Fennoscandia in the context of "Uralic"

⭐ In the context of Uralic languages, Fennoscandia is considered…

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⭐ Core Definition: Fennoscandia

Fennoscandia (Finnish, Swedish and Norwegian: Fennoskandia; Russian: Фенноскандия, romanizedFennoskandiya), or the Fennoscandian Peninsula, is a peninsula in Europe which includes the Scandinavian and Kola peninsulas, mainland Finland, and Karelia. Administratively, this roughly encompasses the mainlands of Finland, Norway and Sweden, as well as Murmansk Oblast, the Republic of Karelia, and parts of northern Leningrad Oblast in Russia.

Its name comes from the Latin words Fennia (Finland) and Scandia (Scandinavia). The term was first used by the Finnish geologist Wilhelm Ramsay in 1898.

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👉 Fennoscandia in the context of Uralic

The Uralic languages (/jʊəˈrælɪk/ yoor-AL-ik), sometimes called the Uralian languages (/jʊəˈrliən/ yoor-AY-lee-ən), are spoken predominantly in Europe and North Asia. The Uralic languages with the most native speakers are Hungarian, Finnish, and Estonian. Other languages with speakers above 100,000 are Erzya, Moksha, Mari, Udmurt and Komi spoken in the European parts of the Russian Federation. Still smaller minority languages are Sámi languages of the northern Fennoscandia; other members of the Finnic languages, ranging from Livonian in northern Latvia to Karelian in northwesternmost Russia; the Samoyedic languages and the other members of the Ugric languages, Mansi and Khanty spoken in Western Siberia.

The name Uralic derives from the family's purported "original homeland" (Urheimat) hypothesized to have been somewhere in the vicinity of the Ural Mountains, and was first proposed by Julius Klaproth in Asia Polyglotta (1823).

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Fennoscandia in the context of Sápmi

68°N 20°E / 68°N 20°E / 68; 20

Sápmi is the cultural region traditionally inhabited by the Sámi people. Sápmi includes the northern parts of Fennoscandia, stretching over four countries: Norway, Sweden, Finland, and Russia. Most of Sápmi lies north of the Arctic Circle, bounded by the Barents Sea, Norwegian Sea, and White Sea. In the south, Sápmi extends to the counties of Trøndelag in Norway and Jämtland in Sweden.

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Fennoscandia in the context of Finland

Finland, officially the Republic of Finland, is a Nordic country in Northern Europe. It borders Sweden to the northwest, Norway to the north, and Russia to the east, with the Gulf of Bothnia to the west and the Gulf of Finland to the south, opposite Estonia. Finland has a population of 5.6 million, the majority being ethnic Finns. Its capital and largest city is Helsinki. The official languages are Finnish and Swedish, the mother tongues of 84.1 percent and 5.1 percent of the population, respectively. Finland's climate varies from humid continental in the south to boreal in the north. Its land is predominantly covered by boreal forest, with over 180,000 recorded lakes.

Finland was first settled around 9000 BC after the last Ice Age. During the Stone Age, various cultures emerged, distinguished by different styles of ceramics. The Bronze Age and Iron Ages were marked by contacts with other cultures in Fennoscandia and the Baltic region. From the late 13th century, Finland became part of Sweden following the Northern Crusades. In 1809, as a result of the Finnish War, Finland was captured from Sweden and became an autonomous grand duchy within the Russian Empire. During this period, Finnish art flourished and an independence movement gradually developed.

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Fennoscandia in the context of Gulf of Bothnia

The Gulf of Bothnia (/ˈbɒθniə/, Swedish: Bottniska viken, Finnish and Meänkieli: Pohjanlahti) is divided into the Bothnian Bay, the (North) Kvarken and the Bothnian Sea, and it is the northernmost arm of the Baltic Sea, between Finland's west coast (Ostrobothnia (East Bothnia)) and the northern part of Sweden's east coast (Västerbotten (Westrobothnia, West Bothnia) and Norrbotten (North Bothnia)). In the south of the gulf lies Åland, between the Sea of Åland and the Archipelago Sea.

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Fennoscandia in the context of Subarctic

The subarctic zone is a region in the Northern Hemisphere immediately south of the true Arctic, north of hemiboreal regions and covering much of Alaska, Canada, Iceland, the north of Fennoscandia, Northwestern Russia, Siberia, and the Cairngorms. Generally, subarctic regions fall between 50°N and 70°N latitude, depending on local climates. Precipitation is usually low, and vegetation is characteristic of the taiga.

Daylight at these latitudes is quite extreme between summer and winter due to its high latitude. Near the summer solstice for instance, subarctic regions can experience an all-night period of either civil, nautical, or astronomical twilight (or in the northern reaches full daylight), since the sun never dips more than 18 degrees below the horizon. Noctilucent clouds are best observed within this range of latitude.

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Fennoscandia in the context of History of Denmark

The history of Denmark as a unified kingdom began in the 8th century, but historic documents describe the geographic area and the people living there—the Danes—as early as 500 AD. These early documents include the writings of Jordanes and Procopius. With the Christianization of the Danes c. 960 AD, it is clear that there existed a kingship. King Frederik X can trace his lineage back to the Viking kings Gorm the Old and Harald Bluetooth from this time, thus making the Monarchy of Denmark the oldest in Europe. The area now known as Denmark has a rich prehistory, having been populated by several prehistoric cultures and people for about 12,000 years, since the end of the last ice age.

Denmark's history has particularly been influenced by its geographical location between the North and Baltic seas, a strategically and economically important placement between Sweden and Germany, at the center of mutual struggles for control of the Baltic Sea (dominium maris baltici). Denmark was long in disputes with Sweden over control of Skånelandene and with Germany over control of Schleswig (a Danish fief) and Holstein (a German fief).

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Fennoscandia in the context of Fell

Fell (from Old Norse: fell, "mountain → landscape over the tree line"; cf. Icelandic: fell, Norwegian: fjell, Swedish: fjäll) is a high and barren landscape feature, such as a mountain or moor-covered hill, often mountain landscape over the tree line, etc. The term is most often employed in Fennoscandia, Iceland, the Isle of Man, parts of northern England, and Scotland.

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