Geography | |
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Location | Northern Europe |
Coordinates | 63°00′N14°00′E / 63.000°N 14.000°E |
Adjacent to | Arctic Sea, Atlantic Ocean |
Area | 750,000 km2 (290,000 sq mi) |
Highest elevation | 2,469 m (8100 ft) |
Highest point | Galdhøpiggen |
Administration | |
Mainland | |
Mainland | |
Parts of Lapland |
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Scandinavia |
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The Scandinavian Peninsula [1] is located in Northern Europe, and roughly comprises the mainlands of Sweden, Norway and the northwestern area of Finland.
The name of the peninsula is derived from the term Scandinavia, the cultural region of Denmark, Norway and Sweden. That cultural name is in turn derived from the name of Scania, the region at the southern extremity of the peninsula which was for centuries a part of Denmark, which is the ancestral home of the Danes, and is now part of Sweden. [2] [3] [4]
The Scandinavian Peninsula is the largest of the peninsulas of Europe, with a greater area than the Balkan, Iberian and Italian peninsulas. During the Ice Ages, the sea level of the Atlantic Ocean dropped so much that the Baltic Sea, the Gulf of Bothnia and the Gulf of Finland disappeared, and the countries now surrounding them, including Germany, Poland, the other Baltic countries and Scandinavia, were directly joined by land.
The largest peninsula in Europe, the Scandinavian Peninsula is approximately 1,850 kilometres (1,150 mi) long with a width varying approximately from 370 to 805 km (230 to 500 mi). The Scandinavian mountain range generally defines the border between Norway and Sweden.
Its highest elevation was Glittertinden in Norway at 2,470 m (8,104 ft) above sea level, but since the glacier at its summit partially melted, [5] the highest elevation is at 2,469 m (8,100 ft) at Galdhøpiggen, also in Norway. These mountains also have the largest glacier on the mainland of Europe, Jostedalsbreen.
About one quarter of the Scandinavian Peninsula lies north of the Arctic Circle, its northernmost point being at Cape Nordkyn, Norway.
The climate across Scandinavia varies from tundra (Köppen: ET) and subarctic (Dfc) in the north, with cool marine west coast climate (Cfc) in northwestern coastal areas reaching just north of Lofoten, to humid continental (Dfb) in the central portion and marine west coast (Cfb) in the south and southwest. [6] The region is rich in timber, iron and copper with the best farmland in southern Sweden. Large petroleum and natural-gas deposits have been found off Norway's coast in the North Sea and the Atlantic Ocean.
Much of the population of the Scandinavian Peninsula is naturally concentrated in its southern part, which is also its agricultural region. The largest cities of the peninsula are Stockholm, Sweden; Oslo, Norway; Gothenburg, Sweden; Malmö, Sweden and Bergen, Norway, in that order.
The Scandinavian Peninsula occupies part of the Baltic Shield, a stable and large crust segment formed of very old, crystalline metamorphic rocks. Most of the soil covering this substrate was scraped by glaciers during the Ice Ages of antiquity, especially in northern Scandinavia, where the Baltic Shield is closest to the surface of the land.[ citation needed ] As a consequence of this scouring, the elevation of the land and the cool-to-cold climate, a relatively small percentage of its land is arable. [7]
The glaciation during the Ice Ages also deepened many of the river valleys, which were invaded by the sea when the ice melted, creating the noteworthy fjords of Norway. In the southern part of the peninsula, the glaciers deposited vast numbers of terminal moraines, configuring a very chaotic landscape. [8] These terminal moraines covered all of what is now Denmark.
Although the Baltic Shield is mostly geologically stable and hence resistant to the influences of other neighbouring tectonic formations, the weight of nearly four kilometres of ice during the Ice Ages caused all of the Scandinavian terrain to sink. When the ice sheet disappeared, the shield rose again, a tendency that continues to this day at a rate of about one metre per century. [8] Conversely, the southern part has tended to sink to compensate, causing flooding of the Low Countries and Denmark.
The crystalline substrate of the land and absence of soil in many places have exposed mineral deposits of metal ores, such as those of iron, copper, nickel, zinc, silver and gold. The very most valuable of these have been the deposits of iron ore in northwestern Sweden. In the 19th century these deposits prompted the building of a railway from northwestern Sweden to the Norwegian seaport of Narvik so that the iron ore could be exported by ship to places like southern Sweden, Germany, Great Britain and Belgium for smelting into iron and steel. This railway is in a region of Norway and Sweden that otherwise does not have any railways because of the very rugged terrain, mountains and fjords of that part of Scandinavia.
The first recorded human presence in the southern area of the peninsula and Denmark dates from 12,000 years ago. [9] As the ice sheets from the glaciation retreated, the climate allowed a tundra biome that attracted reindeer hunters. The climate warmed up gradually, favouring the growth of evergreen trees first and then deciduous forest which brought animals like aurochs. Groups of hunter-fisher-gatherers started to inhabit the area from the Mesolithic (8200 BC), up to the advent of agriculture in the Neolithic (3200 BC).
