1.
Geographic coordinate system
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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
2.
Norway
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The Antarctic Peter I Island and the sub-Antarctic Bouvet Island are dependent territories and thus not considered part of the Kingdom. Norway also lays claim to a section of Antarctica known as Queen Maud Land, until 1814, the kingdom included the Faroe Islands, Greenland, and Iceland. It also included Isle of Man until 1266, Shetland and Orkney until 1468, Norway has a total area of 385,252 square kilometres and a population of 5,258,317. The country shares a long border with Sweden. Norway is bordered by Finland and Russia to the north-east, Norway has an extensive coastline, facing the North Atlantic Ocean and the Barents Sea. King Harald V of the Dano-German House of Glücksburg is the current King of Norway, erna Solberg became Prime Minister in 2013, replacing Jens Stoltenberg. A constitutional monarchy, Norway divides state power between the Parliament, the Cabinet and the Supreme Court, as determined by the 1814 Constitution, the kingdom is established as a merger of several petty kingdoms. By the traditional count from the year 872, the kingdom has existed continuously for 1,144 years, Norway has both administrative and political subdivisions on two levels, counties and municipalities. The Sámi people have an amount of self-determination and influence over traditional territories through the Sámi Parliament. Norway maintains close ties with the European Union and the United States, the country maintains a combination of market economy and a Nordic welfare model with universal health care and a comprehensive social security system. Norway has extensive reserves of petroleum, natural gas, minerals, lumber, seafood, the petroleum industry accounts for around a quarter of the countrys gross domestic product. On a per-capita basis, Norway is the worlds largest producer of oil, the country has the fourth-highest per capita income in the world on the World Bank and IMF lists. On the CIAs GDP per capita list which includes territories and some regions, from 2001 to 2006, and then again from 2009 to 2017, Norway had the highest Human Development Index ranking in the world. It also has the highest inequality-adjusted ranking, Norway ranks first on the World Happiness Report, the OECD Better Life Index, the Index of Public Integrity and the Democracy Index. Norway has two names, Noreg in Nynorsk and Norge in Bokmål. The name Norway comes from the Old English word Norðrveg mentioned in 880, meaning way or way leading to the north. In contrasting with suðrvegar southern way for Germany, and austrvegr eastern way for the Baltic, the Anglo-Saxon of Britain also referred to the kingdom of Norway in 880 as Norðmanna land. This was the area of Harald Fairhair, the first king of Norway, and because of him
3.
Counties of Norway
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Norway is divided into 19 administrative regions, called counties, until 1918, they were known as amter. The counties form the first-level subdivisions of Norway and are divided into 428 municipalities. Svalbard and Jan Mayen are outside the county division and ruled directly on national level, the capital Oslo is considered both a county and a municipality. In 2017 the government decided to abolish the current counties and to them with fewer, larger administrative regions. Below is a list of the Norwegian counties as they have been since 1919, note that the counties are administered both by appointees of the national government and to a lesser extent by their own elected bodies. The county numbers are from the numbering system ISO 3166-2, NO. The number 13 was dropped from the system when the city of Bergen was merged into Hordaland in 1972, from the consolidation to a single kingdom, Norway was divided into a number of geographic regions that had its own legislative assembly or Thing, such as Gulating and Frostating. The second-order subdivision of these regions was into fylker, such as Egdafylke and Hordafylke, in 1914, the historical term fylke was brought into use again to replace the term amt introduced during the union with Denmark. Current day counties often, but not necessarily, correspond to the historical areas. Finnmark, the Faroe Islands, the Orkney Islands, Shetland, the Hebrides, Isle of Man, Iceland and Greenland were Norwegian skattland, from the end of the 12th century, Norway was divided into several syssel. The head of the various syssel was the syslemann, who represented the king locally, the following shows a reconstruction of the different syssel in Norway c. 1300, including sub-syssel where these seem established, from 1308, the term len in Norway signified an administrative region roughly equivalent to todays counties. The historic len was an important administrative entity during the period of Dano-Norwegian unification after their amalgamation as one state, which lasted for the period 1536–1814. At the beginning of the 16th century the political divisions were variable, up to 1660 the four principal len were headquartered at the major fortresses Bohus Fortress, Akershus Fortress, Bergenhus Fortress and the fortified city of Trondheim. The sub-regions corresponded to the districts for the Lutheran church in Norway. Båhus len Akershus len Trondheim len Bergenhus len These four principal len were in the 1530s divided into approximately 30 smaller regions. From that point forward through the beginning of the 17th century the number of subsidiary len was reduced, from 1660 Norway had nine principal len comprising 17 subsidiary len, Len written as län continues to be used as the administrative equivalent of county in Sweden to this day. Each len was governed by a lenman, with the royal decree of February 19,1662, each len was designated an amt and the lenmann was titled amtmann, from German Amt, reflecting the bias of the Danish court of that period
4.
Districts of Norway
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The country Norway is historically divided into a number of districts. Many districts have deep roots, and only partially coincide with todays administrative units of counties and municipalities. The districts are defined by geographical features, often valleys, mountain ranges, fjords, plains, or coastlines, many such regions were petty kingdoms up to the early Viking age. A high percentage of Norwegians identify themselves more by the district live in or come from. Thus, dialects and regional commonality in folk culture tended to correspond to those same geographical units, the construction of railroads between distant parts of the country. The opening of dozens of new airports all over the country through the 1960s and 1970s, the release of private cars from government rationing and import restrictions from the 1950s onwards. A concrete display of the Norwegian habit of identifying themselves by district can be seen in the many regional costumes, called bunad, the following list is non-exhaustive and partially overlapping. The first name is the name in Bokmål, the second Nynorsk, helgeland Lofoten Ofoten Salten Vesterålen See also Finnmark, Hålogaland and Troms
5.
