches of government are located in different settlements. In some cases, a distinction is made between the capital and the seat of government, which is in another place. The word capital derives from the Latin caput, meaning head, in several English-speaking states, the terms county town, county seat, and borough seat are also used in lower subdivisions. In unitary states, subnational capitals are known as administrative centres. The capital is often, but not necessarily, the largest city of its constituent, historically, the major economic centre of a state or region often becomes the focal point of political power, and becomes a capital through conquest or federation. Examples are Ancient Babylon, Abbasid Baghdad, Ancient Athens, Rome, Constantinople, Changan, Ancient Cusco, Madrid, Paris, London, Moscow, Beijing, Tokyo, Vienna, and Berlin. Some of these cities are or were also religious centres, e. g. Constantinople, Rome, Jerusalem, Ancient Babylon, Moscow, Belgrade, Paris, and Peking. A capital city that is also the economic, cultural. The convergence of political and economic or cultural power is by no means universal, traditional capitals may be economically eclipsed by provincial rivals, e. g. Nanking by Shanghai, Quebec City by Montreal, and numerous US state capitals. The decline of a dynasty or culture could also mean the extinction of its city, as occurred at Babylon. Although many capitals are defined by constitution or legislation, many long-time capitals have no legal designation as such, for example Bern, Edinburgh, Lisbon, London, Paris, are located in or near them. In Canada, there is a capital, while the ten provinces. The states of such countries as Mexico, Brazil, and Australia all have capital cities, for example, the six state capitals of Australia are Adelaide, Brisbane, Hobart, Melbourne, Perth, and Sydney. In Australia, the capital cities is regularly used, to refer to the aforementioned state capitals plus the federal capital Canberra and Darwin. Abu Dhabi is the city of the Emirate of Abu Dhabi. In unitary states which consist of multiple constituent countries, such as the United Kingdom or the Kingdom of Denmark, the national capitals of Germany and Russia, the Stadtstaat of Berlin and the Federal City of Moscow, are also constituent states of both countries in their own right
Capital (political)
–
Parliament Hill, the national legislative buildings, in
Ottawa, the capital of
Canada.
Capital (political)
–
The
Roman Forum was surrounded by many government buildings as the capital of
Ancient Rome.
Capital (political)
–
The
Western Wall is one of the greatest findings of the Jewish history in
Jerusalem.
Capital (political)
–
Cornwall Council headquarters in the
county town of
Truro.
10.
Streymoy
–
Streymoy is the largest and most populated island of the Faroe Islands. The capital, Tórshavn, is located on its east coast, the name means island of currents. It also refers to the largest region of the country also includes the islands of Hestur, Koltur. The island is oblong in shape and stretches roughly in northwest-southeast direction with a length of 47 kilometres, there are two deeply indented fjords in the southeast, Kollafjørður and Kaldbaksfjørður. The island is mountainous, especially in the northwest, with the highest peak Kopsenni and that area is dominated by over 500-metre-high cliffs. The area is known as Vestmannabjørgini, which means Cliffs of Vestmanna, like the rest of the Faroe Islands there are numerous short streams and minor lakes. The main vegetation is grass, with no trees, some of the villages have planted trees inside or just outside the village. These parks need to have fence around them in order to keep sheep out, Streymoy is separated from the nearby Eysturoy, second largest island of the Faroe Islands by the narrow sound of Sundini in the east. To the west lies the island of Vágar, and to the south the island of Sandoy, three additional smaller islands are situated around the southern tip of Streymoy, Koltur, Hestur and Nólsoy. There are about 22,400 inhabitants on the island, which more than 40% of the whole population of the Faroe Islands. Around 1,200 people live in Vestmanna,800 in Kollafjørður, besides being the seat of the government Tórshavn is also the chief port, seat of the university and the commercial centre of the islands. The other important towns include, Vestmanna, the ferry port in the west, Kollafjørður at the centre. From a historic point of view the village of Kirkjubøur near the tip of the island is very important as it was an episcopal center during the Middle Ages. All the settlements are connected by surfaced roads, the main entry road to Tórshavn passes through a 2.8 kilometres long tunnel. The connection to the island Eysturoy is via a bridge over the Sundini sound, since 2002, the almost 5 kilometres long Vágar Tunnel connects Streymoy to Vágar thereby completing the road connections of the three mainland islands. Streymoy is connected by ferry service to the island of Sandoy from the ferry port on Gamla Rætt near Kirkjubøur. In summertime, scheduled ferry connects Tórshavn with Hanstholm in Denmark and Seyðisfjörður in Iceland, the closest airport is on Vágar island, it is the only airport in the Faroe Islands. Media related to Streymoy at Wikimedia Commons The dictionary definition of Streymoy at Wiktionary Tórshavn and Streymoy Tourist Information
Streymoy
–
Skælingur (767 m) on Streymoy
Streymoy
–
Map of Streymoy
Streymoy
–
The Streymin bridge over Sundini Sound connects Eysturoy (this side) to Streymoy (distant side).
Streymoy
–
The capital Tórshavn is on Streymoy.
11.
Urban area
–
An urban area is a human settlement with high population density and infrastructure of built environment. Urban areas are created through urbanization and are categorized by urban morphology as cities, in urbanism, the term contrasts to rural areas such as villages and hamlets and in urban sociology or urban anthropology it contrasts with natural environment. The worlds urban population in 1950 of just 746 million has increased to 3.9 billion in the decades since, in 2009, the number of people living in urban areas surpassed the number living in rural areas and since then the world has become more urban than rural. This was the first time that the majority of the population lived in a city. In 2014 there were 7.25 billion people living on the planet, Urban areas are created and further developed by the process of urbanization. Urban areas are measured for various purposes, including analyzing population density, historian John Gurda writes, I have tried to uncover Milwaukees civic bedrock - the shifting foundation on which individuals have built their lives and the community has constructed its identity. There is no doubt that the deepest layer of bedrock is economic. In every age, people have chosen to live in areas not because of their climates or landmarks or cultural attractions. It was economic opportunity that brought people to Milwaukee, and it is economic opportunity that keeps them there, I define cities as concentrations of people animated by concentrations of capital. More simply put, money is the root of all cities, official definitions vary somewhat between nations. The ten largest metropolitan areas account for half of the population, about 3 million people live in Buenos Aires City and the Greater Buenos Aires metropolitan area totals around 13 million, making it one of the largest urban areas in the world. The metropolitan areas of Córdoba, Rosario, Mendoza and Tucumán have around 1.3 million inhabitants each and La Plata, seven other provinces have over one million people each, Mendoza, Tucumán, Entre Ríos, Salta, Chaco, Corrientes and Misiones. According to IBGE urban areas already concentrate 84. 35% of the population, while the Southeast region remains the most populated one, with over 80 million inhabitants. The largest metropolitan areas in Brazil are São Paulo, Rio de Janeiro, and Belo Horizonte — all in the Southeastern Region — with 20,12, and 5 million inhabitants respectively. The majority of state capitals are the largest cities in their states, except for Vitória, the capital of Espírito Santo, and Florianópolis, there are also non-capital metropolitan areas in the states of São Paulo, Minas Gerais, Rio Grande do Sul and Santa Catarina. According to Statistics Canada, an area in Canada is an area with a population of at least 1,000 people where the density is no fewer than 400 persons per square kilometre. If two or more areas are within 2 km of each other by road, they are merged into a single urban area. Accordingly, the new definition set out three types of population centres, small, medium and large
Urban area
–
Greater Tokyo Area, the world's most populous urban area, with about 35 million people.
Urban area
–
Buenos Aires Córdoba
Urban area
Urban area
–
Rosario Mendoza
12.
Middle Ages
–
In the history of Europe, the Middle Ages or Medieval Period lasted from the 5th to the 15th century. It began with the fall of the Western Roman Empire and merged into the Renaissance, 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 subdivided into the Early, High. Population decline, counterurbanisation, invasion, and movement of peoples, 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 seventh century, North Africa and the Middle East—once part of the Byzantine Empire—came under the rule of the Umayyad Caliphate, although there were substantial changes in society and political structures, the break with classical antiquity was not complete. The still-sizeable Byzantine Empire survived in the east and remained a major power, the empires law code, the Corpus Juris Civilis or Code of Justinian, was rediscovered in Northern Italy in 1070 and became widely admired later in the Middle Ages. In the West, most kingdoms incorporated the few extant Roman institutions, monasteries were founded as campaigns to Christianise pagan Europe continued. The Franks, under the Carolingian dynasty, briefly established the Carolingian Empire during the later 8th, the Crusades, first preached in 1095, were military attempts by Western European Christians to regain control of the Holy Land from Muslims. Kings became the heads of centralised nation states, reducing crime and violence, intellectual life was marked by scholasticism, a philosophy that emphasised joining faith to reason, and by the founding of universities. Controversy, heresy, and the Western Schism within the Catholic Church paralleled the conflict, civil strife. Cultural and technological developments transformed European society, concluding the Late Middle Ages, the Middle Ages is one of the three major periods in the most enduring scheme for analysing European history, classical civilisation, or Antiquity, the Middle Ages, and the Modern Period. Medieval writers divided history into periods such as the Six Ages or the Four Empires, when referring to their own times, they spoke of them as being modern. In the 1330s, the humanist and poet Petrarch referred to pre-Christian times as antiqua, leonardo Bruni was the first historian to use tripartite periodisation in his History of the Florentine People. Bruni and later argued that Italy had recovered since Petrarchs time. The Middle Ages first appears in Latin in 1469 as media tempestas or middle season, in early usage, there were many variants, including medium aevum, or middle age, first recorded in 1604, and media saecula, or middle ages, first recorded in 1625. The alternative term medieval derives from medium aevum, tripartite periodisation became standard after the German 17th-century historian Christoph Cellarius divided history into three periods, Ancient, Medieval, and Modern. The most commonly given starting point for the Middle Ages is 476, for Europe as a whole,1500 is often considered to be the end of the Middle Ages, but there is no universally agreed upon end date. English historians often use the Battle of Bosworth Field in 1485 to mark the end of the period
Middle Ages
–
The
Cross of Mathilde, a
crux gemmata made for
Mathilde, Abbess of Essen (973–1011), who is shown kneeling before the Virgin and Child in the
enamel plaque. The body of Christ is slightly later. Probably made in
Cologne or
Essen, the cross demonstrates several medieval techniques:
cast figurative sculpture,
filigree, enamelling, gem polishing and setting, and the reuse of Classical
cameos and
engraved gems.
Middle Ages
–
A late Roman statue
depicting the four Tetrarchs, now in
Venice
Middle Ages
–
Coin of
Theodoric
Middle Ages
–
Mosaic showing
Justinian with
the bishop of
Ravenna, bodyguards, and courtiers
13.
