Socialist Federal Republic of Yugoslavia
The Socialist Federal Republic of Yugoslavia was a country located in central and Southeastern Europe that existed from its foundation in the aftermath of World War II until its dissolution in 1992 amid the Yugoslav Wars. Covering an area of 255,804 km², the SFRY was bordered by the Adriatic Sea and Italy to the west and Hungary to the north and Romania to the east, Albania and Greece to the south; the nation was a socialist state and a federation governed by the League of Communists of Yugoslavia and made up of six socialist republics: Bosnia and Herzegovina, Macedonia, Montenegro and Slovenia with Belgrade as its capital. In addition, it included two autonomous provinces within Serbia: Vojvodina; the SFRY's origin is traced to 26 November 1942, when the Anti-Fascist Council for the National Liberation of Yugoslavia was formed during World War II. On 29 November 1945, the Federal People's Republic of Yugoslavia was proclaimed after the deposition of King Peter II, thus ending the monarchy.
Until 1948, the new communist government sided with the Eastern Bloc under the leadership of Josip Broz Tito at the beginning of the Cold War, but after the Tito–Stalin split of 1948, Yugoslavia pursued a policy of neutrality. It became one of the founding members of the Non-Aligned Movement, transitioned from a planned economy to market socialism; the SFRY maintained neutrality during the Cold War as part of its foreign policy. It was a founding member of CERN, the United Nations, Non-Aligned Movement, OSCE, IFAD, WTO, BTWC. Following the death of Tito on 4 May 1980, the Yugoslav economy started to collapse, which increased unemployment and inflation; the economic crisis led to a rise in ethnic nationalism in early 1990s. With the collapse of communism in Eastern Europe, inter-republic talks on transformation of the federation failed. In 1991 some European states recognized their independence; the federation collapsed along federal borders, followed by the start of the Yugoslav Wars, the final downfall and breakup of the federation on 27 April 1992.
Two of its republics and Montenegro, remained within a reconstituted state known as the "Federal Republic of Yugoslavia", but this union was not recognized internationally as the official successor state to the SFRY. The term "former Yugoslavia" is now used retrospectively; the name Yugoslavia, an Anglicised transcription of Jugoslavija, is a composite word made up of jug and slavija. The Slavic word jug means'south', while slavija denotes a'land of the Slavs'. Thus, a translation of Jugoslavija would be'South-Slavia' or'Land of the South Slavs'; the full official name of the federation varied between 1945 and 1992. Yugoslavia was formed in 1918 under the name Kingdom of Serbs and Slovenes. In January 1929, King Alexander I assumed dictatorship of the kingdom and renamed it the Kingdom of Yugoslavia, for the first time making the term "Yugoslavia"—which had been used colloquially for decades —the official name of the state. After the Kingdom was occupied by the Axis during World War II, the Anti-Fascist Council for the National Liberation of Yugoslavia announced in 1943 the formation of the Democratic Federal Yugoslavia in the substantial resistance-controlled areas of the country.
The name deliberately left the republic-or-kingdom question open. In 1945, King Peter II was deposed, with the state reorganized as a republic, accordingly renamed Federal People's Republic of Yugoslavia, with the constitution coming into force in 1946. In 1963, amid pervasive liberal constitutional reforms, the name Socialist Federal Republic of Yugoslavia was introduced; the state is most referred to by the latter name, which it held for the longest period of all. Of the three main Yugoslav languages, the Serbo-Croatian and Macedonian language name for the state was identical, while Slovene differed in capitalization and the spelling of the adjective "Socialist"; the names are as follows: Serbo-Croatian and Macedonian languages Latin: Socijalistička Federativna Republika Jugoslavija Cyrillic: Социјалистичка Федеративна Република Југославија Serbo-Croatian pronunciation: Macedonian pronunciation: Slovene language Socialistična federativna republika Jugoslavija Due to the length of the name, abbreviations were used to refer to the Socialist Federal Republic of Yugoslavia, though the state was most known as Yugoslavia.