Centre Party (Norway)
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The Centre Party is an agrarian centrist political party in Norway. From its founding until 2000, the party joined only governments not led by the Labour Party, governments headed by prime ministers from the party include the short-lived Kolstad and Hundseids Cabinet between 1931 and 1933, and the longer-lasting Bortens Cabinet from 1965 until 1971. The party was founded at the convention of the Norsk Landmandsforbund during 17 to 19 June 1920. In 1922 the association was renamed to the Norwegian Agrarian Association, during the eight decades since the Centre Party was created as a political faction of a Norwegian agrarian organisation, the party has changed a great deal. The 1930s have in the post-war era been seen as a time in the partys history. This is partly because Vidkun Quisling, who became leader of Nasjonal Samling, was Minister of Defence in the Farmers Party Kolstad. Quisling was however not a member of the Farmers Party, while there were fascist sympaties among parts of the Farmers Partys electorate, the Farmers Party itself never supported fascism. It was after all the Farmers Party that enabled the first stable Labour cabinet in Norway, in 1935, they reached a compromise with the Labour Party, which led to the Nygaardsvold Cabinet. In addition, the Farmers Party was represented in the cabinet by Anders Fjeldstad. Political scientist Trond Nordby in 2009 also said that the Farmers Party has been given a bad reputation from this time. In 1959 the party changed their name to the Norwegian Democratic Party — Democrats, in June 1959 the name was changed to the current Centre Party. This happened out of the need to attract an additional electorate with the decline of the agrarian share of the population. The partys membership peaked at 70,000 in 1971. In local elections, the party enjoys strong support in small municipalities. After the 2007 elections,83 of the mayors in Norway represent the Centre Party, only the Labour Party has more mayors, and relative to party size, the Centre Party has more mayors than any other. The Centre Party had been a part of only non-socialist coalition governments from 1930 to 2000, in seven governments and these negotiations succeeded and the Centre Party entered the Second Stoltenberg Cabinet on 17 October 2005 with four ministers. The Red-Greens were re-elected to government in the 2009 election and it has been argued that the partys ideology has moved more towards social democracy in recent years. This included increased duties of 429% on lamb, 344% on beef, the party is known in Norway for their support of high toll tariffs on foreign cheese and meat, called toll protection, and their proposal to shoot all wolves in Norway
6.
Demonym
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A demonym is a word that identifies residents or natives of a particular place, which is derived from the name of that particular place. It is a neologism, previously gentilic was recorded in English dictionaries, e. g. the Oxford English Dictionary, thus a Thai may be any resident or citizen of Thailand, of any ethnic group, or more narrowly a member of the Thai people. Conversely, some groups of people may be associated with multiple demonyms, for example, a native of the United Kingdom may be called a British person, a Brit, or a Briton. In some languages, when a parallel demonym does not exist, in English, demonyms are capitalized and are often the same as the adjectival form of the place, e. g. Egyptian, Japanese, or Greek. Significant exceptions exist, for instance the adjectival form of Spain is Spanish, English widely includes country-level demonyms such as Ethiopian or Guatemalan and more local demonyms such as Seoulite, Wisconsinite, Chicagoan, Michigander, Fluminense, and Paulista. Some places lack a commonly used and accepted demonym and this poses a particular challenge to those toponymists who research demonyms. The word gentilic comes from the Latin gentilis and the English suffix -ic, the word demonym was derived from the Greek word meaning populace with the suffix for name. National Geographic attributes the term demonym to Merriam-Webster editor Paul Dickson in a recent work from 1990 and it was subsequently popularized in this sense in 1997 by Dickson in his book Labels for Locals. However, in What Do You Call a Person From, a Dictionary of Resident Names attributed the term to George H. Scheetz, in his Names Names, A Descriptive and Prescriptive Onymicon, which is apparently where the term first appears. Several linguistic elements are used to create demonyms in the English language, the most common is to add a suffix to the end of the location name, slightly modified in some instances. Cairo → Cairene Cyrenaica → Cyrene Damascus → Damascene Greece → Greek Nazareth → Nazarene Slovenia → Slovene Often used for Middle Eastern locations and European locations. Kingston-upon-Hull → Hullensian Leeds → Leodensian Spain → Spaniard Savoy → Savoyard -ese is usually considered proper only as an adjective, thus, a Chinese person is used rather than a Chinese. Monaco → Monégasque Menton → Mentonasque Basque Country → Basque Often used for French locations, mostly they are from Africa and the Pacific, and are not generally known or used outside the country concerned. In much of East Africa, a person of an ethnic group will be denoted by a prefix. For example, a person of the Luba people would be a Muluba, the plural form Baluba, similar patterns with minor variations in the prefixes exist throughout on a tribal level. And Fijians who are indigenous Fijians are known as Kaiviti and these demonyms are usually more informal and colloquial. In the United States such informal demonyms frequently become associated with mascots of the sports teams of the state university system. In other countries the origins are often disputed and these will typically be formed using the standard models above
7.