History of the Faroe Islands
–
The early details of the Faroe Islands are often unclear. It is possible that Brendan, an Irish monk, sailed past the islands during his North Atlantic voyage in the 6th century and he saw an Island of Sheep and a Paradise of Birds, which some say could be the Faroes with its dense bird population and sheep. Norsemen settled the Faroe Islands in the 9th century or 10th century, the islands were officially converted to Christianity around the year 1000, and became a part of the Kingdom of Norway in 1035. Norwegian rule on the islands continued until 1380, when the became part of the dual Denmark–Norway kingdom. Following the 1814 Treaty of Kiel that ended the dual Denmark–Norway kingdom, during World War II, after Denmark was occupied by Nazi Germany, the British invaded and occupied the Faroe Islands until shortly after the end of the war. Scientists from Aberdeen University have also found early cereal pollen from domesticated plants, archaeologist Mike Church noted that Dicuil mentioned what may have been the Faroes. He also suggested that the living there might have been from Ireland, Scotland or Scandinavia. There is a Latin account of a made by Saint Brendan. This association, however, is far from conclusive in its description, many other islands lie in the northerly British Ocean. One reaches them from the islands of Britain, by sailing directly for two days and two nights with a full sail in a favourable wind the whole time. Most of these islands are small, they are separated by narrow channels, Norse settlement of the Faroe Islands is recorded in the Færeyinga saga, whose original manuscript is lost. Portions of the tale were inscribed in three other sagas, such as Flateyjarbók, Saga of Óláfr Tryggvason, and AM62 fol, similar to other sagas, the historical credibility of the Færeyinga saga is highly 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 Harald Hårfagre, between 872–930 CE. The Saga of Óláfr Tryggvason indicates that Kamban was residing in the Faroes long before the rule of Harald Hårfagre, and this mass migration to the Faroe Islands shows a prior knowledge of the Viking settlements locations, furthering the claim of Grímur Kambans settlement much earlier. While Kamban is recognized as the first Viking settler of the Faroe Islands, writings from the Papar, an order of Irish monks, show that they left the Faroe Islands due to ongoing Viking raids. The name of the islands is first recorded on the Hereford map, the name has long been understood as based on Old Norse fár livestock, thus fær-øer sheep islands. The main historical source for this period is the 13th century work Færeyinga saga, Færeyinga saga only exists today as copies in other sagas, in particular the manuscripts called Saga of Óláfr Tryggvason, Flateyjarbók and one registered as AM62 fol
History of the Faroe Islands
–
Faroese stamp depicting Saint Brendan discovering the Faroe Islands
History of the Faroe Islands
–
Faroese stamp depicting
Tróndur í Gøtu raising
the hammer of Thor against Christianity
14.
Thing (assembly)
–
A thing was the governing assembly of a Northern Germanic society, made up of the free people of the community presided over by lawspeakers. Its meeting-place was called a thingstead, the Anglo-Saxon folkmoot or folkmote was analogous, the forerunner to the witenagemot and a precursor of the modern Parliament of the United Kingdom. The Old Norse, Old Frisian, and Old English þing with the assembly is identical in origin to the English word thing, German Ding, Dutch ding. All of these derive from Proto-Germanic *þingą meaning appointed time. The word shift in the meaning of the thing from assembly to object is mirrored in the evolution of the Latin causa to modern French chose, Spanish/Italian/Catalan cosa. In English the term is attested from 685 to 686 CE in the meaning assembly, later it referred to a being, entity or matter. The early sense of meeting, assembly did not survive the shift to Middle English, the meaning of personal possessions, commonly in the plural, first appears in Middle English around 1300. In the pre-Christian clan-culture of Scandinavia the members of a clan were obliged to avenge injuries against their dead, a balancing structure was necessary to reduce tribal feuds and avoid social disorder. It is known from North-Germanic cultures that the institution was the thing, although similar assemblies are reported also from other Germanic peoples. The thing was the assembly of the men and women of a country. There were consequently hierarchies of things, so that the things were represented at the higher-level thing. At the thing, disputes were solved and political decisions were made, the place for the thing was often also the place for public religious rites and for commerce. The thing met at regular intervals, legislated, elected chieftains and kings, and judged according to the law, the things negotiations were presided over by the lawspeaker and the chieftain or the king. In reality the thing was dominated by the most influential members of the community, the heads of clans and wealthy families, Haugating, the Thing for Vestfold in Norway, was located in Tønsberg at Haugar. This site was one of Norways most important places for the proclamation of kings, in 1130, Harald Gille called together a meeting at the Haugating at which he was declared to be King of Norway. Sigurd Magnusson was proclaimed king in 1193 at Haugating, magnus VII was acclaimed hereditary King of Norway and Sweden at the Haugating in August 1319. Main things in Sweden were the Thing of all Swedes, the Thing of all Geats, the island of Gotland had twenty things in late medieval times, each represented at the island-thing called landsting by its elected judge. New laws were decided at the landsting, which also took other decisions regarding the island as a whole, the landstings authority was successively eroded after the island was occupied by the Teutonic Order in 1398
Thing (assembly)
–
Germanic thing, drawn after the depiction in a relief of the
Column of Marcus Aurelius (AD 193)
Thing (assembly)
–
The Icelandic
Althing in session, as imagined in the 1890s by British artist
W. G. Collingwood.
Thing (assembly)
–
Þorgnýr the Lawspeaker showing the power of his office to the King of Sweden at
Gamla Uppsala, 1018. The lawspeaker forced King
Olof Skötkonung not only to accept peace with his enemy, King
Olaf the Stout of Norway, but also to give his daughter to him in marriage. Illustration by C. Krogh.
15.
Peninsula
–
A peninsula is a piece of land surrounded by water on the majority of its border, while being connected to a mainland from which it extends out. Examples include the upper and lower peninsulas of the state of Michigan, the surrounding water is usually understood to be continuous, though not necessarily named as a single body of water. Peninsulas are not always named as such, one can also be a headland, cape, island promontory, bill, point, a point is generally considered a tapering piece of land projecting into a body of water that is less prominent than a cape. A river which courses through a very tight meander is also said to form a peninsula within the loop of water. In English, the plural of peninsula is peninsulas or, less commonly, peninsulas can be found on coastlines and in smaller bodies of water throughout the world, ranging in scale from square meters to millions of square kilometers. Theres the Scandinavian Peninsula in Northern Europe, and in Southern Europe theres the Iberian Peninsula, the Italian Peninsula, south America has the Brunswick Peninsula, and Antarctica has the Antarctic Peninsula. In Africa, theres the Horn of Africa, and in Australia, asia has the 3 largest peninsulas in the world, the Arabian Peninsula, the Indian Peninsula, and the Indochinese Peninsula
Peninsula
–
The world's largest peninsula, the
Arabian Peninsula
Peninsula
–
Baja California Peninsula,
Mexico
Peninsula
–
A beach on the Mornington Peninsula
Peninsula
–
NASA satellite photo of
Otago Peninsula and
Otago Harbour. The city of
Dunedin is located at the
isthmus at lower left.
16.
Bergen
–
Bergen, historically Bjørgvin, is a city and municipality in Hordaland on the west coast of Norway. At the end of the first quarter of 2016, the population was 278,121. Bergen is the second-largest city in Norway, the municipality covers 465 square kilometres and is on the peninsula of Bergenshalvøyen. The city centre and northern neighbourhoods are on Byfjorden, the city fjord, many of the extra-municipal suburbs are on islands. Bergen is the centre of Hordaland and consists of eight boroughs—Arna, Bergenhus, Fana, Fyllingsdalen, Laksevåg, Ytrebygda, Årstad. Trading in Bergen may have started as early as the 1020s, according to tradition, the city was founded in 1070 by king Olav Kyrre, its name was Bjørgvin, the green meadow among the mountains. It served as Norways capital in the 13th century, and from the end of the 13th century became a city of the Hanseatic League. Until 1789, Bergen enjoyed exclusive rights to trade between Northern Norway and abroad and it was the largest city in Norway until the 1830s when it was surpassed by the capital. What remains of the quays, Bryggen, is a World Heritage Site, the city was hit by numerous fires over the years. The Bergen School of Meteorology was developed at the Geophysical Institute beginning in 1917, the Norwegian School of Economics was founded in 1936, from 1831 to 1972, Bergen was its own county. In 1972 the municipality absorbed four surrounding municipalities and became a part of Hordaland county, the city is an international centre for aquaculture, shipping, offshore petroleum industry and subsea technology, and a national centre for higher education, media, tourism and finance. Bergen Port is Norways busiest in both freight and passengers with over 300 cruise ship calls a year bringing nearly a half a million passengers to Bergen, almost half of the passengers are German or British. The citys main team is SK Brann and the citys unique tradition is the buekorps. Natives speak the distinct Bergensk dialect, the city features Bergen Airport, Flesland, Bergen Light Rail, and is the terminus of the Bergen Line. Four large bridges connect Bergen to its suburban municipalities, Bergen is well known for having a mild winter climate, though with a lot of precipitation. In December - March, the difference between Bergen and Oslo can be up to 30 degrees Celsius, despite the fact that both cities are at approximately 60 degrees North. The Gulf Stream keeps the sea relatively warm, considering the latitude, the city of Bergen was traditionally thought to have been founded by king Olav Kyrre, son of Harald Hardråde in 1070 AD, four years after the Viking Age ended with the Battle of Hastings. Modern research has, however, discovered that a settlement was established already during the 1020s or 1030s
Bergen
–
From top to bottom: city centre, old town,
Gamlehaugen, city square and
Bryggen
Bergen
–
Hieronymus Scholeus 's rendering of Bergen from around 1580. Published in
Civitates orbis terrarum.
Bergen
–
A
photochrom of Bergen near the end of the 19th century. Visible are
Domkirken in the bottom left side,
Korskirken in the middle, the bay (
Vågen) with its many boats and the
Bergenhus Fortress to the right of the mouth of the bay.
Bergen
–
Bergen: Urban areas (
Statistics Norway)
17.
Skansin
–
Skansin is a historic fortress in Tórshavn, the capital of the Faroe Islands. Skansin is located on a hill beside the port of Tórshavn, the fort was built in 1580 by Magnus Heinason to protect against pirate raids of the town, after he himself was nearly caught up in one such raid. The fort was expanded considerably in 1780 and went through a series of rebuilds for many years afterwards, during the Second World War the fort served Britain as a military base. Two 5.5 inch guns date from the British occupation, one of the Faroese lighthouses, the Skansin Lighthouse, towers over the fortress, pointing the way to the capital. The strategic location of the fort offers picturesque views of Tórshavn port, surrounding landscape. British occupation of the Faroe Islands - Forts of the Faroe Islands Faroeislands. dk - Foto
Skansin
–
Skansin lighthouse is visible in the background. In the foreground is a British gun from the warship
HMS Furious.
18.
