1.
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
2.
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
3.
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
4.
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
5.
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
6.
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
7.
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
8.
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
9.
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
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
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Trøndelag travel guide from Wikivoyage