Daylight saving time
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Daylight saving time is the practice of advancing clocks during summer months by one hour so that evening daylight lasts an hour longer, while sacrificing normal sunrise times. Typically, regions that use Daylight Savings Time adjust clocks forward one hour close to the start of spring, American inventor and politician Benjamin Franklin proposed a form of daylight time in 1784. New Zealander George Hudson proposed the idea of saving in 1895. The German Empire and Austria-Hungary organized the first nationwide implementation, starting on April 30,1916, many countries have used it at various times since then, particularly since the energy crisis of the 1970s. The practice has both advocates and critics, DST clock shifts sometimes complicate timekeeping and can disrupt travel, billing, record keeping, medical devices, heavy equipment, and sleep patterns. Computer software often adjusts clocks automatically, but policy changes by various jurisdictions of DST dates, industrialized societies generally follow a clock-based schedule for daily activities that do not change throughout the course of the year. The time of day that individuals begin and end work or school, North and south of the tropics daylight lasts longer in summer and shorter in winter, with the effect becoming greater as one moves away from the tropics. However, they will have one hour of daylight at the start of each day. Supporters have also argued that DST decreases energy consumption by reducing the need for lighting and heating, DST is also of little use for locations near the equator, because these regions see only a small variation in daylight in the course of the year. After ancient times, equal-length civil hours eventually supplanted unequal, so civil time no longer varies by season, unequal hours are still used in a few traditional settings, such as some monasteries of Mount Athos and all Jewish ceremonies. This 1784 satire proposed taxing window shutters, rationing candles, and waking the public by ringing church bells, despite common misconception, Franklin did not actually propose DST, 18th-century Europe did not even keep precise schedules. However, this changed as rail transport and communication networks came to require a standardization of time unknown in Franklins day. Modern DST was first proposed by the New Zealand entomologist George Hudson, whose shift work job gave him time to collect insects. An avid golfer, he also disliked cutting short his round at dusk and his solution was to advance the clock during the summer months, a proposal he published two years later. The proposal was taken up by the Liberal Member of Parliament Robert Pearce, a select committee was set up to examine the issue, but Pearces bill did not become law, and several other bills failed in the following years. Willett lobbied for the proposal in the UK until his death in 1915, william Sword Frost, mayor of Orillia, Ontario, introduced daylight saving time in the municipality during his tenure from 1911 to 1912. Starting on April 30,1916, the German Empire and its World War I ally Austria-Hungary were the first to use DST as a way to conserve coal during wartime, Britain, most of its allies, and many European neutrals soon followed suit. Russia and a few other countries waited until the year
8.
Central European Summer Time
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It corresponds to UTC + two hours. Other names which have been applied to Central European Summer Time are Middle European Summer Time, Central European Daylight Saving Time, and Bravo Time. Since 1996 European Summer Time has been observed between 1,00 UTC on the last Sunday of March and 1,00 on the last Sunday of October, the following countries and territories use Central European Summer Time. In addition, Libya used CEST during the years 1951–1959, 1982–1989, 1996–1997, European Summer Time Other countries and territories in UTC+2 time zone Other names of UTC+2 time zone
9.
Norwegian language
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Norwegian is a North Germanic language spoken mainly in Norway, where it is the official language. Along with Swedish and Danish, Norwegian forms a continuum of more or less mutually intelligible local and regional variants. These Scandinavian languages, together with Faroese and Icelandic as well as extinct languages. Faroese and Icelandic are hardly mutually intelligible with Norwegian in their spoken form because continental Scandinavian has diverged from them, as established by law and governmental policy, the two official forms of written Norwegian are Bokmål and Nynorsk. The official Norwegian Language Council is responsible for regulating the two forms, and recommends the terms Norwegian Bokmål and Norwegian Nynorsk in English. Two other written forms without official status also exist, one and it is regulated by the unofficial Norwegian Academy, which translates the name as Standard Norwegian. Nynorsk and Bokmål provide standards for how to write Norwegian, no standard of spoken Norwegian is officially sanctioned, and most Norwegians speak their own dialects in all circumstances. Thus, unlike in other countries, the use of any Norwegian dialect. Outside Eastern Norway, this variation is not used. From the 16th to the 19th centuries, Danish was the written language of Norway. As a result, the development of modern written Norwegian has been subject to strong controversy related to nationalism, rural versus urban discourse, historically, Bokmål is a Norwegianised variety of Danish, while Nynorsk is a language form based on Norwegian dialects and puristic opposition to Danish. The unofficial form known as Riksmål is considered more conservative than Bokmål, Norwegians are educated in both Bokmål and Nynorsk. A2005 poll indicates that 86. 3% use primarily Bokmål as their written language,5. 5% use both Bokmål and Nynorsk, and 7. 5% use primarily Nynorsk. Thus, 13% are frequently writing Nynorsk, though the majority speak dialects that resemble Nynorsk more closely than Bokmål. Broadly speaking, Nynorsk writing is widespread in western Norway, though not in major urban areas, examples are Setesdal, the western part of Telemark county and several municipalities in Hallingdal, Valdres, and Gudbrandsdalen. It is little used elsewhere, but 30–40 years ago, it also had strongholds in rural parts of Trøndelag. Today, not only is Nynorsk the official language of four of the 19 Norwegian counties, NRK, the Norwegian broadcasting corporation, broadcasts in both Bokmål and Nynorsk, and all governmental agencies are required to support both written languages. Bokmål is used in 92% of all publications, and Nynorsk in 8%
10.
Population density
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Population density is a measurement of population per unit area or unit volume, it is a quantity of type number density. It is frequently applied to living organisms, and most of the time to humans and it is a key geographical term. Population density is population divided by land area or water volume. Low densities may cause a vortex and lead to further reduced fertility. This is called the Allee effect after the scientist who identified it, commonly this may be calculated for a county, city, country, another territory, or the entire world. The worlds population is around 7,000,000,000, therefore, the worldwide human population density is around 7,000,000,000 ÷510,000,000 =13.7 per km2. If only the Earths land area of 150,000,000 km2 is taken into account and this includes all continental and island land area, including Antarctica. If Antarctica is also excluded, then population density rises to over 50 people per km2, thus, this number by itself does not give any helpful measurement of human population density. Several of the most densely populated territories in the world are city-states, microstates, cities with high population densities are, by some, considered to be overpopulated, though this will depend on factors like quality of housing and infrastructure and access to resources. Most of the most densely populated cities are in Southeast Asia, though Cairo, for instance, Milwaukee has a greater population density when just the inner city is measured, and the surrounding suburbs excluded. Arithmetic density, The total number of people / area of land, physiological density, The total population / area of arable land. Agricultural density, The total rural population / area of arable land, residential density, The number of people living in an urban area / area of residential land. Urban density, The number of people inhabiting an urban area / total area of urban land, ecological optimum, The density of population that can be supported by the natural resources. S. States by population density Selected Current and Historic City, Ward & Neighborhood Density
11.