Magnus Heinason
–
Magnus Heinason was a Faroese naval hero, trader and privateer. Magnus Heinason served William the Silent and his son Maurice of Nassau, Prince of Orange for 10 years as a privateer, Magnus Heinason was given the trading rights to the Faroe Islands by Frederick II of Denmark and Norway from 1559 to 1588. Later he received letters of marque to sink or capture pirate ships, Magnus built the first fortifications in Tórshavn. Only one year later, he was captured and sent to Copenhagen on the orders of the Danish treasurer and statholder, Christofer Walkendorf who was ruling Denmark after the death of Frederick II. Magnus Heinason was tried, and was beheaded 18th and his widow, Sofie von Günsterberg, and his good friend Johannes Lindenov contested this act and brought the matter to the Herrendag in Kolding. Magnus Heinasons death sentence was declared void, the 6th of August 1590, Valkendorff was suspended from his duties and was forced to pay 3,000 Reichsthaler to the heirs. Magnus Heinasons remains were exhumed and taken to Ørslev Monastery on Lindenovs estate where they lie under the floor of the church until this day. Magnus Heinason was engaged three times and married twice, Magnus had a son with a Faroese lady Kollfina around 1560. Rasmus Magnussen lived to the age of 110 years, and at the age of 103 he became the father of a son, in 1580 Magnus met a Norwegian noble lady Margrethe Axeldatter Gyntersberg or von Güntersberg. They had a child Mogensbarn that died as child and they did not marry, because she accused him of rape. The noble family then demanded that he marry Margrethes younger sister and they married in 1582 in Bergenhus, Bergen and had one daughter, Elsebeth Magnusdatter. She later married Anders Matsen Ǣnes and lived at Ǣnes in the Hardangerfjord in Norway, in his job as a priest in the Faroes, Magnus father, Heine Havreki travelled much by sea, to and from the islands. Magnus accompanied him on these journeys, even as a little boy Magnus knew how to sail small boats and gained a lot of experience that would be useful later in life. As a grown man in his career as a seaman and a privateer he would carry out some of his most notorious acts in these same waters, when Magnus was 17 or 18 years old his father was transferred to Norway. Here Magnus was able to live out his dream of becoming a seaman due to family connections on his fathers side. At a young age he was captain of a trade ship on the route that his father had sailed for many years. On his third trip he was attacked by pirates, what actually occurred is not known, but when he returned to Bergen, people ridiculed him for giving up without a fight. He was deeply upset by this incident and swore that he would take revenge and he left Norway and went to the Netherlands where he joined the Navy
Magnus Heinason
–
The Rosenkrantz Tower located on
Bergenhus Fortress
Magnus Heinason
–
Oyndarfjørður
Magnus Heinason
–
Maurice of Nassau, Prince of Orange – portrait by
Michiel Jansz van Mierevelt
Magnus Heinason
–
Frederick II of Denmark and Norway
19.
Proletariat
–
The proletariat is a term for the class of wage-earners, in a capitalist society, whose only possession of significant material value is their labor-power, a member of such a class is a proletarian. The proletarii constituted a class of Roman citizens owning little or no property. This assembly, which met on the Campus Martius to discuss public policy issues, was also used as a means of designating military duties demanded of Roman citizens. The top infantry class assembled with full arms and armor, the two classes brought arms and armor, but less and lesser, the fourth class only spears. In voting, the cavalry and top class were enough to decide an issue, as voting started at the top. As a result of the Marian reforms initiated in 107 B. C. by the Roman general Gaius Marius, proletarians are wage-workers, while some refer to those who receive salaries as the salariat. For Marx, however, wage labor may involve getting a salary rather than a wage per se, intermediate positions are possible, where some wage-labor for an employer combines with self-employment. Socialist parties have often struggled over the question of whether they should seek to organize and represent all the lower classes, according to Marxism, capitalism is a system based on the exploitation of the proletariat by the bourgeoisie. Instead of hiring those means of production, they themselves get hired by capitalists and work for them and these goods or services become the property of the capitalist, who sells them at the market. Surplus value is the difference between the wealth that the proletariat produces through its work, and the wealth it consumes to survive and to provide labor to the capitalist companies. A part of the value is used to renew or increase the means of production, either in quantity or quality. What remains is consumed by the capitalist class, the commodities that proletarians produce and capitalists sell are valued for the amount of labor embodied in them. The same goes for the labor power itself, it is valued, not for the amount of wealth it produces. Marxists argue that new wealth is created through labor applied to natural resources, prole drift, short for proletarian drift, is a term that suggests the tendency in advanced industrialized societies for everything inexorably to become proletarianized, or to become commonplace. This trend is attributed to mass production, mass selling, mass communication, examples include best-seller lists, films and music that must appeal to the masses and shopping malls. Why workers can change the world, hal Draper, Karl Marxs Theory of Revolution, Vol.2, The Politics of Social Classes
Proletariat
–
A
manual labourer at work in
Venezuela. Manual labourers are generally considered to be part of the proletariat.
Proletariat
–
A 1911
Industrial Worker publication advocating industrial unionism based on a critique of capitalism. The proletariat "work for all" and "feed all".
20.
Frederick III of Denmark
–
Frederick III was king of Denmark and Norway from 1648 until his death. He also governed under the name Frederick II as diocesan administrator of the Prince-Bishopric of Verden, and he instituted absolute monarchy in Denmark-Norway in 1660, confirmed by law in 1665 as the first in Western historiography. He also ordered the creation of the Throne Chair of Denmark and he was born the second-eldest son of Christian IV and Anne Catherine of Brandenburg. Frederick was only considered an heir to the throne after the death of his older brother Prince Christian in 1647, in order to be elected king after the death of his father, Frederick conceded significant influence to the nobility. As king, he fought two wars against Sweden and he was defeated in the Dano-Swedish War of 1657–1658, but attained great popularity when he weathered the 1659 Assault on Copenhagen and won the Dano-Swedish War of 1658–1660. Later that year, Frederick used his popularity to disband the elective monarchy in favour of absolute monarchy and he married Sophie Amalie of Brunswick-Lüneburg, with whom he fathered Christian V of Denmark. Frederick was born at Haderslev in Slesvig, the son of Christian IV, in his youth and early manhood, there was no prospect of his ascending the Danish throne, as his older brother Christian was elected heir apparent in 1608. Frederick was educated at Sorø Academy and studied in the Netherlands, as a young man, he demonstrated an interest in theology, natural sciences, and Scandinavian history. He was a reserved and enigmatic prince who seldom laughed, spoke little, and wrote less, even though he lacked the impulsive and jovial qualities of his father, Frederick possessed the compensating virtues of moderation and self-control. On 1 October 1643 Frederick wed Sophie Amalie of Brunswick-Lüneburg, the daughter of George, Duke of Brunswick-Lüneburg, who had an energetic, passionate and he was an enthusiastic collector of books and his collection became the foundation for the Copenhagen Royal Library. In his youth, Frederick became the instrument of his fathers political schemes in the Holy Roman Empire and he was granted administration of the Prince-Archbishopric of Bremen, the Prince-Bishopric of Verden, and named coadjutor of the Bishopric of Halberstadt. Thus, from an age, he had considerable experience as an administrator. At the age of eighteen, he was the commandant of the Bremian fortress of Stade. During the Torstenson War of 1643–45, Frederick lost control of his possessions within the empire and he was then appointed commander in the royal shares in the Duchies of Schleswig and Holstein by his father. His command was not successful, chiefly owing to his quarrels with the Earl-Marshal Anders Bille and this was Fredericks first collision with the Danish nobility, who afterwards regarded him with extreme distrust. The death of his elder brother Christian in June 1647 opened the possibility for Frederick to be elected heir apparent to the Danish throne, however, this issue was still unsettled when Christian IV died on 28 February 1648. After long deliberation among the Danish Estates and in the Rigsraadet, on 6 July, Frederick received the homage of his subjects, and he was crowned on 23 November. The Haandfæstning included provisions curtailing the already diminished royal prerogative in favour of increased influence for the Rigsraadet, in the first years of his reign, the Rigsraadet was the main power center of Danish politics
Frederick III of Denmark
–
Frederick III
Frederick III of Denmark
–
Duke Frederick, painting by
Pieter Isaacsz
Frederick III of Denmark
–
King Frederik III on horseback. Painting by
Wolfgang Heimbach.
Frederick III of Denmark
–
The peace banquet (Fredstaffelet) at Frederiksborg Castle following the signing of the Treaty of Roskilde in 1658.
21.
Kristoffer Gabel
–
Christoffer Gabel was a Danish statesman. He was born on 6 January 1617 at Glückstadt and his father, Wulbern or Waldemar Gabel, originally a cartographer and subsequently recorder of Glückstadt, was killed at the siege of the fortress there, by the German Imperial Army, in 1628. Nothing is known of Christoffers youth, but it is certain he received a university education, Christoffers name is first recorded in 1639, as overseer and accountant at the court of the Archbishop of Bremen, Duke Frederick. His activities won the kings lifelong gratitude and he was enriched, ennobled, and in 1664 made governor of Copenhagen. From 1660 to 1670 he was regarded as the most influential figure at court, during this period he carried out a pro-French foreign policy, while his domestic policy was affected by laziness and corruption. When Frederick III died, in February 1670, Gabels power was at an end, the new ruler, Christian V did not favour him, and accusations against Gabel poured in from every quarter. When, on 18 April 1670, he was dismissed, there was no sympathy for a man who had grown wealthy in a time of widespread poverty. He was stripped of all titles and privileges, except the control of the Faroe Islands. He spent his time in Copenhagen, and died on 13 October 1673 and was buried in St. Peters Church
Kristoffer Gabel
–
Christoffer von Gabel
22.
Bailiff
–
A bailiff is a manager, overseer or custodian, a legal officer to whom some degree of authority or jurisdiction is given. Bailiffs are of various kinds and their offices and duties vary greatly, another official sometimes referred to as a bailiff was the vogt, see Vogt and Vogt. In the Holy Roman Empire a similar function was performed by the Amtmann, Bailiff was the term used by the Normans for what the Saxons had called a reeve, the officer responsible for executing the decisions of a court. The duty of the bailiff would thus include serving summonses and orders, the district within which the bailiff operated was called his bailiwick, even to the present day. Bailiffs were outsiders and free men, that is, they were not usually from the bailiwick they were responsible for. Throughout Norman England, the Saxon and Norman populations gradually mixed, primarily then, bailiff referred to the officer executing the decisions of manorial courts, and the hundred courts. Likewise, in Scotland a bailie was the officer of a barony. With the introduction of Justices of the Peace, magistrates courts acquired their own bailiffs, historically, courts were not always concerned with legal matters, and often decided administrative matters for the area within their jurisdiction. A bailiff of a manor, therefore, would oversee the manors lands and buildings, collect its rents, manage its accounts. In the 19th century, the functions of courts were mostly replaced by the creation of elected local authorities. Nevertheless, the bailiff is retained as a title by the chief officers of various towns and the keepers of royal castles, such as the High Bailiff of Westminster. In Scotland, bailie now refers to an officer corresponding to an English alderman. The high court acquired the sheriffs, the county court the bailiffs, to avoid confusion with their underlings, the County Courts Act 1888 renamed bailifs as High Bailiffs. This act also formally acknowledged the High Bailiffs right to appoint under-bailiffs as he wished, the High Bailiff gradually became a purely ceremonial role, the courts clerk liaising with under-bailiffs directly. The Law of Distress Amendment Act 1888 enacts that no person may act as an under-bailiff to levy any distress for rent, unless he is authorized by a county court judge to act as an under-bailiff. The County Courts Act 1888 restricted the hours an under-bailiff could execute a possession warrant and it also limited the ability to bring a legal complaint against a bailiff, six days notice now had to be given. In the Channel Islands the bailiff is the first civil officer in each of the two bailiwicks and he is appointed by the Crown, and holds office until retirement. He presides as a judge in the court, and takes the opinions of the jurats, he also presides over the states
Bailiff
–
Bailiff's notice on boarded-up premises, London, 2015.