The northern and central part of the peninsula is partially inhabited by the Sami, often referred to as "Lapps" or "Laplanders", who began to arrive several thousand years after the Scandinavian Peninsula had already been inhabited in the south. In the earliest recorded periods they occupied the arctic and subarctic regions as well as the central part of the peninsula as far south as Dalarna, Sweden. They speak the Sami language, a non-Indo-European language of the Uralic family which is related to Finnish and Estonian. The first inhabitants of the peninsula were the Norwegians[ when? ] on the west coast of Norway, the Danes in what is now southern and western Sweden and southeastern Norway, the Svear in the region around Mälaren as well as a large portion of the present day eastern seacoast of Sweden and the Geats in Västergötland and Östergötland. These peoples spoke closely related dialects of an Indo-European language, Old Norse. Although political boundaries have shifted, descendants of these peoples still are the dominant populations in the peninsula in the early 21st century. [10]
Although the Nordic countries look back on more than 1,000 years of history as distinct political entities, the international boundaries came late and emerged gradually. It was not until the middle of the 17th century that Sweden had a secure outlet on the Kattegat and control of the south Baltic coast. The Swedish and Norwegian boundaries were finally agreed and marked out in 1751. The Finnish-Norwegian border on the peninsula was established after extensive negotiation in 1809, and the common Norwegian-Russian districts were not partitioned until 1826. Even then the borders were still fluid, with Finland gaining access to the Barents Sea in 1920, but ceding this territory to the Soviet Union in 1944. [11]
Denmark, Sweden and the Russian Empire dominated the political relationships on the Scandinavian Peninsula for centuries, with Iceland, Finland and Norway only gaining their full independence during the 20th century. The Kingdom of Norway – long held in personal union by Denmark – fell to Sweden after the Napoleonic Wars and only attained full independence in 1905. Having been an autonomous grand duchy within the Russian Empire since 1809, Finland declared independence during the Soviet revolution of Russia in 1917. Iceland declared its independence from Denmark in 1944, while Denmark was under the occupation of Nazi Germany. Iceland was encouraged to do this by the British and American armed forces that were defending Iceland from Nazi invasion.
The Wehrmacht invaded Norway in 1940 and the German Army occupied all of Norway until May 1945. With the acquiescence of the Kingdom of Sweden, German troops moved from northern Norway, across northern Sweden, into Finland, which had become an ally of Nazi Germany. Then, in the spring of 1941, the German Army and the Finnish Army invaded the Soviet Union together. The Republic of Finland had a grievance against the Soviet Union because the Red Army had invaded southeastern Finland in the Winter War (1939–40) and had taken a large area of territory away from Finland.
Sweden remained a neutral country during the First World War, the Korean War and the Cold War.
In 1945, Norway, Denmark and Iceland were founding members of the United Nations. Sweden joined the U.N. soon after. Finland joined during the 1950s. The first Secretary General of the United Nations, Trygve Lie, was a Norwegian citizen. The second Secretary General of the United Nations, Dag Hammarskjöld, was a Swedish citizen. Thus the people of the Scandinavian Peninsula had a strong influence in international affairs during the 20th century.
In 1949, Norway, Denmark and Iceland became founding members of the North Atlantic Treaty Organisation for their defence against East Germany, the Soviet Union and all other potential invaders, and these three countries remain members as of 2021 [update] . [12]
Sweden and Finland joined the European Union in 1995. Norway, however, remains outside the Union.
The Baltic Sea is an arm of the Atlantic Ocean that is enclosed by Denmark, Estonia, Finland, Germany, Latvia, Lithuania, Poland, Russia, Sweden, and the North and Central European Plain.
The Kalmar Union was a personal union in Scandinavia, agreed at Kalmar in Sweden as designed by widowed Queen Margaret of Norway and Sweden. From 1397 to 1523, it joined under a single monarch the three kingdoms of Denmark, Sweden, and Norway, together with Norway's overseas colonies.
Scandinavia is a subregion of Northern Europe, with strong historical, cultural, and linguistic ties between its constituent peoples. Scandinavia most commonly refers to Denmark, Norway, and Sweden. It can sometimes also refer to the Scandinavian Peninsula. In English usage, Scandinavia is sometimes used as a synonym for Nordic countries. Iceland and the Faroe Islands are sometimes included in Scandinavia for their ethnolinguistic relations with Sweden, Norway and Denmark. While Finland differs from other Nordic countries in this respect, some authors call it Scandinavian due to its economic and cultural similarities.
The history of Sweden can be traced back to the melting of the Northern Polar Ice Caps. From as early as 12000 BC, humans have inhabited this area. Throughout the Stone Age, between 8000 BC and 6000 BC, early inhabitants used stone-crafting methods to make tools and weapons for hunting, gathering and fishing as means of survival. Written sources about Sweden before AD 1000 are rare and short, usually written by outsiders. It was not until the 14th century that longer historical texts were produced in Sweden. It is therefore usually accepted that Swedish recorded history, in contrast with pre-history, starts around the 11th century, when sources are common enough that they can be contrasted with each other.