The most common abbreviation is SFRY, though SFR Yugoslavia was used in an official capacity by the media. On 6 April 1941, Yugoslavia was invaded by the Axis powers led by Nazi Germany. Yugoslav resistance was soon established in two forms, the Royal Yugoslav Army in the Homeland and the Communist Yugoslav Partisans; the Partisan supreme commander was Josip Broz Tito, under his command the movement soon began establishing "liberated territories" which attracted the attention of occupying forces. Unlike the various nationalist militias operating in occupied Yugoslavia, the Partisans were a pan-Yugoslav movement promoting the "brotherhood and unity" of Yugoslav nations, representing the republican, left-wing, socialist elements of the Yugoslav political
Denmark the Kingdom of Denmark, is a Nordic country and the southernmost of the Scandinavian nations. Denmark lies southwest of Sweden and south of Norway, is bordered to the south by Germany; the Kingdom of Denmark comprises two autonomous constituent countries in the North Atlantic Ocean: the Faroe Islands and Greenland. Denmark proper consists of a peninsula, an archipelago of 443 named islands, with the largest being Zealand and the North Jutlandic Island; the islands are characterised by flat, arable land and sandy coasts, low elevation and a temperate climate. Denmark has a total area of 42,924 km2, land area of 42,394 km2, the total area including Greenland and the Faroe Islands is 2,210,579 km2, a population of 5.8 million. The unified kingdom of Denmark emerged in the 10th century as a proficient seafaring nation in the struggle for control of the Baltic Sea. Denmark and Norway were ruled together under one sovereign ruler in the Kalmar Union, established in 1397 and ending with Swedish secession in 1523.
The areas of Denmark and Norway remained under the same monarch until Denmark -- Norway. Beginning in the 17th century, there were several devastating wars with the Swedish Empire, ending with large cessions of territory to Sweden. After the Napoleonic Wars, Norway was ceded to Sweden, while Denmark kept the Faroe Islands and Iceland. In the 19th century there was a surge of nationalist movements, which were defeated in the 1864 Second Schleswig War. Denmark remained neutral during World War I. In April 1940, a German invasion saw brief military skirmishes while the Danish resistance movement was active from 1943 until the German surrender in May 1945. An industrialised exporter of agricultural produce in the second half of the 19th century, Denmark introduced social and labour-market reforms in the early 20th century that created the basis for the present welfare state model with a developed mixed economy; the Constitution of Denmark was signed on 5 June 1849, ending the absolute monarchy, which had begun in 1660.
It establishes a constitutional monarchy organised as a parliamentary democracy. The government and national parliament are seated in Copenhagen, the nation's capital, largest city, main commercial centre. Denmark exercises hegemonic influence in the Danish Realm, devolving powers to handle internal affairs. Home rule was established in the Faroe Islands in 1948. Denmark negotiated certain opt-outs, it is among the founding members of NATO, the Nordic Council, the OECD, OSCE, the United Nations. Denmark is considered to be one of the most economically and developed countries in the world. Danes enjoy a high standard of living and the country ranks in some metrics of national performance, including education, health care, protection of civil liberties, democratic governance and human development; the country ranks as having the world's highest social mobility, a high level of income equality, is among the countries with the lowest perceived levels of corruption in the world, the eleventh-most developed in the world, has one of the world's highest per capita incomes, one of the world's highest personal income tax rates.
The etymology of the word Denmark, the relationship between Danes and Denmark and the unifying of Denmark as one kingdom, is a subject which attracts debate. This is centered on the prefix "Dan" and whether it refers to the Dani or a historical person Dan and the exact meaning of the -"mark" ending. Most handbooks derive the first part of the word, the name of the people, from a word meaning "flat land", related to German Tenne "threshing floor", English den "cave"; the -mark is believed to mean woodland or borderland, with probable references to the border forests in south Schleswig. The first recorded use of the word Danmark within Denmark itself is found on the two Jelling stones, which are runestones believed to have been erected by Gorm the Old and Harald Bluetooth; the larger stone of the two is popularly cited as Denmark's "baptismal certificate", though both use the word "Denmark", in the form of accusative ᛏᛅᚾᛘᛅᚢᚱᚴ tanmaurk on the large stone, genitive ᛏᛅᚾᛘᛅᚱᚴᛅᚱ "tanmarkar" on the small stone.
The inhabitants of Denmark are there called "Danes", in the accusative. The earliest archaeological findings in Denmark date back to the Eem interglacial period from 130,000–110,000 BC. Denmark has been inhabited since around 12,500 BC and agriculture has been evident since 3900 BC; the Nordic Bronze Age in Denmark was marked by burial mounds, which left an abundance of findings including lurs and the Sun Chariot. During the Pre-Roman Iron Age, native groups began migrating south, the first tribal Danes came to the country between the Pre-Roman and the Germanic Iron Age, in the Roman Iron Age; the Roman provinces maintained trade routes and relations with native tribes in Denmark, Roman coins have been found in Denmark. Evidence of strong Celtic cultural influence dates from this period in Denmark and much of North-West Europe and is among other things reflected in the finding of the Gundestrup cauldron; the tribal Danes came from the east Danish islands and Scania and spoke an early form of North Germanic.