Bailiff
–
Ontario Provincial Bailiff Shoulder Flash
23.
Copenhagen
–
Copenhagen, Danish, København, Latin, Hafnia) is the capital and most populous city of Denmark. Copenhagen has an population of 1,280,371. The Copenhagen metropolitan area has just over 2 million inhabitants, the city is situated on the eastern coast of the island of Zealand, another small portion of the city is located on Amager, and is separated from Malmö, Sweden, by the strait of Øresund. The Øresund Bridge connects the two cities by rail and road, originally a Viking fishing village founded in the 10th century, Copenhagen became the capital of Denmark in the early 15th century. Beginning in the 17th century it consolidated its position as a centre of power with its institutions, defences. After suffering from the effects of plague and fire in the 18th century and this included construction of the prestigious district of Frederiksstaden and founding of such cultural institutions as the Royal Theatre and the Royal Academy of Fine Arts. Later, following the Second World War, the Finger Plan fostered the development of housing, since the turn of the 21st century, Copenhagen has seen strong urban and cultural development, facilitated by investment in its institutions and infrastructure. The city is the cultural, economic and governmental centre of Denmark, Copenhagens economy has seen rapid developments in the service sector, especially through initiatives in information technology, pharmaceuticals and clean technology. Since the completion of the Øresund Bridge, Copenhagen has become integrated with the Swedish province of Scania and its largest city, Malmö. With a number of connecting the various districts, the cityscape is characterized by parks, promenades. Copenhagen is home to the University of Copenhagen, the Technical University of Denmark, the University of Copenhagen, founded in 1479, is the oldest university in Denmark. Copenhagen is home to the FC København and Brøndby football clubs, the annual Copenhagen Marathon was established in 1980. Copenhagen is one of the most bicycle-friendly cities in the world, the Copenhagen Metro serves central Copenhagen while the Copenhagen S-train network connects central Copenhagen to its outlying boroughs. Serving roughly 2 million passengers a month, Copenhagen Airport, Kastrup, is the largest airport in the Nordic countries, the name of the city reflects its origin as a harbour and a place of commerce. The original designation, from which the contemporary Danish name derives, was Køpmannæhafn, meaning merchants harbour, the literal English translation would be Chapmans haven. The English name for the city was adapted from its Low German name, the abbreviations Kbh. or Kbhvn are often used in Danish for København, and kbh. for københavnsk. The chemical element hafnium is named for Copenhagen, where it was discovered, the bacterium Hafnia is also named after Copenhagen, Vagn Møller of the State Serum Institute in Copenhagen named it in 1954. Excavations in Pilestræde have also led to the discovery of a well from the late 12th century, the remains of an ancient church, with graves dating to the 11th century, have been unearthed near where Strøget meets Rådhuspladsen
Copenhagen
–
From upper left:
Christiansborg Palace,
Frederik's Church,
Tivoli Gardens and
Nyhavn.
Copenhagen
–
Reconstruction of Copenhagen c. 1500
Copenhagen
–
The
Tøjhus Arsenal (
1604)
Copenhagen
–
The
Børsen, former stock exchange (completed
1640)
24.
England
–
England is a country that is part of the United Kingdom. It shares land borders with Scotland to the north and Wales to the west, the Irish Sea lies northwest of England and the Celtic Sea lies to the southwest. England is separated from continental Europe by the North Sea to the east, the country covers five-eighths of the island of Great Britain in its centre and south, and includes over 100 smaller islands such as the Isles of Scilly, and the Isle of Wight. England became a state in the 10th century, and since the Age of Discovery. The Industrial Revolution began in 18th-century England, transforming its society into the worlds first industrialised nation, Englands terrain mostly comprises low hills and plains, especially in central and southern England. However, there are uplands in the north and in the southwest, the capital is London, which is the largest metropolitan area in both the United Kingdom and the European Union. In 1801, Great Britain was united with the Kingdom of Ireland through another Act of Union to become the United Kingdom of Great Britain and Ireland. In 1922 the Irish Free State seceded from the United Kingdom, leading to the latter being renamed the United Kingdom of Great Britain, the name England is derived from the Old English name Englaland, which means land of the Angles. The Angles were one of the Germanic tribes that settled in Great Britain during the Early Middle Ages, the Angles came from the Angeln peninsula in the Bay of Kiel area of the Baltic Sea. The earliest recorded use of the term, as Engla londe, is in the ninth century translation into Old English of Bedes Ecclesiastical History of the English People. According to the Oxford English Dictionary, its spelling was first used in 1538. The earliest attested reference to the Angles occurs in the 1st-century work by Tacitus, Germania, the etymology of the tribal name itself is disputed by scholars, it has been suggested that it derives from the shape of the Angeln peninsula, an angular shape. An alternative name for England is Albion, the name Albion originally referred to the entire island of Great Britain. The nominally earliest record of the name appears in the Aristotelian Corpus, specifically the 4th century BC De Mundo, in it are two very large islands called Britannia, these are Albion and Ierne. But modern scholarly consensus ascribes De Mundo not to Aristotle but to Pseudo-Aristotle, the word Albion or insula Albionum has two possible origins. Albion is now applied to England in a poetic capacity. Another romantic name for England is Loegria, related to the Welsh word for England, Lloegr, the earliest known evidence of human presence in the area now known as England was that of Homo antecessor, dating to approximately 780,000 years ago. The oldest proto-human bones discovered in England date from 500,000 years ago, Modern humans are known to have inhabited the area during the Upper Paleolithic period, though permanent settlements were only established within the last 6,000 years
England
–
Stonehenge, a
Neolithic monument
England
–
Flag
England
–
Boudica led an uprising against the
Roman Empire
England
–
Replica of a 7th-century ceremonial
helmet from the
Kingdom of East Anglia, found at
Sutton Hoo
25.
Church of the Faroe Islands
–
The Church of the Faroe Islands is one of the smallest of the worlds state churches. Prior to its becoming independent on 29 July 2007, it had been a diocese of the Church of Denmark, about 81. 6% of the Faroe Islanders belong to the state church. Other churches in the Faroe Islands include the Plymouth Brethren and the Catholic Church, according to Færeyinga saga, it was the Viking chief Sigmundur Brestisson who brought Christianity to the Faroe Islands. On the orders of the Norwegian king Olaf Tryggvason, Sigmundur forced the people to convert to Christianity in 999. Resistance to the new religion led by the notorious Tróndur í Gøtu was quickly suppressed, from the time Christianity was introduced until the Reformation there were probably 33 bishops in the Faroe Islands. This period was not always peaceful, the sagas of the Faroe Islands contain two accounts of the way the church took possession of a large proportion of the land, overtaxing the people so harshly that it led to open rebellion. The saga of the battle of Mannafallsdal relates that the bishop was killed outside his church by the rebels, the historical value of this saga is highly debatable - but it does serve to illustrate the conflict between the theocratic church and an impoverished population. However, there is documentation of the fact that the bishops residence in Kirkjubø was burnt to the ground by the rebels. Bishop Erlend died in Bergen in 1308, in 1540 the last Catholic bishop in the Faroe Islands was removed from his position. His Protestant replacement only lasted a few years - then he too left the islands, brochmands devotional book dating back to about 1650 and Thomas Kingos hymns from 1699 constituted a significant proportion of the spiritual life of the islands right up until the twentieth century. Indeed, the expression Brochmandslestur is still used to long and, as some might perceive them, boring texts. See main articles, Faroese language conflict, Christmas Meeting of 1888 When the Danish trade monopoly was lifted in 1856, the restoration of long-suppressed Faroese culture also led to changes in Christianity on the islands. After great contention, Faroese was given the status as Danish in hymns. The ecclesiastical rituals were introduced in Faroese in 1930, and in 1961 the authorised Faroese edition of the Bible was published, during the first half of the 20th century, Dean Jákup Dahl had translated the New Testament from Greek - this was published in 1937. Dahl also translated the psalms from the Old Testament, and after his death in 1944 a vicar named Kristian Osvald Viderø continued to translate the rest of the Bible from Hebrew. In 1963 the first Faroese hymn book was published, and in the year the old title of Dean on the islands was upgraded to Deputy Bishop. In 1977 the first female vicar was ordained, and in 1990 the Faroe Islands became an independent diocese with its own bishop within the Church of Denmark. In 2005 the Faroes signed a treaty with Denmark that allows for the taking over of most public institutions, including the Vágar Airport, on the National Holiday Ólavsøka,29 July 2007, the Faroese Church became totally independent of the Church of Denmark
Church of the Faroe Islands
–
The old wooden church of
Gøta.
Church of the Faroe Islands
–
Arrival of Christianity about 1000 AD: Chieftain Tróndur í Gøtu defending the Nordic Religion of the Vikings
Church of the Faroe Islands
–
Faroese clergymen played a major part in the National awakening and language conflict, which was a conflict within Faroese society rather than with the Danish.
26.
Gunboat War
–
The Gunboat War was the naval conflict between Denmark–Norway and the British Navy during the Napoleonic Wars. The wars name is derived from the Danish tactic of employing small gunboats against the conventional Royal Navy, in Scandinavia it is seen as the later stage of the English Wars, whose commencement is accounted as the First Battle of Copenhagen in 1801. The naval conflict between Britain and Denmark commenced with the First Battle of Copenhagen in 1801 when Horatio Nelsons squadron of Admiral Parkers fleet attacked the Danish capital, the tactical advantages were that they were highly manoeuvrable, especially in still and shallow waters and presented small targets. On the other hand, the boats were vulnerable and likely to sink from a single hit and they therefore could not be used in rough seas, and they were less effective against large warships. The Danish Commander Steen Andersen Bille is credited with being the force behind the post-1807 Dano-Norwegian strategy of gunboat warfare. Below is a description of each of the four classes of gunboats according to Junior Lieutenant Garde, kanonchaluppen, These were the larger type of gunboat. Each was armed with two 24-pound cannon and four 4-pound howitzers and had an establishment of 69 –79 men. Kanonjollen, These were the type of gunboat. Each was armed with one 24-pound cannon and two 4-pound howitzers, and had wartime establishment of 41 men, morterchaluppen, These were the larger, mortar-armed gunboats. Each was armed with one 100-pound mortar and two 4-pound howitzers, and had an establishment of 40 men. Morterbarkasserne, These were smaller, mortar-armed gunboats, each was armed with one mortar and had a wartime establishment of 19 men. They were little more than ordinary ships’ boats into which a mortar had been set and they had a tendency to leak badly after 5 –7 mortar shells had been fired. Their crews then had to bring back into harbour, remove the mortar. Reserve crew who could not be accommodated on board were quartered in buildings on land or in the frigate Triton which was in ordinary, battle-ready gunboats had their crews on board. Defences on the Norwegian coast in 1808 are listed at Royal Dano-Norwegian Navy order of battle in Norway, ten schooner-rigged gunboats capable of operating in the rougher Norwegian Sea were built in Bergen and Trondheim in the years 1808 to 1811. Further economic damage was done by raids on the smaller islands, British warships landed to replenish firewood and water supplies, and forcibly to buy, commandeer or simply take livestock to augment their provisions. The war overlapped, in time, the Anglo-Russian War, as a result, the British expanded their trade embargo to Russian waters and the British navy conducted forays northwards into the Barents Sea. The navy conducted raids on Hasvik and Hammerfest and disrupted the Pomor trade, in the engagement the British suffered only one man wounded, the Danes lost 12 men while 20 were wounded, some mortally
Gunboat War
–
Battle between the frigate
HMS Tartar and Danish gunboats at
Alvøen near
Bergen in 1808
Gunboat War
–
Danish shallop gunboat
Gunboat War
–
Battle of Zealand Point
Gunboat War
–
The Spanish
Division of the North sent to fight the British in Denmark pledging to turn against France and side with the British
27.