Old Norse
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Old Norse was a North Germanic language that was spoken by inhabitants of Scandinavia and inhabitants of their overseas settlements during about the 9th to 13th centuries. These dates, however, are not absolute, since written Old Norse is found well into the 15th century, Old Norse was divided into three dialects, Old West Norse, Old East Norse and Old Gutnish. Old West and East Norse formed a continuum, with no clear geographical boundary between them. For example, Old East Norse traits were found in eastern Norway, although Old Norwegian is classified as Old West Norse, most speakers spoke Old East Norse in what is present day Denmark and Sweden. Old Gutnish, the more obscure dialectal branch, is included in the Old East Norse dialect due to geographical associations. It developed its own features and shared in changes to both other branches. The 12th century Icelandic Gray Goose Laws state that Swedes, Norwegians, Icelanders and Danes spoke the same language, another term used, used especially commonly with reference to West Norse, was norrœnt mál. In some instances the term Old Norse refers specifically to Old West Norse, the Old East Norse dialect was spoken in Denmark, Sweden, settlements in Kievan Rus, eastern England, and Danish settlements in Normandy. The Old Gutnish dialect was spoken in Gotland and in settlements in the East. In the 11th century, Old Norse was the most widely spoken European language, in Kievan Rus, it survived the longest in Veliky Novgorod, probably lasting into the 13th century there. Norwegian is descended from Old West Norse, but over the centuries it has heavily influenced by East Norse. Old Norse also had an influence on English dialects and Lowland Scots and it also influenced the development of the Norman language, and through it and to a smaller extent, that of modern French. Various other languages, which are not closely related, have heavily influenced by Norse, particularly the Norman dialects, Scottish Gaelic. The current Finnish and Estonian words for Sweden are Ruotsi and Rootsi, of the modern languages, Icelandic is the closest to Old Norse. Written modern Icelandic derives from the Old Norse phonemic writing system, contemporary Icelandic-speakers can read Old Norse, which varies slightly in spelling as well as semantics and word order. However, pronunciation, particularly of the phonemes, has changed at least as much as in the other North Germanic languages. Faroese retains many similarities but is influenced by Danish, Norwegian, although Swedish, Danish and the Norwegian languages have diverged the most, they still retain asymmetric mutual intelligibility. Speakers of modern Swedish, Norwegian and Danish can mostly understand each other without studying their neighboring languages, the languages are also sufficiently similar in writing that they can mostly be understood across borders
12.
Valley
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A valley is a low area between hills, often with a river running through it. In geology, a valley or dale is a depression that is longer than it is wide, the terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of two main types or a mixture of them, with respect to the cross section of the slopes or hillsides. A valley in its broadest geographic sense is known as a dale. A valley through which a river runs may also be referred to as a vale, a small, secluded, and often wooded valley is known as a dell or in Scotland as a glen. A wide, flat valley through which a river runs is known in Scotland as a strath, a mountain cove is a small valley, closed at one or both ends, in the central or southern Appalachian Mountains which sometimes results from the erosion of a geologic window. A small valley surrounded by mountains or ridges is sometimes known as a hollow, a deep, narrow valley is known as a cwm. Similar geological structures, such as canyons, ravines, gorges, gullies, chines, a valley formed by erosion is called an erosional valley, a valley formed by geologic events such as drop faults or the rise of highlands is called a structural valley. A valley formed by flowing water, or river valley, is usually V-shaped, the exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls, shallower slopes may produce broader and gentler valleys. However, in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment, in prehistory, the rivers were used as a source of fresh water and food, as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, most of the first civilizations developed from these river valley communities. In geography, a vale is a river valley, usually with a particularly wide flood plain or flat valley bottom. In Southern England, vales commonly occur between the escarpment slopes of pairs of chalk formations, where the dome has been eroded, exposing less resistant underlying rock. Rift valleys, such as the Albertine Rift, are formed by the expansion of the Earths crust due to tectonic activity beneath the Earths surface, there are various forms of valley associated with glaciation that may be referred to as glacial valleys. A valley carved by glaciers is normally U-shaped, the valley becomes visible upon the recession of the glacier that forms it. When the ice recedes or thaws, the remains, often littered with small boulders that were transported within the ice. Floor gradient does not affect the shape, it is the glaciers size that does
13.
Ditch
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A ditch is a small to moderate depression created to channel water. A ditch can be used for drainage, to water from low-lying areas, alongside roadways or fields. A trench is a narrow ditch. Ditches are commonly seen around farmland, especially in areas that have required drainage, such as The Fens in eastern England and much of the Netherlands. Roadside ditches may provide a hazard to motorists and cyclists, whose vehicles may crash into them and get damaged, flipped over or stuck, especially in weather conditions. In Anglo-Saxon, the word dïc already existed and was pronounced deek in northern England, the origins of the word lie in digging a trench and forming the upcast soil into a bank alongside it. This practice has meant that the name dïc was given to either the excavation or the bank, thus Offas Dyke is a combined structure and Car Dyke is a trench, though it once had raised banks as well. In the midlands and north of England, a dike is what a ditch is in the south, a property boundary marker or small drainage channel. Where it carries a stream, it may be called a dike as in Rippingale Running Dike. The Weir Dike is a dike in Bourne North Fen, near Twenty. Drainage ditches play major roles in agriculture throughout the world, improper drainage systems accelerate water contamination, excessively desiccate soils during seasonal drought, and become a financial burden to maintain. Industrial earth-moving equipment facilitates maintenance of straight drainage trenches, but entrenchment results in increasing environmental, sustainable channel design can result in ditches that are largely self-maintaining due to natural geomorphological equilibrium. Slowed net siltation and erosion result in net reduction in sediment transport, flooding can be a major cause of recurring crop loss—particularly in heavy soils—and can severely disrupt urban economies as well. However, excess drainage results in recurring drought induced crop yield losses, controlled subsurface drainage from sensitive areas to vegetated drainage ditches makes possible a better balance between water drainage and water retention needs. The initial investment allows a community to draw down local water tables when, particularly in Colorado, the term ditch is also applied to open aqueducts that traverse hillsides as part of transbasin diversion projects. Examples include the Grand Ditch over La Poudre Pass, the Berthoud Pass Ditch, black Beach, The Mucklands of Canastota, New York
14.