Historians believe that before their arrival, most of Jutland and the nearest islands were settled by tribal J
A moraine is any glacially formed accumulation of unconsolidated glacial debris that occurs in both and glaciated regions on Earth, through geomorphological processes. Moraines are formed from debris carried along by a glacier and consisting of somewhat rounded particles ranging in size from large boulders to minute glacial flour. Lateral moraines are formed at the side of the ice flow and terminal moraines at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines, till-covered areas with irregular topography, medial moraines which are formed where two glaciers meet. Moraines may be composed of debris ranging in size from silt-sized glacial flour to large boulders; the debris is sub-angular to rounded in shape. Moraines may be on the glacier’s surface or deposited as piles or sheets of debris where the glacier has melted. Moraines may form through a number of processes, depending on the characteristics of sediment, the dynamics on the ice, the location on the glacier in which the moraine is formed.
Moraine forming processes may be loosely divided into active. Passive processes involve the placing of chaotic supraglacial sediments onto the landscape with limited reworking forming hummocky moraines; these moraines are composed of supraglacial sediments from the ice surface. Active processes form or rework moraine sediment directly by the movement of ice, known as glaciotectonism; these form push moraines and thrust-block moraines, which are composed of till and reworked proglacial sediment. Moraine may form by the accumulation of sand and gravel deposits from glacial streams emanating from the ice margin; these fan deposits may coalesce to form a long moraine bank marking the ice margin. Several processes may combine to form and rework a single moraine, most moraines record a continuum of processes. Moraines can be classified either by origin, location with respect to a glacier or former glacier, or by shape; the first approach is suitable for moraines associated with contemporary glaciers—but more difficult to apply to old moraines, which are defined by their particular morphology, since their origin is debated.
Some moraine types are known only from ancient glaciers, while medial moraines of valley glaciers are poorly preserved and difficult to distinguish after the retreat or melting of the glacier. Lateral moraines are parallel ridges of debris deposited along the sides of a glacier; the unconsolidated debris can be deposited on top of the glacier by frost shattering of the valley walls and/or from tributary streams flowing into the valley. The till is carried along the glacial margin; because lateral moraines are deposited on top of the glacier, they do not experience the postglacial erosion of the valley floor and therefore, as the glacier melts, lateral moraines are preserved as high ridges. Lateral moraines stand high because they protect the ice under them from the elements, causing it to melt or sublime less than the uncovered parts of the glacier. Multiple lateral moraines may develop as the glacier retreats. Ground moraines are till-covered areas with irregular topography and no ridges forming rolling hills or plains.
They are accumulated at the base of the ice as lodgment till, but may be deposited as the glacier retreats. In alpine glaciers, ground moraines are found between the two lateral moraines. Ground moraines may be modified into drumlins by the overriding ice. Rogen moraines or ribbed moraines are a type of basal moraines that form a series of ribs perpendicular to the ice flow in an ice sheet; the depressions between the ribs are sometimes filled with water, making the Rogen moraines look like tigerstripes on aerial photographs. Rogen moraines are named after Lake Rogen in Härjedalen, the landform’s type locality. End moraines, or terminal moraines, are ridges of unconsolidated debris deposited at the snout or end of the glacier, they reflect the shape of the glacier's terminus. Glaciers act much like a conveyor belt, carrying debris from the top of the glacier to the bottom where it deposits it in end moraines. End moraine size and shape are determined by whether the glacier is advancing, receding or at equilibrium.
The longer the terminus of the glacier stays in one place, the more debris accumulate in the moraine. There are two types of end moraines: recessional. Terminal moraines mark the maximum advance of the glacier. Recessional moraines are small ridges left. After a glacier retreats, the end moraine may be destroyed by postglacial erosion. Recessional moraines are observed as a series of transverse ridges running across a valley behind a terminal moraine, they form perpendicular to the lateral moraines that they reside between and are composed of unconsolidated debris deposited by the glacier. They are created during temporary halts in a glacier's retreat. A medial moraine is a ridge of moraine, it forms when two glaciers meet and the debris on the edges of the adjacent valley sides join and are carried on top of the enlarged glacier. As the glacier melts or retreats, the debris is deposited and a ridge down the middle of the valley floor is created; the Kaskawulsh Glacier in the Kluane National Park, has a ridge of medial moraine 1 km wide.