Cruizer class brig-sloop
–
The Cruizer class was an 18-gun class of brig-sloops of the Royal Navy. Brig-sloops were the same as ship-sloops except for their rigging, a ship-sloop was rigged with three masts whereas a brig-sloop was rigged as a brig with only a fore mast and a main mast. Of the vessels in the class, eight were lost to the enemy, fourteen were wrecked while in British service. Lastly, four foundered while in British service, in all cases of foundering and in many cases of wrecking all the crew was lost. Many of the vessels in the class were sold, some into mercantile service, the fate of the others is generally unknown. In December 1796, the Navy Board placed new orders for four flush-decked sloops, in order to compare the qualities of ship-rigged and brig-rigged vessels, one vessel to each design was to be completed as a ship-sloop and the other as a brig-sloop. The hull design was exceeding fine, a noted deadrise amidships, the order placed in March 1797 for the first sister ship to Cruizer was subsequently cancelled, but new orders were placed from 1802 up to 1813. A final order in 1815 was cancelled in 1820, the Dutch built three 18 gun-brigs — Zwaluw, Mercuur and Kemphaan — to a similar design, in one case apparently a copy, though without the square tuck stern. The Russian brig Olymp was also built to the same lines, few men in the Royal Navy had a good word to say for the gun-brigs, which rolled terribly and were greatly over-crowded, but they had to be employed. It should be noted later in the same book he was more complementary as regards the larger brigs such as the Cruizer class HMS Penguin. Perhaps the most salient aspect of his statement is that the Cruizer class and its smaller sister class, the class proved to be ideal for many of the shallow water commitments in the Baltic and Ionian Seas, as well as around Danish waters. Prior to 1808, the complement of officers, men, after 1808, the vessels carried 20 marines comprising 1 sergeant,1 corporal and 18 privates. During the Anglo-American War of 1812, several ships of the class fell victim to larger American ship-rigged sloops of war of nominally the same class, the American vessels enjoyed an advantage in weight of broadside and number of crew. The ship-rigged sloops enjoyed the ability to sail, and their rigging proved more resistant to damage, by contrast. The comparison was made in the London press unfavorably and was not entirely fair, the American ship-rigged sloops were bigger vessels, averaging just over 500 tons, the Cruizer-class vessels were not quite 400 tons. The crew sizes were disproportionate at 175 to 120, and at least some of the Cruizer class in these combats were outfitted with 24-pounder carronades vice the normal 32-pounders, the rigging was often the deciding factor as the USS Peacock vs. HMS Epervier combat would highlight. When HMS Epervier lost her main topmast and had her foremast damaged she was disabled, USS Wasp, in another combat, would retain control despite the loss of her gaff, main topmast, and the mizzen topgallant. USS Wasp vs. HMS Avon provides another example, despite being fought gallantly, Avon was crippled by loss of a gaff
Cruizer class brig-sloop
–
The Cruizer -class brig-sloop
HMS Pelorus aground at low water
Cruizer class brig-sloop
–
Sketch of a brig-sloop, probably
HMS Clio, by Cmdr. William Farrington, ca. 1812,
Peabody Essex Museum
Cruizer class brig-sloop
–
HMS Surinam struck by lightning, 11 December 1806, by
Nicholas Matthews Condy,
National Maritime Museum,
Greenwich
Cruizer class brig-sloop
–
An earlier
USS Wasp boards the Cruizer -class
HMS Frolic, 1812
28.
HMS Clio (1807)
–
HMS Clio was Cruizer-class brig-sloop of the Royal Navy, launched at James Betts shipyard in Mistleythorn on 10 January 1807. Her establishment was 71 officers and men,24 boys and 20 marines and she served in the Baltic during the Napoleonic Wars, accomplished the re-establishment of British rule on the Falkland Islands in 1833, and participated in the First Opium War. She was broken up in 1845, in February 1807 Commander Thomas Folliott Baugh commissioned her and sailed her to the Leith Station on the North Sea. Here he succeeded in taking several prizes, but not until 1808, the first appears to have been the Helyra, Hook, master, from Bergen, which Clio sent into Leith in July. Then on 21 September 1808, while she was cruising off Fleckoro, Clio captured a small Danish privateer armed with six guns, the captured vessel arrived at Leith on 12 October. On 7 December she captured the Vrouw Heltya, on 30 March 1808, during the Gunboat War, Clio entered Tórshavn, the capital of the Faroe Islands, and briefly captured the fort at Skansin. The fort surrendered without firing a shot as the party approached. The landing party spiked the forts eight 18-pounder guns and took all the guns and weapons before leaving. Shortly after, on 6 May, a German privateer who had assumed the name Baron von Hompesch plundered the defenceless city, the Admiralty Prize Court, however, refused to condemn it as a lawful prize. Later, after the Jørgen Jørgensen affair, Britain declared the Faroese, the Icelanders, after this adventure Clio captured some more Danish vessels. On 10 August she captured the Vrou Sophia, on 1 September she captured the Junge Jacob and the Wilhelmina Frederica. On 21 September she captured two more, names unknown, which she sent in to Gothenburg, more small prizes followed in 1809. On 23 February 1809, Clio took five Danish vessels, another account has her capturing seven Danish privateers and arriving at Whitby with one of them on 26 February. She detained an American vessel that was sailing from Hambro to Petersburg and sent her into Leith, on 7 September she captured the Danish galliot Providentia and on 14 September the sloop Speculation. On 7 November she, with Childers in company, captured Danish schooner No.32, then on 15 and 16 November she captured the Danish vessels Three Children, Perlin, St Ola, and Fine Smaakin. One of these may have been the vessel arrived at Leith on the 17th. Two more Danish vessels arrived at Leith on 5 December, Baugh was promoted to Post-captain on 21 October 1810. While temporarily under the command of Lieutenant M. J. Popplewell and that same day she was in company when Pyramus captured the Danish vessel Fanoe
HMS Clio (1807)
–
Sketch of a brig-sloop, probably HMS Clio, by Cmdr. William Farrington, ca. 1812,
Peabody Essex Museum
29.
Touch hole
–
The vent is the access point through which the propellant charge is ignited. In small arms, the flash from a charge of priming held in the pan is enough to ignite the charge within. In artillery, priming powder, a fuse, squib, or friction igniter is inserted into the hole to ensure ignition of the charge. The powder in the hole was lit either with a slow match. Spiking a gun was a method of disabling a cannon by hammering a barbed steel spike into the touch-hole. If a cannon was in danger of being captured by the enemy, captured guns would be spiked if they could not be hauled away and the guns recapture seemed likely. If a special spike was unavailable, spiking could be done by driving a bayonet into the touch-hole and breaking it off, guns could also be rendered useless by burning their wooden carriages or blowing off their trunnions
Touch hole
–
Essential parts of a cannon: 1. the
projectile or cannonball (shot) 2.
gunpowder 3. touch hole (or vent)
30.
HMS Furious (47)
–
HMS Furious was a modified Courageous-class battlecruiser built for the Royal Navy during the First World War. Furious was modified and became a carrier while under construction. Her forward turret was removed and a deck was added in its place. Later in the war, the ship had her rear turret removed and a flight deck installed aft of the superstructure. Furious was briefly laid up after the war before she was reconstructed with a flight deck in the early 1920s. After her conversion, Furious was used extensively for trials of naval aircraft, during the early months of the Second World War the carrier spent her time hunting for German raiders in the North Atlantic and escorting convoys. This changed dramatically during the Norwegian Campaign in early 1940 when her aircraft provided air support to British troops ashore in addition to attacking German shipping, the first of what would be a large number of aircraft ferry missions was made by the carrier during the campaign. After the withdrawal of British troops in May, Furious made several anti-shipping strikes in Norway with little result before beginning a routine of ferrying aircraft for the Royal Air Force. At first Furious made several trips to West Africa, but she began to ferry aircraft to Gibraltar in 1941, an unsuccessful attack on German-occupied ports on the Arctic Ocean interrupted the ferry missions in mid-1941. Furious was given a refit in the United States and spent a few months training after her return in April 1942. She made several more trips in mid-1942 before her aircraft attacked airfields in Vichy French Algeria as part of the opening stages of Operation Torch in November 1942. The ship remained in the Mediterranean until February 1943 when she was transferred to the Home Fleet, Furious spent most of 1943 training, but made a number of attacks on the German battleship Tirpitz and other targets in Norway during the first half of 1944. By September 1944, the ship was showing her age and she was placed in reserve, Furious was decommissioned in April 1945, but was not sold for scrap until 1948. He justified their existence by claiming he needed fast, shallow-draught ships for his Baltic Project, Furious had an overall length of 786 feet 9 inches, a beam of 88 feet, and a draught of 24 feet 11 inches at deep load. She displaced 19,513 long tons normally and 22,890 long tons at deep load and she had a metacentric height of 5.33 feet at deep load. Furious and her half-sisters were the first large warships in the Royal Navy to have geared steam turbines. To save design time the installation used in the light cruiser Champion, the four Brown-Curtis turbines were powered by eighteen Yarrow small-tube boilers that were designed to produce a total of 90,000 shaft horsepower. The ships speed was an estimated 31.5 knots, Furious was designed to normally carry 750 long tons of fuel oil, but could carry a maximum of 3,160 long tons
HMS Furious (47)
–
HMS Furious circa 1935—36
HMS Furious (47)
–
Furious as originally completed. She had a flying-off deck for aircraft forward.
HMS Furious (47)
–
Closeup of the ship shortly following its initial conversion and in
dazzle paint scheme. An
SSZ class blimp is on the after deck
31.
Cabinet of the Faroe Islands
–
The Cabinet of the Faroe Islands has been the chief executive body and the government of the Faroe Islands since the islands became self-governing in 1948. The cabinet is led by the Prime Minister, there are around 7 members of the Cabinet, known as Ministers, all of whom are also heads of specific government ministries. The ministers are appointed by the Prime Minister, the Faroese government currently consists of seven ministers including the Prime Minister. Løgting Politics of the Faroe Islands Tinganes. fo - The Faroese Prime Ministers Office
Cabinet of the Faroe Islands
–
Faroe Islands
32.