Gully
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A gully is a landform created by running water, eroding sharply into soil, typically on a hillside. Gullies resemble large ditches or small valleys, but are metres to tens of metres in depth and width, when the gully formation is in process, the water flow rate can be substantial, causing a significant deep cutting action into soil. The earliest known usage of the term is from 1657 and it originates from the French word goulet, a diminutive form of goule which means throat. It is possible that the term was derived from a type of knife at the time, gullying or gully erosion is the process by which gullies are formed. Hillsides are more prone to gullying when they are cleared of vegetation, through deforestation, the eroded soil is easily carried by the flowing water after being dislodged from the ground, normally when rainfall falls during short, intense storms such as during thunderstorms. A gully may grow in length by means of erosion at a knick point. This erosion can result from interflow as well as surface runoff, gullies reduce the productivity of farmland where they incise into the land, and produce sediment that may clog downstream waterbodies. Because of this, much effort is invested into the study of gullies within the scope of geomorphology, in the prevention of gully erosion, the total soil loss from gully formation and subsequent downstream river sedimentation can be sizeable. Gullies can be formed or enlarged by a number of human activities, artificial gullies are formed during hydraulic mining when jets or streams of water are projected onto soft alluvial deposits to extract gold or tin ore. The remains of mining methods are very visible landform features in old goldfields such as in California. The badlands at Las Medulas for example, were created during the Roman period by hushing or hydraulic mining of the gold-rich alluvium with water supplied by numerous aqueducts tapping nearby rivers, each aqueduct produced large gullies below by erosion of the soft deposits. The effluvium was carefully washed with smaller streams of water to extract the nuggets, gullies are widespread at mid- to high latitudes on the surface of Mars, and are some of the youngest features observed on that planet, probably forming within the last few 100,000 years. Flow as springs from deeper seated liquid water aquifers in the subsurface is also a possible explanation for the formation of some Martian gullies. Arroyo Coulee Couloir Canyon Gulch Ravine Wadi Lavaka Badlands Rill Oxford English Dictionary
15.
Coat of arms
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A coat of arms is an heraldic visual design on an escutcheon, surcoat, or tabard. The coat of arms on an escutcheon forms the central element of the heraldic achievement which in its whole consists of shield, supporters, crest. A coat of arms is traditionally unique to a person, family, state. The ancient Romans used similar insignia on their shields, but these identified military units rather than individuals, the first evidence of medieval coats of arms has been attributed to the 11th century Bayeux Tapestry in which some of the combatants carry shields painted with crosses. However, that heraldic interpretation remains controversial, coats of arms came into general use by feudal lords and knights in battle in the 12th century. By the 13th century, arms had spread beyond their initial battlefield use to become a flag or emblem for families in the social classes of Europe. Exactly who had a right to use arms, by law or social convention, in the German-speaking regions both the aristocracy and burghers used arms, while in most of the rest of Europe they were limited to the aristocracy. The use of spread to the clergy, to towns as civic identifiers. Flags developed from coats of arms, and the arts of vexillology, the coats of arms granted to commercial companies are a major source of the modern logo. Despite no widespread regulation, heraldry has remained consistent across Europe, some nations, like England and Scotland, still maintain the same heraldic authorities which have traditionally granted and regulated arms for centuries and continue to do so in the present day. In England, for example, the granting of arms is and has controlled by the College of Arms. Unlike seals and other emblems, heraldic achievements have a formal description called a blazon. Many societies exist that also aid in the design and registration of personal arms, in the heraldic traditions of England and Scotland, an individual, rather than a family, had a coat of arms. In those traditions coats of arms are legal property transmitted from father to son, wives, undifferenced arms are used only by one person at any given time. Other descendants of the bearer could bear the ancestral arms only with some difference. One such charge is the label, which in British usage is now always the mark of an apparent or an heir presumptive. Because of their importance in identification, particularly in seals on legal documents and this has been carried out by heralds and the study of coats of arms is therefore called heraldry. In time, the use of arms spread from military entities to educational institutes, the author Helen Stuart argues that some coats of arms were a form of corporate logo
16.
Willow ptarmigan
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The willow ptarmigan is a bird in the grouse subfamily Tetraoninae of the pheasant family Phasianidae. It is also known as the willow grouse and in Ireland and Britain and it is the state bird of Alaska. In the summer the birds are brown, with dappled plumage. The species has remained little changed from the bird that roamed the tundra during the Pleistocene, nesting takes place in the spring when clutches of four to ten eggs are laid in a scrape on the ground. The chicks are precocial and soon leave the nest and while they are young, the willow ptarmigan is a medium to large ground-dwelling bird and is the most numerous of the three species of ptarmigan. Males and females are about the size, the adult length varying between 35 and 44 centimetres with a wingspan ranging from 60 and 65 centimetres. The weight is 430 to 810 grams and it is deep-chested and has a fairly long neck, a broad bill, short feathered legs and a moderately short rounded tail. In the summer, the plumage is marbled brown, with a reddish hue to the neck and breast. It has two inconspicuous wattles above the eyes, which red and prominent in the breeding season. The female is similar in appearance but lacks the wattles and has brown feathers scattered among the feathers on the belly. During winter, the plumage of both sexes becomes completely white, except for black feathers in the tail. The summer plumage is browner and in the winter, the willow ptarmigan lacks the rock ptarmigans black stripe between the eyes and bill. The white-tailed ptarmigan in North America is smaller, has a tail and finely-barred greyer plumage. The distinctive British Isles subspecies L. l. scoticus was once considered a separate true British species but is now classified as a sub-species and this moorland bird is reddish brown all over, except for its white feet. The voice is low-pitched and guttural and includes chuckles, repeated clucking sounds, when displaying, the male makes rattles and barking noises. The willow ptarmigans scientific name, Lagopus lagopus is derived from Ancient Greek lagos hare + pous foot, nineteen subspecies have been recognised though some are believed not to be valid. Most differ little in appearance, though the red grouse is rather distinct, during the Pleistocene, the willow ptarmigan widely occurred in continental Europe. Authors who recognize paleosubspecies have named the Pleistocene willow ptarmigan L. l. noaillensis and these marginally different birds are said to have gradually changed from the earlier Lagopus atavus into the present-day species L. lagopus