Supraglacial moraines are created by debris accumulated on top of glacial ice. This debris can accumulate due to ice flow toward the surface in the ablation zone, melting of surface ice or from debris that falls onto the glacier from valley sidewalls. Washboard moraines known as minor or corrugated moraines, are low-amplitude ge
South America is a continent in the Western Hemisphere in the Southern Hemisphere, with a small portion in the Northern Hemisphere. It may be considered a subcontinent of the Americas, how it is viewed in the Spanish and Portuguese-speaking regions of the Americas; the reference to South America instead of other regions has increased in the last decades due to changing geopolitical dynamics. It is bordered on the west on the north and east by the Atlantic Ocean, it includes twelve sovereign states, a part of France, a non-sovereign area. In addition to this, the ABC islands of the Kingdom of the Netherlands and Tobago, Panama may be considered part of South America. South America has an area of 17,840,000 square kilometers, its population as of 2016 has been estimated at more than 420 million. South America ranks fourth in fifth in population. Brazil is by far the most populous South American country, with more than half of the continent's population, followed by Colombia, Argentina and Peru. In recent decades Brazil has concentrated half of the region's GDP and has become a first regional power.
Most of the population lives near the continent's western or eastern coasts while the interior and the far south are sparsely populated. The geography of western South America is dominated by the Andes mountains. Most of the continent lies in the tropics; the continent's cultural and ethnic outlook has its origin with the interaction of indigenous peoples with European conquerors and immigrants and, more locally, with African slaves. Given a long history of colonialism, the overwhelming majority of South Americans speak Portuguese or Spanish, societies and states reflect Western traditions. South America occupies the southern portion of the Americas; the continent is delimited on the northwest by the Darién watershed along the Colombia–Panama border, although some may consider the border instead to be the Panama Canal. Geopolitically and geographically all of Panama – including the segment east of the Panama Canal in the isthmus – is included in North America alone and among the countries of Central America.
All of mainland South America sits on the South American Plate. South America is home to Angel Falls in Venezuela. South America's major mineral resources are gold, copper, iron ore and petroleum; these resources found in South America have brought high income to its countries in times of war or of rapid economic growth by industrialized countries elsewhere. However, the concentration in producing one major export commodity has hindered the development of diversified economies; the fluctuation in the price of commodities in the international markets has led to major highs and lows in the economies of South American states causing extreme political instability. This is leading to efforts to diversify production to drive away from staying as economies dedicated to one major export. South America is one of the most biodiverse continents on earth. South America is home to many interesting and unique species of animals including the llama, piranha, vicuña, tapir; the Amazon rainforests possess high biodiversity, containing a major proportion of the Earth's species.
Brazil is the largest country in South America, encompassing around half of the continent's land area and population. The remaining countries and territories are divided among three regions: The Andean States, the Guianas and the Southern Cone. Traditionally, South America includes some of the nearby islands. Aruba, Curaçao, Trinidad and the federal dependencies of Venezuela sit on the northerly South American continental shelf and are considered part of the continent. Geo-politically, the island states and overseas territories of the Caribbean are grouped as a part or subregion of North America, since they are more distant on the Caribbean Plate though San Andres and Providencia are politically part of Colombia and Aves Island is controlled by Venezuela. Other islands that are included with South America are the Galápagos Islands that belong to Ecuador and Easter Island, Robinson Crusoe Island, Chiloé and Tierra del Fuego. In the Atlantic, Brazil owns Fernando de Noronha and Martim Vaz, the Saint Peter and Saint Paul Archipelago, while the Falkland Islands are governed by the United Kingdom, whose sovereignty over the islands is disputed by Argentina.