Argir
–
Argir is a village in the Faroe Islands. Argir most likely takes its name from Old Irish airge meaning summer pasture, several placenames in Faroe carry the same name with this meaning. Once a village south of Tórshavn, Argir has grown and is now merged with Tórshavn, in 1997 it joined the municipality of Tórshavn. In recent years more and more houses have built in Argir. The uppermost part of Argir is now so far away from Torshavn that a car is practically needed to be able to live there, in return the area offers a magnificent view over the sea and the capital. There is a boat harbour with boathouses in Argir. The church in Argir was built in 1974, from the 16th century there was a leprosy-hospital in Argir. Some paupers were living there as well, when the leprosy was eradicated in 1750 the hospital was turned into a workhouse for the poor. Argirs football team is AB, they play in the mens top division. Argir has one of the largest rowing clubs of the Faroes, it is called Argja Róðrarfelag, list of towns in the Faroe Islands Faroeislands. dk, Agir Images and description of all cities on the Faroe Islands
Argir
–
Argir and a part of Tórshavn
Argir
–
Map showing the position of Argir on Streymoy
Argir
–
Argir, January 2010.
Argir
–
Argir, a sign with the village name.
33.
Subpolar oceanic climate
–
Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, and above 0 °C in the coldest month. It typically lacks a dry season, as precipitation is evenly dispersed throughout the year. Oceanic climates generally have cool summers and mild to cool winters, Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies, many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. Precipitation is both adequate and reliable throughout the year in oceanic climates, extended months of rain and cloudy conditions are common in oceanic climates. Seattle is an example of this, between October and May, Seattle experiences high rainfall and is mostly or partly cloudy six out of every seven days. In most areas with a 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, outside of Australia and parts of New Zealand, most areas with an oceanic climate experience at least one snowstorm per year. In the poleward locations of the climate zone, snowfall is more frequent. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature, summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the subpolar oceanic climate, with long and cold winters and cool. Examples of this climate include parts of coastal Iceland in the Northern Hemisphere and extreme southern Chile, Oceanic climates are not necessarily always found in coastal locations on the aforementioned parallels, however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream, which moves in a west to east direction across the middle latitudes, advancing low pressure systems, storms, in coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the adjacent to them. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Oceanic climates in Europe occur mostly in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, Germany, Norway, the north coast of Spain, examples of oceanic climates are found in London, Bergen, Dublin, Berlin, Bilbao, Donostia-San Sebastian, Biarritz, Bayonne, Zürich, Copenhagen and Paris. With decreasing distance to the Mediterranean Sea, the climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe
Subpolar oceanic climate
–
Seattle, a city with an oceanic climate
Subpolar oceanic climate
–
World map showing oceanic climate zones, as defined by the
Köppen climate types "Cfb", "Cfc", "Cwb" and "Cwc"
Subpolar oceanic climate
–
Curitiba, capital city of Brazilian
Paraná state features a subtropical highland climate
34.
Aleutian Islands
–
The Aleutian Islands are a chain of 14 large volcanic islands and 55 smaller ones belonging to both the United States and Russia. Crossing longitude 180°, at which point east and west longitude end, the westernmost U. S. island in real terms, however, is Attu Island, west of which runs the International Date Line. The islands, with their 57 volcanoes, are in the part of the Pacific Ring of Fire. Physiographically, they are a section of the larger Pacific Border province. These Islands are most known for the battles and skirmishes occurred there during the Aleutian Islands Campaign of World War II. It was one of two attacks on the United States during that war. The largest islands in the Aleutians are Attu, and Unalaska, Umnak, and Unimak in the Fox Islands. The largest of those is Unimak Island, with an area of 1,571.41 mi², followed by Unalaska Island, the axis of the archipelago near the mainland of Alaska has a southwest trend, but near 179° its direction changes to the northwest. This change of direction corresponds to a curve in the line of fissures that have contributed their products to the building of the islands. Such curved chains are repeated about the Pacific Ocean in the Kuril Islands, the Japanese chain, and in the Philippines. All these island arcs are at the edge of the Pacific Plate and experience much seismic activity, but are still habitable, the general elevation is greatest in the eastern islands and least in the western. The island chain is a continuation of the Aleutian Range on the mainland. The coasts are rocky and surf-worn, and the approaches are exceedingly dangerous and these volcanic islands reach heights of 6,200 feet. Makushin Volcano located on Unalaska Island, is not quite visible from within the town of Unalaska, though the steam rising from its cone is visible on a clear day. Residents of Unalaska need only to one of the smaller hills in the area, such as Pyramid Peak or Mt. Newhall. The volcanic Bogoslof and Fire Islands, which rose from the sea in 1796 and 1883 respectively, in 1906 a new volcanic cone rose between the islets of Bogoslof and Grewingk, near Unalaska, followed by another in 1907. These cones were demolished by an explosive eruption on September 1,1907. Newly found information in 2017, the volcanic cone erupted sending ash, the Aleutians seen from space The climate of the islands is oceanic, with moderate and fairly uniform temperatures and heavy rainfall
Aleutian Islands
–
Unalaska Island in the Aleutian Islands.
Aleutian Islands
–
Aleutian Islands
Aleutian Islands
–
The Aleutian Islands from 32,000 feet.
Aleutian Islands
–
Image of the islands taken by the
STS-56 crew.
35.
Zona Austral
–
The Zona Austral is one of the five natural regions into which CORFO divided continental Chile in 1950 corresponding to the Chilean portion of Patagonia. It is surrounded by the Zona Sur and the Chacao Channel to the north, the Pacific Ocean and Drakes Passage to the south and west, if excluding Chiloé Archipelago Zona Austral covers all of Chilean Patagonia. In the far south, which extends from Valdivia through the Chacao Channel to Cape Horn, the Andes and this district of the country is mountainous, heavily forested and inhospitable. The heavy and continuous throughout this region, especially in the latitude of Chiloé, gives rise to a large number of rivers. Farther south this excessive precipitation is in the form of snow in the Andes, forming glaciers at a low level which in places discharge into the inlets. The perpetual snow-line here descends to 1,000 to 1,200 m above sea-level, an important transverse mountain range of the Andes separates the valleys of the rivers Simpson and Ibañez. This section is dominated by the active Hudson volcano and the jagged Cerro Castillo, southward from General Carrera lake is found a wide oblique opening in the range, through which flows the river Baker. The main chain of the Andes in the west is a rugged mass of ice and snow of an average height of 2700 m. Monte San Valentin is the point of the Andes in the region extending from 49° to 46° S latitude Monte San Lorenzo. The section from 48° to 52° S latitude is a continuous ice-capped mountain range, and some of the glaciers extend from the lakes to the western channels. The highest mountain in the section is Lautaro volcano, but the most famous compose the Cordillera del Paine in the south and the Fitz Roy group in the north. The southernmost part of zone is formed by two small parallel ranges called Cordillera Sarmiento and Cordillera Riesco, which are separated by the Fjord of the Mountains. Up to Strait of Magellan, the slope of the Cordillera does not, properly speaking. The extent of the glaciers is considerable in this region, which, farther south the Andes terminates in Cape Horn. In this section the mountains are composed principally of crystalline rocks, the rest of the land consists of literally thousands of islands forming numerous archipelagos interwoven with sometimes-narrow channels, which provide the main routes of navigation. The grouping of such shows that they are in part the summits of a submerged mountain chain. Three groups of these, called Chiloé, Guaitecas and Chonos archipelagoes, the largest island of this portion of Austral Chile is Chiloé, which is inhabited. Some of the islands of these groups are also inhabited, though the excessive rainfall of these latitudes
Zona Austral
–
Patagonia
Zona Austral
–
Grey Glacier in the picture is one of the many outlet glaciers of the
Southern Patagonian Ice Field
Zona Austral
–
View of
Puerto Williams with
Dientes de Navarino mountains behind
Zona Austral
–
Panoramical view of
Coihaique
36.
Precipitation
–
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, rain, sleet, snow, graupel, Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and precipitates. Thus, fog and mist are not precipitation but suspensions, because the vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated, Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers, moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain is occurring. A stationary front is often present near the area of freezing rain, provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. Eventually, the droplets will grow large enough to form raindrops. Lake-effect snowfall can be locally heavy, thundersnow is possible within a cyclones comma head and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation, on the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. The movement of the trough, or intertropical convergence zone. Precipitation is a component of the water cycle, and is responsible for depositing the fresh water on the planet. Approximately 505,000 cubic kilometres of water falls as precipitation each year,398,000 cubic kilometres of it over the oceans and 107,000 cubic kilometres over land. Given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres, Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on celestial bodies, e. g. when it gets cold, Mars has precipitation which most likely takes the form of frost. Precipitation is a component of the water cycle, and is responsible for depositing most of the fresh water on the planet. Approximately 505,000 km3 of water falls as precipitation each year,398,000 km3 of it over the oceans, given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective, stratiform, and orographic rainfall, Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice
Precipitation
–
A thunderstorm with heavy precipitation
Precipitation
–
Long-term mean precipitation by month
Precipitation
–
Late-summer
rainstorm in
Denmark
Precipitation
–
Lenticular cloud forming due to mountains over Wyoming
37.
Relative humidity
–
Relative humidity is the ratio of the partial pressure of water vapor to the equilibrium vapor pressure of water at a given temperature. Relative humidity depends on temperature and the pressure of the system of interest and it requires less water vapor to attain high relative humidity at low temperatures, more water vapour is required to attain high relative humidity in warm or hot air. Humans are sensitive to high humidity because the body uses evaporative cooling, enabled by perspiration. Perspiration evaporates from the more slowly under humid conditions than under arid. For example, if the air temperature is 24 °C and the humidity is zero percent. If the relative humidity is 100 percent at the air temperature. In other words, if the air is 24 °C and contains saturated water vapor, then the human body cools itself at the rate as it would if it were 27 °C. The heat index and the humidex are indices that reflect the effect of temperature. In cold climates, the temperature causes lower capacity for water vapour to flow about. Dry cracked skin can result from dry air, low humidity causes tissue lining nasal passages to dry, crack and become more susceptible to penetration of Rhinovirus cold viruses. Low humidity is a cause of nosebleeds. The use of a humidifier in homes, especially bedrooms, can help with these symptoms, indoor relative humidities should be kept above 30% to reduce the likelihood of the occupants nasal passages drying out. Humans can be comfortable within a range of humidities depending on the temperature—from thirty to seventy percent—but ideally between 50% and 60%. Very low humidity can create discomfort, respiratory problems, and aggravate allergies in some individuals, in the winter, it is advisable to maintain relative humidity at 30 percent or above. Extremely low relative humidities may also cause eye irritation, wooden furniture can shrink, causing the paint that covers these surfaces to fracture. When the temperature is low and the humidity is high. When relative humidity approaches 100 percent, condensation can occur on surfaces, leading to problems with mold, corrosion, decay, condensation can pose a safety risk as it can promote the growth of mold and wood rot as well as possibly freezing emergency exits shut. The basic principles for buildings, above, also apply to vehicles, in addition, there may be safety considerations
Relative humidity
–
Humidity and hygrometry
38.