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Hunting
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Hunting is the practice of killing or trapping animals, or pursuing or tracking them with the intent of doing so. Hunting wildlife or feral animals is most commonly done by humans for food, recreation, to predators that are dangerous to humans or domestic animals. Lawful hunting is distinguished from poaching, which is the killing, trapping or capture of the hunted species. The species that are hunted are referred to as game or prey and are usually mammals, Hunting can also be a means of pest control. However, hunting has also contributed to the endangerment, extirpation and extinction of many animals. The pursuit, capture and release, or capture for food of fish is called fishing, the practice of foraging or gathering materials from plants and mushrooms is also considered separate from hunting. The word hunt serves as both a noun and a verb, the noun has been dated to the early 12th century, act of chasing game, from the verb hunt. The meaning of a body of persons associated for the purpose of hunting with a pack of hounds is first recorded in the 1570s, meaning the act of searching for someone or something is from about 1600. The verb, Old English huntian to chase game, perhaps developed from hunta hunter, is related to hentan to seize, from Proto-Germanic huntojan, the general sense of search diligently is first recorded c. Hunting has a history and may well pre-date the rise of the species Homo sapiens. Evidence from western Kenya suggests that hunting has been occurring for more two million years. Furthermore, evidence exists that hunting may have one of the multiple environmental factors leading to the Holocene extinction of megafauna. North American megafauna extinction was coincidental with the Younger Dryas impact event, however, in other locations such as Australia, humans are thought to have played a very significant role in the extinction of the Australian megafauna that was widespread prior to human occupation. The closest surviving relatives of the species are the two species of Pan, the common chimpanzee and bonobos. Common chimpanzees have a diet that includes troop hunting behaviour based on beta males being led by an alpha male. Bonobos have also observed to occasionally engage in group hunting. With the establishment of language, culture, and religion, hunting became a theme of stories and myths, as well as such as dance. Hunting was a component of hunter-gatherer societies before the domestication of livestock
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Lierne
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Lierne is a municipality in Nord-Trøndelag county, Norway. It is part of the Namdalen region, and it is the largest municipality in Trøndelag, the administrative centre of the municipality is the village of Sandvika. Other villages include Inderdal, Sørli, and Tunnsjø senter, the municipality borders Sweden to the south and east. Most of Lierne lies on the Swedish side of the divide between Norway and Sweden. The cross-country race Flyktningerennet is held every year. It is a race that follows a route from Nordli to Gäddede in Strömsund Municipality, Sweden, the municipality of Lierne was established on 1 January 1874 when it was separated from Snåsa. Initially, the population of Lierne was 1,015, on 1 July 1915, it was divided into two municipalities, Nordli and Sørli. On 1 January 1964 they were merged back together again under the former name Lierne, after the merger, there were 2,045 residents in the new municipality. The Old Norse form of the name was Finnahlíð, where the first element is the genitive case of finnr which means Sami person. The later form Lierne is the plural form of li which means mountainside. The coat-of-arms is from modern times, they were granted on 3 February 1984, the arms show three white Willow Ptarmigans on a blue background. The birds are plentiful in the area and hunting them was of great importance historically for the inhabitants to survive during the winters in the area, the bird was thus chosen as a symbol for the municipality. See also, the coats-of-arms of Sirdal and Holtålen The Church of Norway has two parishes within the municipality of Lierne and it is part of the Namdal deanery in the Diocese of Nidaros. Lierne National Park is located in the municipality, and Blåfjella-Skjækerfjella National Park is partly located in Lierne, Lierne has a significant population of brown bears. The municipality is governed by a council of elected representatives. The municipal council of Lierne is made up of 15 representatives that are elected to four years. Currently, the party breakdown is as follows, Nord-Trøndelag travel guide from Wikivoyage Municipal fact sheet from Statistics Norway
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Sirdal
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Sirdal is a municipality in Vest-Agder county, Norway. It is located in the part of the traditional district of Lister. The administrative centre of the municipality is the village of Tonstad, other villages in Sirdal include Bjørnestad, Haughom, Kvæven, Lunde, and Tjørhom. The old parish of Sirdal was first established as a municipality in 1849 when it was separated from the municipality of Bakke. On 1 January 1903, an area of Sirdal was transferred to the neighboring municipality of Fjotland. On 1 January 1905, the municipality of Sirdal was dissolved and these large, sparsely populated municipalities merged along with the Øksendal area of Bakke municipality to recreate the municipality of Sirdal on 1 January 1960. This time, Sirdal started out with a population of 1,426, on 1 January 1987, the Virak and Espetveit areas of northern Flekkefjord were transferred to Sirdal municipality. The municipality is named after the Sirdalen valley which runs through it, the Old Norse form of the name was Sírudalr. The first element is the case of the river name Síra. The last element is dalr which means valley or dale, the meaning of the river name is unknown. The coat-of-arms is from modern times, they were granted on 17 January 1986, the arms show three white-colored willow ptarmigans on a green background. The birds were chosen as a symbol for the hills and moors which make up the largest part of the municipality, the willow ptarmigan is a typical bird for the area. The Church of Norway has one parish within the municipality of Sirdal and it is part of the Lister deanery in the Diocese of Agder og Telemark. Sirdal municipality includes the northernmost valley in Vest-Agder county, bordering Aust-Agder county to the northeast, to the south, it borders on the municipality of Flekkefjord and to the east is Kvinesdal. Sirdal is the largest area municipality in Vest-Agder, lakes in the region include Gravatnet, Kulivatnet, Kvifjorden, Øyarvatnet, Rosskreppfjorden, Sirdalsvatnet, and Valevatn. The mountain Urddalsknuten lies at the end of the municipality. In 1990, the road opened between the Sirdalen valley and the Setesdal valley over the Suleskard mountain pass. It connected Sirdal to Brokke in the municipality of Valle to the east