South Georgia and the South Sandwich Islands may be associate
Somalia the Federal Republic of Somalia (Somali: Jamhuuriyadda Federaalka Soomaaliya. Jumhūrīyah aṣ-Ṣūmāl al-Fīdirālīyah, is a country located in the Horn of Africa, it is bordered by Ethiopia to the west, Djabuti to the northwest, the Gulf of Aden to the north, the Guardafui Channel and Somali Sea to the east, Kenya to the southwest. Somalia has the longest coastline on Africa's mainland, its terrain consists of plateaus and highlands. Climatically, hot conditions prevail year-round, with periodic monsoon winds and irregular rainfall. Somalia has an estimated population of around 14.3 million. And has been described as the most culturally homogeneous country in Africa. Around 85% of its residents are ethnic Somalis, who have inhabited the northern part of the country. Ethnic minorities are concentrated in the southern regions; the official languages of are Arabic. Most people in the country are Muslim, with the majority being Sunni. In antiquity, Somalia was an important commercial centre, it is among the most probable locations of the fabled ancient Land of Punt.
During the Middle Ages, several powerful Somali empires dominated the regional trade, including the Ajuran Empire, the Adal Sultanate, the Warsangali Sultanate, the Sultanate of the Geledi. The toponym Somalia was coined by the Italian explorer Luigi Robecchi Bricchetti. In the late 19th century, the British and Italian empires established the colonies of British Somaliland and Italian Somaliland. In the interior, Mohammed Abdullah Hassan's Darwiish repelled the British four times, forcing a retreat to the coast, before succumbing in the Somaliland campaign. Italy acquired full control of the northeastern and southern parts of the area after waging the Campaign of the Sultanates against the ruling Majeerteen Sultanate and Sultanate of Hobyo. In 1960, the two regions united to form the independent Somali Republic under a civilian government; the Supreme Revolutionary Council seized power in 1969 and established the Somali Democratic Republic, which collapsed in 1991 as the Somali Civil War broke out.
During this period most regions returned to religious law. The early 2000s saw the creation of interim federal administrations; the Transitional National Government was established in 2000, followed by the formation of the Transitional Federal Government in 2004, which reestablished the military. In 2006, the TFG assumed control of most of the nation's southern conflict zones from the newly formed Islamic Courts Union; the ICU subsequently splintered into more radical groups such as Al-Shabaab, which battled the TFG and its AMISOM allies for control of the region. By mid-2012, the insurgents had lost most of the territory that they had seized, a search for more permanent democratic institutions began. A new provisional constitution was passed in August 2012; the same month, the Federal Government of Somalia was formed and a period of reconstruction began in Mogadishu. Somalia has maintained an informal economy based on livestock, remittances from Somalis working abroad, telecommunications, it is a member of the United Nations, the Arab League, African Union, Non-Aligned Movement and the Organisation of Islamic Cooperation.
Somalia has been inhabited since at least the Paleolithic. During the Stone Age, the Doian and Hargeisan cultures flourished here; the oldest evidence of burial customs in the Horn of Africa comes from cemeteries in Somalia dating back to the 4th millennium BCE. The stone implements from the Jalelo site in the north were characterized in 1909 as important artefacts demonstrating the archaeological universality during the Paleolithic between the East and the West. According to linguists, the first Afroasiatic-speaking populations arrived in the region during the ensuing Neolithic period from the family's proposed urheimat in the Nile Valley, or the Near East; the Laas Geel complex on the outskirts of Hargeisa in northwestern Somalia dates back 5,000 years, has rock art depicting both wild animals and decorated cows. Other cave paintings are found in the northern Dhambalin region, which feature one of the earliest known depictions of a hunter on horseback; the rock art is in the distinctive Ethiopian-Arabian style, dated to 1,000 to 3,000 BCE.
Additionally, between the towns of Las Khorey and El Ayo in northern Somalia lies Karinhegane, the site of numerous cave paintings of real and mythical animals. Each painting has an inscription below it, which collectively have been estimated to be around 2,500 years old. Ancient pyramidical structures, ruined cities and stone walls, such as the Wargaade Wall, are evidence of an old civilization that once thrived in the Somali peninsula; this civilization enjoyed a trading relationship with ancient Egypt and Mycenaean Greece since the second millennium BCE, supporting the hypothesis that Somalia or adjacent regions were the location of the ancient Land of Punt. The Puntites traded myrrh, gold, short-horned cattle and frankincense with the Egyptians, Babylonians, Indians and Romans through their commercial ports. An Egyptian expedition sent to Punt by the 18th dynasty Queen Hatshepsut is recorded on the temple reliefs at Deir el-Bahari, during the reign of the Puntite King Parahu and Queen Ati.