Sunshine duration
–
It is a general indicator of cloudiness of a location, and thus differs from insolation, which measures the total energy delivered by sunlight over a given period. Sunshine duration is usually expressed in hours per year, or in hours per day, the first measure indicates the general sunniness of a location compared with other places, while the latter allows for comparison of sunshine in various seasons in the same location. Another often-used measure is percentage ratio of recorded bright sunshine duration, an important use of sunshine duration data is to characterize the climate of sites, especially of health resorts. This also takes account the psychological effect of strong solar light on human well-being. It is often used to promote tourist destinations, if the Sun were to be above the horizon 50% of the time for a standard year consisting of 8,760 hours, apparent maximal daytime duration would be 4,380 hours for any point on Earth. However, there are physical and astronomical effects that change that picture, namely, atmospheric refraction allows the Sun to be still visible even when it physically sets below the horizon. For that reason, average daytime is longest in polar areas, places on the Arctic Circle have the longest total annual daytime,4,647 hours, while the North Pole receives 4,575. Because of elliptic nature of the Earths orbit, the Southern Hemisphere is not symmetrical, the Equator has a total daytime of 4,422 hours per year. Given the theoretical maximum of daytime duration for a given location, bright sunshine hours represent the total hours when the sunlight is stronger than a specified threshold, as opposed to just visible hours. Visible sunshine, for example, occurs around sunrise and sunset, measurement is performed by instruments called sunshine recorders. For the specific purpose of sunshine duration recording, Campbell–Stokes recorders are used, when the intensity exceeds a pre-determined threshold, the tape burns. The total length of the trace is proportional to the number of bright hours. Another type of recorder is the Jordan sunshine recorder, newer, electronic recorders have more stable sensitivity than that of the paper tape. In 2003, the duration was finally defined as the period during which direct solar irradiance exceeds a threshold value of 120 W/m². The sky is clear in these regions, and fair weather is virtually perpetual, the descending branch of the Hadley cell and the long-term lack of atmospheric disturbances helps to explain the seemingly endless supply of sunny, cloud-free days in the deserts. Low clouding conditions are associated with rainfall shortage, as seen in these dry regions. In the belt encompassing northern Chad and the Tibesti Mountains, northern Sudan, southern Libya, some places in the interior of the Arabian Peninsula receive 3, 600–3,800 hours of bright sunshine annually. The largest sun-baked region in the world is North Africa, the sunniest month in the world is December in Eastern Antarctica, with almost 23 hours of bright sun daily
Sunshine duration
–
Campbell–Stokes recorder measures sunshine
39.
Faroe Islands national football team
–
The Faroe Islands national football team, represents the Faroe Islands in association football and is controlled by the Faroe Islands Football Association. The Faroe Islands became a member of FIFA in 1988 and UEFA in 1990 and is the fourth smallest UEFA country by population, Faroe Islands have never advanced to the finals of the FIFA World Cup or UEFA European Championship. They took part in the Island Games in 1989 and 1991 and they also took part in the Nordic Football Championship for the first time in 2000–01, the last time the competition was played. In the Faroe Islands the team is known as the landsliðið, home matches are played at Tórsvøllur. From 1930 to 1988, before international membership, the Faroe Islands only played friendly matches against Iceland, Shetland, Orkney Islands, Greenland. None of these fixtures were considered either by FIFA, nor the Faroe Islands Football Association. The Faroe Islands gained membership of FIFA on 2 July 1988, the first official victory was a 1–0 win, in a friendly against Canada in 1989. Faroe Islands participated in two Island Games, winning tournaments in 1989 and 1991. They never entered the tournament again, as the opponent teams were considered too weak a match for the Faroese side, Faroe Islands pulled one of the biggest upsets in footballing history when they beat Austria 1–0 in their first ever competitive international on 12 September 1990. The game, a Euro 92 qualifier, was played in Landskrona, Sweden, torkil Nielsen, a salesman for his local builders company scored the goal. Guðlaugsson pre-match speech goes, Think of the Faroese flag, take it with you on that field. Throw yourself into the tackles against those arrogant Austrians with one mission – to win the game for your nation, tonight you pay back your childhood home. You have the opportunity now and it is an irrepaple blow if you dont cease it, the win was against all odds and to this day, this is the story about Faroese football – and the story about sports in the Faroe Islands. American sports magazine Soccerphile rated the Faroese victory number 10 of all-time football greatest upsets, one month later the Faroe Islands lost 4–1 to Denmark at Parken, Copenhagen. The same team got another good result in the qualifying tournament, the Faroe Islands lost the remaining five matches of the tournament. Since Landskrona, Faroese football stepped up to the challenge, regurlarly getting good results against better teams, however, it was a surprise to many around Europe when Allan Simonsen in 1994 was appointed the new coach for the Faroese national team. Having had a career in Borussia Monchengladbach and F. C. Barcelona. Allan Simonsen was in charge of the Faroese team for seven years, among other things he asked the Football Association to lengthen the season, and also asked the clubs for fitter players
Faroe Islands national football team
–
Faroe Islands national football team in March 2013
Faroe Islands national football team
–
Faroe Islands playing against Italy on 2 September 2011. The match ended in a 1–0 defeat.
40.
Gundadalur
–
Gundadalur is the name of an area in Tórshavn, Faroe Islands. It is home to three different football pitches and other sports facilities, the largest one is the national stadium Tórsvøllur, a multi-use stadium. The actual Gundadalur Stadium is located just alongside Tórsvøllur, there are two sports halls in the same area. Høllin á Hálsi is the oldest one, built in 1970, the sports hall has been owned by Tórshavn Municipality since 2004. Gundadalshøllin is the sports hall, lying below and south of Høllin á Hálsi. Both sports halls are used for handball and volleyball, but also for other public events. Gundadalshøllin is owned by the handball clubs Neistin and Kyndil, there is also a swimming hall in Gundadalur that was built in 1984. It has one swimming pool which is 25 meters long with six lanes, there is a gymnastics venue inside a hall at the north-eastern side of Tórsvøllur, it is called Fimi and is owned by Tórshavn Municipality. Outside the western corner of the Gundadalur Stadium is a sportshall for badminton, north of the badminton hall is a tennis venue. Just outside the valley of Gundadalur is a venue for athletics, the Upper Field is the main field used for first level matches and is the home ground of HB and B36. It can also host the matches of other Faroese teams in the European competitions, the Lower Field, is mostly used for training and also lower level matches. Is the home ground of Giza/Hoyvík and Undrið FF
Gundadalur
–
Gundadalur
Gundadalur
–
Hoydalar, 18 July 1909: First known photo of a football match between two clubs of the Faroe Islands.
HB Tórshavn (white arms) won 3-1 over
TB Tvøroyri.
Gundadalur
–
View to Gundadalur and Hálsi, the sports area of
Tórshavn.
41.
Faroe Islands Premier League
–
The Faroe Islands Premier League is the top level of football in the Faroe Islands. It was founded in 2005, replacing 1, deild and it is organised by the Faroe Islands Football Association. The league is now called Effodeildin, from February 2009 to December 2011 was known as Vodafonedeildin and Formuladeildin from 2005 to 2008 for sponsorship reasons. The league will be called Effodeildin until 2017, all teams in the league have semi-professional status. It currently has 10 participating clubs, at the end of each season, two teams are relegated and two promoted from 1. Deild The league was founded in 1942, although clubs did not take part in European competition until 1992, in 2003 HB Tórshavn won the league and equalled KÍ Klaksvíks record of 17 titles, a year later HB bettered that and won the title for the 18th time. Deild was renamed Formuladeildin for sponsorship reasons, deild adopted the name of 1. Deild, the 3rd and 4th tier were named 2, then 5 years later in 2009, a 3-year deal was agreed with Vodafone and the name was changed again to Vodafonedeildin. In February 2012 the name was changed to Effodeildin, a 3-year deal was agreed with the Faroese petrol company Effo, the league renewed with Effo and will be called Effodeildin until 2017. ||07 Vestur || B36 || EB/Streymur || HB || ÍF || KÍ || NSÍ || Skála || TB || Vikingur || Source, Source, GÍ merged into Vikingur for 2008 Source, League at UEFA League at FSF League at Faroe Soccer
Faroe Islands Premier League
–
Faroe Islands Premier League (Effodeildin)
42.
FF Giza
–
Fótbóltsfelagið Giza was a Faroese football club based in the capital Tórshavn. The team plays its matches on Niðari Vøllur in Gundadalur. Earlier they played their matches in Argir. The club was founded 1 January 1968 as Nólsoyar Ítróttarfelag – often abbreviated to NÍF – representing the isle of Nólsoy, the club changed their name to FF Giza on 1 January 2010. Their hometown was also changed from Nólsoy to Tórshavn, in 2012 the two clubs FF Giza and FC Hoyvík merged into Giza/Hoyvík. Their best team played in 2 and they were number three, only the difference in goals kept them from getting promotion to 1. Deild, TB Tvøroyri and Giza/Hoyvík had 40 points, but TB Tvøroyri got promoted, note, Flags indicate national team as defined under FIFA eligibility rules. Players may hold more than one non-FIFA nationality, note, Flags indicate national team as defined under FIFA eligibility rules. Players may hold more than one non-FIFA nationality, starting from 2007, the club has annually named its player of the year. com
FF Giza
–
FF Giza
FF Giza
–
Giza/Hoyvík vs.
FC Suðuroy in 2. deild, 15 September 2012.
43.
Team handball
–
Handball is a team sport in which two teams of seven players each pass a ball using their hands with the aim of throwing it into the goal of the other team. A standard match consists of two periods of 30 minutes, and the team scores more goals wins. Modern handball is played on a court 40 by 20 metres, the goals are surrounded by a 6-meter zone where only the defending goalkeeper is allowed, goals must be scored by throwing the ball from outside the zone or while diving into it. The sport is played indoors, but outdoor variants exist in the forms of field handball and Czech handball. The game is fast and high-scoring, professional teams now typically score between 20 and 35 goals each, though lower scores were not uncommon until a few decades ago, body contact is permitted by the defenders trying to stop the attackers from approaching the goal. The game was codified at the end of the 19th century in northern Europe, the modern set of rules was published in 1917 in Germany, and had several revisions since. The first international games were played under rules for men in 1925. Mens handball was first played at the 1936 Summer Olympics in Berlin as outdoors, and the time at the 1972 Summer Olympics in Munich as indoors. Womens team handball was added at the 1976 Summer Olympics, the International Handball Federation was formed in 1946 and, as of 2016, has 197 member federations. The sport is most popular in the countries of continental Europe, in the womens world championships, only two non-European countries have won the title, South Korea and Brazil. The game also enjoys popularity in the Far East, North Africa, There is evidence of ancient Roman women playing a version of handball called expulsim ludere. There are records of games in medieval France, and among the Inuit in Greenland. By the 19th century, there existed similar games of håndbold from Denmark, házená in the Czech Republic, handbol in Ukraine, the team handball game of today was codified at the end of the 19th century in northern Europe—primarily in Denmark, Germany, Norway and Sweden. The first written set of team handball rules was published in 1906 by the Danish gym teacher, lieutenant and Olympic medalist Holger Nielsen from Ordrup grammar school, north of Copenhagen. The modern set of rules was published on 29 October 1917 by Max Heiser, Karl Schelenz, after 1919 these rules were improved by Karl Schelenz. The first international games were played under rules, between Germany and Belgium by men in 1925 and between Germany and Austria by women in 1930. In 1926, the Congress of the International Amateur Athletics Federation nominated a committee to draw up rules for field handball. The International Amateur Handball Federation was formed in 1928 and later the International Handball Federation was formed in 1946, Mens field handball was played at the 1936 Summer Olympics in Berlin
Team handball
–
Handball player moves towards the goal prior to throwing the ball, while the goalkeeper waits to stop it.