The Nordic Council is the official body for formal inter-parliamentary Nordic cooperation among the Nordic countries. Formed in 1952, it has 87 representatives from Denmark, Finland, Iceland, Norway, and Sweden as well as from the autonomous areas of the Faroe Islands, Greenland, and Åland. The representatives are members of parliament in their respective countries or areas and are elected by those parliaments. The Council holds ordinary sessions each year in October/November and usually one extra session per year with a specific theme. The council's official languages are Danish, Finnish, Icelandic, Norwegian, and Swedish, though it uses only the mutually intelligible Scandinavian languages—Danish, Norwegian, and Swedish—as its working languages. These three comprise the first language of around 80% of the region's population and are learned as a second or foreign language by the remaining 20%.
In physical geography, a fjord or fiord is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounded landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be 29,000 km (18,000 mi) long with its nearly 1,200 fjords, but only 2,500 km (1,600 mi) long excluding the fjords.
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. Queen Margrethe II can trace her 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.
The northern region of Europe has several definitions. A restrictive definition may describe Northern Europe as being roughly north of the southern coast of the Baltic Sea, which is about 54°N, or may be based on other geographical factors such as climate and ecology.
The terms Baltic Sea Region, Baltic Rim countries, and the Baltic Sea countries/states refer to slightly different combinations of countries in the general area surrounding the Baltic Sea, mainly in Northern Europe. The term "Baltic states" refers specifically to one such grouping.
The Baltic Shield is a segment of the Earth's crust belonging to the East European Craton, representing a large part of Fennoscandia, northwestern Russia and the northern Baltic Sea. It is composed mostly of Archean and Proterozoic gneisses and greenstone which have undergone numerous deformations through tectonic activity. It contains the oldest rocks of the European continent with a thickness of 250–300 km.
Europe, the westernmost portion of Eurasia, is often divided into regions and subregions based on geographical, cultural or historical factors. Since there is no universal agreement on Europe's regional composition, the placement of individual countries may vary based on criteria being used. For instance, the Balkans is a distinct geographical region within Europe, but individual countries may alternatively be grouped into South-eastern Europe or Southern Europe.
The Scandinavian Peninsula became ice-free around the end of the last ice age. The Nordic Stone Age begins at that time, with the Upper Paleolithic Ahrensburg culture, giving way to the Mesolithic hunter-gatherers by the 7th millennium BC. The Neolithic stage is marked by the Funnelbeaker culture, followed by the Pitted Ware culture.
The history of Scandinavia is the history of the geographical region of Scandinavia and its peoples. The region is located in Northern Europe, and consists of Denmark, Norway and Sweden. Finland and Iceland are at times, especially in English-speaking contexts, considered part of Scandinavia.
The Baltic Ice Lake is a name given by geologists to a freshwater lake that evolved in the Baltic Sea basin as glaciers retreated from that region at the end of the last ice age. The lake existed between 12,600 and 10,300 years Before Present (BP).
Scandinavian studies is an interdisciplinary academic field of area studies, mainly in the United States and Germany, that primarily focuses on the Scandinavian languages and cultural studies pertaining to Scandinavia and Scandinavian language and culture in the other Nordic countries. While Scandinavia is defined as Denmark, Norway and Sweden, the term Scandinavian in an ethnic, cultural and linguistic sense is often used synonymously with North Germanic and also refers to the peoples and languages of the Faroe Islands and Iceland; furthermore a minority in Finland are ethnically Scandinavian and speak Swedish natively.
The climate of the Nordic countries is that of a region in Northern Europe that consists of Denmark, Finland, Iceland, Norway and Sweden and their associated territories, which include the Faroe Islands, Greenland and Åland. Stockholm, Sweden has on average the warmest summer of the Nordic capitals, with an average maximum temperature of 23 °C (73 °F) in July; Copenhagen, Oslo and Helsinki have an average July maximum temperature of 22 °C (72 °F).
The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the Würm glaciation. It was characterized by a large ice sheet that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age, Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (Weichsel-Kaltzeit), Weichselian glacial (Weichsel-Glazial), Weichselian Stage or, rarely, the Weichselian complex (Weichsel-Komplex).
The Nordic countries are a geographical and cultural region in Northern Europe and the North Atlantic. It includes the sovereign states of Denmark, Finland, Iceland, Norway and Sweden; the autonomous territories of the Faroe Islands and Greenland; and the autonomous region of Åland.
The Scandinavian Mountains or the Scandes is a mountain range that runs through the Scandinavian Peninsula. The western sides of the mountains drop precipitously into the North Sea and Norwegian Sea, forming the fjords of Norway, whereas to the northeast they gradually curve towards Finland. To the north they form the border between Norway and Sweden, reaching 2,000 metres (6,600 ft) high at the Arctic Circle. The mountain range just touches northwesternmost Finland but are scarcely more than hills at their northernmost extension at the North Cape.
North Germanic peoples, commonly called Scandinavians, Nordic peoples and in a medieval context Norsemen, were a Germanic linguistic group originating from the Scandinavian Peninsula. They are identified by their cultural similarities, common ancestry and common use of the Proto-Norse language from around 200 AD, a language that around 800 AD became the Old Norse language, which in turn later became the North Germanic languages of today.