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Church of Norway
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The Church of Norway, from 2017 called the Peoples Church, is a Lutheran denomination of Protestant Christianity that serves as the peoples church and the largest church in Norway. The church was established after the Lutheran reformation in Denmark–Norway in 1536–1537 broke ties with the Holy See, the church professes the Lutheran Christian faith, with its foundation on the Bible, the Apostles, Nicene and Athanasian Creeds, Luthers Small Catechism and the Augsburg Confession. The church is a member of the Porvoo Communion with 12 other churches and it has also signed some other ecumenical texts, including the Joint Declaration on the Doctrine of Justification with the Roman Catholic Church. Until 1969, the name for administrative purposes was simply the State Church or sometimes just the Church. While the church remains state-funded and integrated in the administration with a special constitutional role, it is largely self-governing in doctrinal matters. On 27 May,2016, Stortinget passed a new bill that establishes the Church of Norway as an independent legal entity rather than a branch of the civil service, the Church of Norway officially ceased to be the state church on January 1,2017. Until 1845 the Church of Norway was the only religious organization in Norway. Dissenterloven was a passed by the Storting on 16 July 1845 that allowed the establishment of alternative religious bodies. This bill was in 1969 replaced by Lov om trudomssamfunn og ymist anna, until 2012 the constitutional head of the church was the King of Norway, who is obliged to profess himself a Lutheran. After the constitutional amendment of May 21,2012, the church is self-governed with regard to doctrinal issues, bishops and priests are civil servants also after the 2012 constitutional reform. Each parish has an autonomous administration, the state itself does not administer church buildings, buildings and adjacent land instead belong to the parish as an independent public institution. The Minister of Church Affairs, Trond Giske, was responsible for proposing the 2012 amendments, the church itself explained that, In 2012 the Parliament changed the constitution such that Norway no longer has a public religion. The Church of Norway can accordingly no longer be labeled as state church, a bill passed in 2016 created the Church of Norway as an independent legal entity, effective from 1 January 2017. The church has a structure, with 1,284 parishes,106 deaneries,11 dioceses and since 2 October 2011. The dioceses are – according to the rank of the five historic sees and then according to age, Nidaros, seated in Trondheim, bishops, Presiding Bishop of Nidaros and Bishop of Nidaros Cathedral Deanery Helga Haugland Byfuglien, Bishop of Nidaros Tor Singsaas. Bjørgvin, seated in Bergen, covering the counties of Hordaland, Oslo, seated in Oslo, covering Oslo and parts of the county of Akershus. Stavanger, seated in Stavanger, covering the county of Rogaland, Hamar, seated in Hamar, covering the counties of Hedmark and Oppland. Nord-Hålogaland, seated in Tromsø, covering the counties of Troms and Finnmark, agder og Telemark, seated in Kristiansand, covering the counties of Vest-Agder, Aust-Agder and Telemark
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Diocese of Nidaros
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Nidaros is a diocese in the Lutheran Church of Norway. It covers Nord-Trøndelag and Sør-Trøndelag counties and its cathedral city is Trondheim, the diocese is divided into 12 deaneries. Finn Wagle was the bishop from 1991 to 2008, on 1 July 2008 Tor Singsaas took over the position. The diocese of Nidaros was established in 1068 and it then covered the counties of Sør-Trøndelag, Nord-Trøndelag, Nordland, Troms, and Finnmark, along with the regions of Nordmøre and Romsdal and Härjedalen, and also the northern part of Østerdalen. The region of Sunnmøre was transferred from Diocese of Bjørgvin to the new Archdiocese of Nidaros some time after 1152 – to secure it more income, the northern part of Østerdalen was transferred to Diocese of Oslo some time after 1537. The province of Jämtland was transferred from Diocese of Uppsala to Nidaros in 1570, the region of Sunnmøre was transferred from Nidaros to the Diocese of Bjørgvin in 1622. The provinces of Jämtland and Härjedalen were lost to Sweden in 1645, nord-Norge was established as a diocese of its own in 1804. The parish of Innset was transferred from Diocese of Hamar to Nidaros in 1966, the regions of Nordmøre and Romsdal were established as a diocese of its own in 1983. The Diocese of Nidaros is divided into twelve deaneries, each one corresponds to several municipalities in the diocese. Each municipality is divided into one or more parishes which each contain one or more congregations. See each municipality below for lists of churches and parishes within them, the bishops of Nidaros since the Protestant Reformation when Norway switched from Catholicism to Lutheranism
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Haltdalen Church
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Haltdalen Church is a parish church in the municipality of Holtålen in Sør-Trøndelag county, Norway. The church is located in the village of Haltdalen, the church was built in 1881 by architects Jacob Digre and Gustav Olsen. The wooden building was built in the Neo-gothic style and was built to hold about 300 people, the church is part of the Haltdalen parish in the Gauldal deanery in the Diocese of Nidaros
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Haltdalen Stave Church
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Haltdalen Stave Church is a stave church originally from Haltdalen in the municipality of Holtålen in Sør-Trøndelag county, Norway. It is now on display at the Sverresborg museum in Trondheim, the church was probably built in the 1170s. The church on display is a version of two churches from Ålen and Haltdalen. The western wall and the portal is from the old Ålen church and this is a single-nave stave church of the east Scandinavian-style, and it is the only one that is preserved. The replica was undertaken by the Norwegian Institute for Cultural Heritage Research as a three-year research, a gallery was added around the outside of the building, inspired by other stave churches, to provide the building with extra strength against the stormy weather of the Vestmannaeyjar. The church was built and consecrated in summer 2000, the project was supported by a Norwegian government grant of 5. The replica also includes an altar decorated with a replica of the St Olav frontal, one of the finest surviving medieval Norwegian works of art, undertaken under the leadership of Terje Nordsted