In 2015, isotopic analysis of ancient baboon mummies from Punt, brought to Egypt as gifts indicated that the specimens originated from an area encompassing eastern Somalia and the Eritrea-Ethiopia corridor. In the classical era, the Macrobians, who may have b
Finland the Republic of Finland, is a country in Northern Europe bordering the Baltic Sea, Gulf of Bothnia, Gulf of Finland, between Norway to the north, Sweden to the northwest, Russia to the east. Finland is situated in the geographical region of Fennoscandia; the capital and largest city is Helsinki. Other major cities are Espoo, Tampere and Turku. Finland's population is 5.52 million, the majority of the population is concentrated in the southern region. 88.7% of the population is Finnish and speaks Finnish, a Uralic language unrelated to the Scandinavian languages. Finland is the eighth-largest country in Europe and the most sparsely populated country in the European Union; the sovereign state is a parliamentary republic with a central government based in the capital city of Helsinki, local governments in 311 municipalities, one autonomous region, the Åland Islands. Over 1.4 million people live in the Greater Helsinki metropolitan area, which produces one third of the country's GDP. Finland was inhabited when the last ice age ended 9000 BCE.
The first settlers left behind artefacts that present characteristics shared with those found in Estonia and Norway. The earliest people were hunter-gatherers; the first pottery appeared in 5200 BCE. The arrival of the Corded Ware culture in southern coastal Finland between 3000 and 2500 BCE may have coincided with the start of agriculture; the Bronze Age and Iron Age were characterised by extensive contacts with other cultures in the Fennoscandian and Baltic regions and the sedentary farming inhabitation increased towards the end of Iron Age. At the time Finland had three main cultural areas – Southwest Finland and Karelia – as reflected in contemporary jewellery. From the late 13th century, Finland became an integral part of Sweden through the Northern Crusades and the Swedish part-colonisation of coastal Finland, a legacy reflected in the prevalence of the Swedish language and its official status. In 1809, Finland was incorporated into the Russian Empire as the autonomous Grand Duchy of Finland.
In 1906, Finland became the first European state to grant all adult citizens the right to vote, the first in the world to give all adult citizens the right to run for public office. Following the 1917 Russian Revolution, Finland declared itself independent. In 1918, the fledgling state was divided by civil war, with the Bolshevik-leaning Red Guard supported by the new Soviet Russia, fighting the White Guard, supported by the German Empire. After a brief attempt to establish a kingdom, the country became a republic. During World War II, the Soviet Union sought to occupy Finland, with Finland losing parts of Karelia, Kuusamo and some islands, but retaining their independence. Finland established an official policy of neutrality; the Finno-Soviet Treaty of 1948 gave the Soviet Union some leverage in Finnish domestic politics during the Cold War era. Finland joined the OECD in 1969, the NATO Partnership for Peace in 1994, the European Union in 1995, the Euro-Atlantic Partnership Council in 1997, the Eurozone at its inception, in 1999.
Finland was a relative latecomer to industrialisation, remaining a agrarian country until the 1950s. After World War II, the Soviet Union demanded war reparations from Finland not only in money but in material, such as ships and machinery; this forced Finland to industrialise. It developed an advanced economy while building an extensive welfare state based on the Nordic model, resulting in widespread prosperity and one of the highest per capita incomes in the world. Finland is a top performer in numerous metrics of national performance, including education, economic competitiveness, civil liberties, quality of life, human development. In 2015, Finland was ranked first in the World Human Capital and the Press Freedom Index and as the most stable country in the world during 2011–2016 in the Fragile States Index, second in the Global Gender Gap Report, it ranked first on the World Happiness Report report for 2018 and 2019. A large majority of Finns are members of the Evangelical Lutheran Church, freedom of religion is guaranteed under the Finnish Constitution.