Team handball
–
Stamp depicting 1972 Olympics
Team handball
–
Team timeout.
Team handball
–
The referees (blue shirts) keep both teams between them.
44.
Neistin
–
Neistin is a Faroese handball club in Tórshavn, which was founded on 21 March 1931. Neistin has many different teams for men and women, boys and they have teams in the mens best division, which is named after the head sponsor which is Atlantic Airways, Atlantic Airways deildin. Neistin has also a team in the womens best division, Sunset deildin, in April 2011 both men and women won the best divisions in Faroese handball and became Fareose champions. It was the first time in 33 years that both teams of Neistin won the Faroese championship, the Faroe Islands Handball Cup has been arranged in the Faroe Islands since 1985 for the men and 1987 for the women. Neistin has won this competition several times, the womens team of Neistin has won the Faroe Islands Handball Cup 12 times,1987,1988,1989,1990,1992,1994,1995,1996,1997,1998,2006 and 2012. The mens team of Neistin has won the Faroe Islands Handball Cup 6 times,1992,1994,2009,2010,2011 and 2012. The mens team of Neistin has won the Faroese Championship in handball 8 times,1949,1953,1955,1978,2000,2008,2010 and 2011, from the Faroese magazine, Myndablaðið NÚ, nr
Neistin
–
The women's team of Neistin won the Faroe Islands Handball Cup 2013, also called the Coca-Cola Cup. Neistin won the final against
VB Vágur 27-24.
Neistin
–
Neistin won the Coca-Cola Cup 2013.
Neistin
–
Neistin playing the final in the Faroe Islands Cup 2013 against
VB Vágur. The players of Neistin on this photo: Marjun Danberg (10), Nicoleta Radu Hansen (75) and Ása Dam á Neystabø (3).
Neistin
–
Neistin's women's team in Sunsetdeildin in a match against
VB Vágur in Vágshøll, March 2011.
45.
Rowing (sport)
–
Rowing, often referred to as crew in the United States, is a sport with origins back to Ancient Egyptian times. It is based on propelling a boat on water using oars, by pushing against the water with an oar, a force is generated to move the boat. The sport can be recreational, where the focus is on learning the technique of rowing, or competitive. There are a number of different boat classes in which athletes compete, modern rowing as a competitive sport can be traced to the early 10th century when races were held between professional watermen on the River Thames in London, United Kingdom. Often prizes were offered by the London Guilds and Livery Companies, amateur competition began towards the end of the 18th century with the arrival of boat clubs at the British public schools of Eton College and Westminster School. Similarly, clubs were formed at the University of Oxford, with a race held between Brasenose College and Jesus College in 1815, at the University of Cambridge the first recorded races were in 1827. In 1843, the first American college rowing club was formed at Yale University, the International Rowing Federation, responsible for international governance of rowing, was founded in 1892 to provide regulation at a time when the sport was gaining popularity. Across six continents,150 countries now have rowing federations that participate in the sport, Rowing is one of the oldest Olympic sports. Though it was on the programme for the 1896 games, racing did not take due to bad weather. Womens rowing was added to the Olympic programme in 1976, today, only fourteen boat classes race at the Olympics, Each year the World Rowing Championships is staged by FISA with 22 boat classes raced. In Olympic years only the boat classes are raced at the World Championships. The European Rowing Championships are held annually, along with three World Rowing Cups in which each event earns a number of points for a country towards the World Cup title, since 2008, rowing has also been competed at the Paralympic Games. Many other competitions often exist for racing clubs, schools, and universities in each nation. While rowing, the athlete sits in the boat facing toward the stern and this may be done on a canal, river, lake, sea, or other large bodies of water. The sport requires strong core balance, physical strength, flexibility, whilst the action of rowing and equipment used remains fairly consistent throughout the world, there are many different types of competition. These include endurance races, time trials, stake racing, bumps racing, the many different formats are a result of the long history of the sport, its development in different regions of the world, and specific local requirements and restrictions. There are two forms of rowing, In sweep or sweep-oar rowing, each rower has one oar and this is generally done in pairs, fours, and eights. In some regions of the world, each rower in a boat is referred to either as port or starboard
Rowing (sport)
–
Eight classes of racing boats, six of which are part of the
Summer Olympic Games.
Rowing (sport)
–
Oars are held in an oarlock at the end of outriggers attached to the side of the boat
Rowing (sport)
–
For rowing as a method of transport or for recreation, see
Rowing. For other uses, see
Rowing (disambiguation).
Rowing (sport)
–
The finish of the
Doggett's Coat and Badge. Painting by
Thomas Rowlandson.
46.
Road bicycle race
–
Road bicycle racing is the cycle sport discipline of road cycling, held on paved roads. Road racing is the most popular form of bicycle racing, in terms of numbers of competitors, events. Professional racing has been most popular in Western Europe, centered historically on France, Spain, Italy, since the mid-1980s the sport has diversified with professional races now held on all continents of the globe. Semi-professional and amateur races are held in many countries. The sport is governed by the Union Cycliste Internationale, as well as the UCIs annual World Championships for men and women, the biggest event is the Tour de France, a three-week race that can attract over 500,000 roadside supporters a day. Road bicycle racing began as a sport in 1868. The first world championship was in 1893 and cycling has been part of the Olympic Games since the sequence started in Athens in 1896. Road racing in its modern form originated in the late 19th century, the sport was popular in the western European countries of France, Spain, Belgium, and Italy. Some of Europes earliest road bicycle races remain among the sports biggest events and these early races include Liège–Bastogne–Liège, Paris–Roubaix, the Tour de France, the Milan–San Remo and Giro di Lombardia, the Giro dItalia, the Volta a Catalunya, and the Tour of Flanders. They provided a template for other races around the world, while the sport has spread throughout the world, these historic races remain the most prestigious for a cyclist to win. Single-day race distances may be as long as 150 miles, races over short circuits, often in town or city centres, are known as criteriums. Individual time trial is an event in which cyclists race alone against the clock on flat or rolling terrain, a team time trial, including two-man team time trial, is a road-based bicycle race in which teams of cyclists race against the clock. In both team and individual time trials, the start the race at different times so that each start is fair. Race distances vary from a few km to between approximately 20 miles and 60 miles, stage races consist of several races, or stages, ridden consecutively. The competitor with the lowest cumulative time to all stages is declared the overall, or general classification. Stage races may also have other classifications and awards, such as stage winners, the points classification winner. A stage race can also be a series of road races, the stage winner is the first person to cross the finish line that day or the time trial rider with the lowest time on the course. The overall winner of a race is the rider who takes the lowest aggregate time to complete all stages
Road bicycle race
–
A breakaway of three riders during the
women's road race at the
2012 Summer Olympics
Road bicycle race
–
The Tour of Gippsland – a stage race in Australia– climbing through the scenic area of the Omeo Shire
Road bicycle race
–
Cyclists
drafting behind one another, forming a paceline
Road bicycle race
–
GT:
1991 Giro d'Italia.
47.
Transport in the Faroe Islands
–
The Faroe Islands is served by an internal transport system based on roads, ferries, and helicopters. International transport, both for passengers and freight, remains difficult due to costs, low traffic, long distances. Exporting domestically produced goods is thus expensive, this limits the development of a commodity-based economy, the second period commenced in the late-19th century, when ferry connections began to emerge. The ferries were largely private initiatives, but they came to be operated by the public sector. This was supplemented by a culture of automobiles. After World War II, a part of the Faroe Islands was accessible via ferries and automobiles, private buses. The third period was characterized by modernization, the introduction of the car ferry made it possible to drive between the large centres of the country. It became possible to drive from the capital Tórshavn to Vágur and Tvøroyri in the south, to Fuglafjørður and Klaksvík in the north, Vágar Airport was built by the British during World War II, it was reopened as a civilian international airport in 1963. Additionally, the network was further developed. Tunnels to distant valleys and firths such as Hvalba, Sandvík, the fourth period saw the emergence of a mainland thanks to tunnels and bridges. In 1973 the first bridge between two islands was established between Norðskáli on Eysturoy and Nesvík on Streymoy, in 1976 the new tunnel between Norðskáli and Eysturoy was completed, the Faroes two largest islands were connected into what is now referred to as Meginlandið, the Mainland. The newest developments of the Faroese transportation network are the sub-sea tunnels, in 2002 the tunnel between Streymoy and Vágar—the latter is the airport island—was finished, and in 2006 the Norðoyatunnilin between Eysturoy and Borðoy was finished. A toll, payable at petrol stations, of 170 DKK is charged to drive through two tunnels, the others are free. Now more than 85% of the Faroese population is accessible by automobile, the combined cost of the project is estimated at almost 2 billion DKK, and will be the most expensive construction project in Faroese history. Eysturoyartunnilin is intended to have a roundabout under the sea, the three tubes will be 7,1 km,2,1 km and 1,8 km long joined together by the roundabout. Sandoyartunnilin will be 10,6 km long, there have been talks about a possible tunnel between Sandoy and Suðuroy. The tunnel would be around 20–25 km long, if completed this would mean that 99% of the Faroes would be connected by road. There are no railways on the Faroe Islands due to the landscape, small population
Transport in the Faroe Islands
–
Ferries of
Strandfaraskip Landsins, with the new vessel
Smyril on the left
Transport in the Faroe Islands
–
Entrance to the Norðoyatunnilin at Leirvík
Transport in the Faroe Islands
–
"Light Art" inside the Norðoyatunnilin
Transport in the Faroe Islands
–
The Norröna of Smyril Line at Tórshavn in 1997. This vessel has since been replaced by the new Norröna.
48.
Smyril Line
–
Smyril Line is a Faroese shipping company, linking the Faroe Islands with Denmark and Iceland, previously, it also served Norway and the United Kingdom. Smyril is the Faroese word for the merlin, since 1983, the company has operated a regular international passenger, car and freight service using a large, modern, multi-purpose ferry named MV Norröna. The original vessel was a Swedish-built ferry formerly named Gustav Vasa and this was replaced by the Norröna, built in Lübeck, Germany in 2003. The large purchase price, some €100 million, gave the financial difficulties. The onwards journey to Seyðisfjörður takes another 15 hours excluding a layover in Tórshavn, until the end of the Summer 2007 timetable Smyril Line also served Lerwick in the Shetland Islands. On 11 November 2008 Smyril Line announced that it would end services to Scrabster, Scotland and Bergen, on 1 September Smyril Line announced that it would end services to Hanstholm and Esbjerg in Denmark and move all its Danish ferry operations to Hirtshals
Smyril Line
–
The old Norröna in
Tórshavn Harbour, 1997
Smyril Line
–
Smyril Line
Smyril Line
Smyril Line
Kingdom of Denmark
Faroe Islands
Tórshavn Municipality
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Asker, Norway
Garðabær, Iceland
Jakobstad, Finland
Mariehamn, Åland[16]
Eslöv, Sweden
Birkerød, Denmark
Riolunato, Italy
Tórshavn travel guide from Wikivoyage