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Trondheim
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Trondheim, historically Kaupangen, Nidaros and Trondhjem, is a city and municipality in Sør-Trøndelag county, Norway. It has a population of 187,353, and is the third most populous municipality in Norway and it is the third largest city in the country, with a population of 169,972 inhabitants within the city borders. The city functions as the centre of Sør-Trøndelag county. Trondheim lies on the shore of Trondheim Fjord at the mouth of the river Nidelva. The settlement was founded in 997 as a trading post, from 1152 to 1537, the city was the seat of the Catholic Archdiocese of Nidaros, since then, it has remained the seat of the Lutheran Diocese of Nidaros and the Nidaros Cathedral. The current municipality dates from 1964, when Trondheim merged with Byneset, Leinstrand, Strinda, for the ecclesiastical history, see Archiepiscopate of Nidaros Trondheim was named Kaupangen by Viking King Olav Tryggvason in 997. Shortly thereafter it came to be called Nidaros, in the beginning it was frequently used as a military retainer of King Olav I. It was frequently used as the seat of the king, and was the capital of Norway until 1217, people have been living in the region for thousands of years as evidenced by the rock carvings in central Norway, the Nøstvet and Lihult cultures and the Corded Ware culture. In ancient times, the Kings of Norway were hailed at Øretinget in Trondheim, Harald Fairhair was hailed as the king here, as was his son, Haakon I, called the Good. The battle of Kalvskinnet took place in Trondheim in 1179, King Sverre Sigurdsson, some scholars believe that the famous Lewis chessmen, 12th-century chess pieces carved from walrus ivory found in the Hebrides and now at the British Museum, may have been made in Trondheim. Trondheim was the seat of the Archdiocese of Nidaros for Norway from 1152, due to the introduction of Lutheran Protestantism in 1537, the last Archbishop, Olav Engelbrektsson, had to flee from the city to the Netherlands, where he died in present-day Lier, Belgium. The city has experienced major fires. Since much of the city was made of wooden buildings, many of the fires caused severe damage. Great fires ravaged the city in 1598,1651,1681,1708, twice in 1717,1742,1788,1841 and 1842, however, the 1651 fire destroyed 90% of all buildings within the city limits. The fire in 1681 led to an almost total reconstruction of the city, overseen by General Johan Caspar von Cicignon, broad avenues like Munkegaten were created, with no regard for property rights, in order to stop the next fire. At the time, the city had a population of roughly 8000 inhabitants, after the Treaty of Roskilde on 26 February 1658, Trondheim and the rest of Trøndelag, became Swedish territory for a brief period, but the area was reconquered 10 months later. The conflict was settled by the Treaty of Copenhagen on 27 May 1660. During World War II, Trondheim was occupied by Nazi Germany from 9 April 1940, the home of the most notorious Norwegian Gestapo agent, Henry Rinnan, was in Trondheim
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Aunegrenda Chapel
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Aunegrenda Chapel is a chapel in the municipality of Holtålen in Sør-Trøndelag county, Norway. The church is located in the village of Aunegrenda, the wooden church building was built in 1952 by architect Morgenstierne & Eide. The church was built to hold about 120 people, the church is part of the Haltdalen parish in the Gauldal deanery in the Diocese of Nidaros
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Hessdalen Church
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Hessdalen Church is a parish church in the municipality of Holtålen in Sør-Trøndelag county, Norway. The church is located in the village of Hessdalen, the church was built in 1940 by architects John Egil Tverdahl and Arne S. Gynnild. The wooden building was built to hold about 186 people, the church is part of the Hessdalen parish in the Gauldal deanery in the Diocese of Nidaros
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World Heritage Site
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A World Heritage Site is a landmark which has been officially recognized by the United Nations, specifically by the United Nations Educational, Scientific and Cultural Organization. Sites are selected on the basis of having cultural, historical, scientific or some form of significance. UNESCO regards these sites as being important to the interests of humanity. The programme catalogues, names, and conserves sites of outstanding cultural or natural importance to the common culture, under certain conditions, listed sites can obtain funds from the World Heritage Fund. The program was founded with the Convention Concerning the Protection of the Worlds Cultural and Natural Heritage, since then,192 state parties have ratified the convention, making it one of the most adhered to international instruments. As of July 2016,1052 sites are listed,814 cultural,203 natural, in 1959, the governments of Egypt and Sudan requested UNESCO to assist their countries to protect and rescue the endangered monuments and sites. In 1960, the Director-General of UNESCO launched an appeal to the Member States for an International Campaign to Save the Monuments of Nubia, the campaign, which ended in 1980, was considered a success. The project cost $80 million, about $40 million of which was collected from 50 countries, the projects success led to other safeguarding campaigns, saving Venice and its lagoon in Italy, the ruins of Mohenjo-daro in Pakistan, and the Borobodur Temple Compounds in Indonesia. UNESCO then initiated, with the International Council on Monuments and Sites, the United States initiated the idea of cultural conservation with nature conservation. The International Union for Conservation of Nature developed similar proposals in 1968, the Convention came into force on 17 December 1975. As of June 2016, it has been ratified by 192 states, including 188 UN member states plus the Cook Islands, the Holy See, Niue, a country must first list its significant cultural and natural sites, the result is called the Tentative List. A country may not nominate sites that have not been first included on the Tentative List, next, it can place sites selected from that list into a Nomination File. The Nomination File is evaluated by the International Council on Monuments and Sites and these bodies then make their recommendations to the World Heritage Committee. There are ten selection criteria – a site must meet at least one of them to be included on the list, up to 2004, there were six criteria for cultural heritage and four criteria for natural heritage. In 2005, this was modified so there is now only one set of ten criteria. Nominated sites must be of outstanding value and meet at least one of the ten criteria. Thus, the Geneva Convention treaty promulgates, Article 53, PROTECTION OF CULTURAL OBJECTS AND OF PLACES OF WORSHIP. There are 1,052 World Heritage Sites located in 165 States Party, of these,814 are cultural,203 are natural and 35 are mixed properties
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Trøndelag travel guide from Wikivoyage