The earliest written appearance of the name Finland is thought to be on three runestones. Two have the inscription finlonti; the third was found in Gotland. It dates back to the 13th century; the name can be assumed to be related to the tribe name Finns, mentioned at first known time AD 98. The name Suomi has uncertain origins, but a candidate for a source is the Proto-Baltic word *źemē, meaning "land". In addition to the close relatives of Finnish, this name is used in the Baltic languages Latvian and Lithuanian. Alternatively, the Indo-European word * gʰm-on "man" has been suggested; the word referred only to the province of Finland Proper, to the northern coast of Gulf of Finland, with northern regions such as Ostrobothnia still sometimes being excluded until later. Earlier theories suggested derivation from suomaa or suoniemi, but these are now considered outdated; some have suggested common etymology with saame and Häme, but that theory is uncertain
A runestone is a raised stone with a runic inscription, but the term can be applied to inscriptions on boulders and on bedrock. The tradition began in the 4th century and lasted into the 12th century, but most of the runestones date from the late Viking Age. Most runestones are located in Scandinavia, but there are scattered runestones in locations that were visited by Norsemen during the Viking Age. Runestones are memorials to dead men. Runestones were brightly coloured when erected, though this is no longer evident as the colour has worn off. Most Runestones are found in present day Sweden; the tradition of raising stones that had runic inscriptions first appeared in the 4th and 5th century, in Norway and Sweden, these early runestones were placed next to graves. The earliest Danish runestones appeared in the 8th and 9th centuries, there are about 50 runestones from the Migration Period in Scandinavia. Most runestones were erected during the period 950-1100 CE, they were raised in Sweden, to a lesser degree in Denmark and Norway.
The tradition is mentioned in both Ynglinga saga and Hávamál: For men of consequence a mound should be raised to their memory, for all other warriors, distinguished for manhood a standing stone, a custom that remained long after Odin's time. —The Ynglinga saga What may have increased the spread of runestones was an event in Denmark in the 960s. King Harald Bluetooth had just been baptised and in order to mark the arrival of a new order and a new age, he commanded the construction of a runestone; the inscription reads King Haraldr ordered this monument made in memory of Gormr, his father, in memory of Þyrvé, his mother. The runestone has three sides. On one side, there is an animal, the prototype of the runic animals that would be engraved on runestones, on another side there is Denmark's oldest depiction of Jesus. Shortly after this stone had been made, something happened in Scandinavia's runic tradition. Scores of chieftains and powerful Norse clans consciously tried to imitate King Harald, from Denmark a runestone wave spread northwards through Sweden.
In most districts, the fad died out after a generation, but, in the central Swedish provinces of Uppland and Södermanland, the fashion lasted into the 12th century. There are about 3,000 runestones among the about 6,000 runic inscriptions in Scandinavia. There are runestones in other parts of the world as the tradition of raising runestones followed the Norsemen wherever they went, from the Isle of Man in the west to the Black Sea in the east, from Jämtland in the north to Schleswig in the south; the runestones are unevenly distributed in Scandinavia: Denmark has 250 runestones, Norway has 50 while Iceland has none. Sweden has as many as between 2,500 depending on definition; the Swedish district of Uppland has the highest concentration with as many as 1,196 inscriptions in stone, whereas Södermanland is second with 391. Outside of Scandinavia, the Isle of Man stands out with its 30 runestones from the 9th century and early 11th century. Scattered runestones have been found in England, Ireland and the Faroe Islands.
With the exception of the runestone on Berezan', there are no runestones in Eastern Europe, due to a lack of available stones and the fact that the local population did not treat the foreigners' stones with much respect. Runestones were placed on selected spots in the landscape, such as assembly locations, bridge constructions, fords. In medieval churches, there are runestones that have been inserted as construction material, it is debated whether they were part of the church location or had been moved there. In southern Scania, runestones can be tied to large estates that had churches constructed on their land. In the Mälaren Valley, the runestones appear to be placed so that they mark essential parts of the domains of an estate, such as courtyard, grave field, borders to neighbouring estates. Runestones appear as single monuments and more as pairs. In some cases, they are part of larger monuments together with other raised stones. However, although scholars know where 95% of all runestones were discovered, only about 40% were discovered in their original location.
The remainder have been found in churches, bridges, graves and water routes. On the other hand, scholars agree that the stones were not moved far from their original sites. In many districts, 50% of the stone inscriptions have traces of Christianity, but, in Uppland, which has the highest concentration of runic inscriptions in the world, about 70% of the 1,196 stone inscriptions are explicitly Christian, shown by engraved crosses or added Christian prayers, only a few runestones are not Christian. Scholars have suggested that the reason why so many Christian runestones were raised in Uppland is that the district was the focal point in the conflict between Norse paganism and the newly Christianized King of Sweden, it is possible that the chieftains tried to demonstrate their allegiance to the king and to display their Christian faith to the world and to God by adding Christian crosses and prayers on their runestones. What speaks against this theory is the fact that Norway, Götaland did not have any corresponding development in the runestone tradition.
Moreover, not a single runestone declares. Additionally, the runestones appear to show. According to another theory, it was a social fashion, popular among