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A moraine is any accumulation of unconsolidated debris ( regolith and rock ), sometimes referred to as glacial till , that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour . Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines ( till -covered areas forming sheets on flat or irregular topography ) and medial moraines (moraines formed where two glaciers meet).

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68-587: Sven is a Scandinavian masculine first name. In Old Norse the meaning was "young man" or "servant" and the original Old Norse spelling was sveinn . Variants such as Svend are found in Danish and Norwegian . Another variant, Svein is used only in the Low Countries and German-speaking countries , and is cognate with the English surname Swain . In medieval Swedish, sven or sven av vapen "sven of arms",

136-584: A loanword from the North Germanic languages ; " Skaði " is the jötunn stepmother of Freyr and Freyja in Norse mythology . It has been suggested that Skaði to some extent is modelled on a Sámi woman. The name for Skaði's father Þjazi is known in Sámi as Čáhci , "the waterman"; and her son with Odin, Sæmingr , can be interpreted as a descendant of Saam , the Sámi population. Older joik texts give evidence of

204-598: A brief but disastrous war between Denmark and Prussia (supported by Austria). Schleswig-Holstein was conquered by Prussia and after Prussia's success in the Franco-Prussian War a Prussian-led German Empire was created and a new power -balance in the Baltic region was established. The Scandinavian Monetary Union , established in 1873, lasted until World War I . The term Scandinavia (sometimes specified in English as Continental Scandinavia or mainland Scandinavia )

272-407: 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

340-483: A modern and more inclusive demonym . In the ethnic or cultural sense the term Scandinavian traditionally refers to speakers of Scandinavian languages , who are mainly descendants of the peoples historically known as Norsemen , but also to some extent of immigrants and others who have been assimilated into that culture and language. In this sense the term refers primarily to native Danes , Norwegians and Swedes as well as descendants of Scandinavian settlers such as

408-452: 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. In permafrost areas an advancing glacier may push up thick layers of frozen sediments at its front. An arctic push moraine will then be formed. A medial moraine

476-569: A visit to Sweden, Andersen became a supporter of early political Scandinavism. In a letter describing the poem to a friend, he wrote: "All at once I understood how related the Swedes, the Danes and the Norwegians are, and with this feeling I wrote the poem immediately after my return: 'We are one people, we are called Scandinavians! ' ". The influence of Scandinavism as a Scandinavist political movement peaked in

544-734: Is 38.0 °C in Målilla (Sweden). The coldest temperature ever recorded is −52.6 °C in Vuoggatjålme , Arjeplog (Sweden). The coldest month was February 1985 in Vittangi (Sweden) with a mean of −27.2 °C. Southwesterly winds further warmed by foehn wind can give warm temperatures in narrow Norwegian fjords in winter. Tafjord has recorded 17.9 °C in January and Sunndal 18.9 °C in February. The words Scandinavia and Scania ( Skåne ,

612-567: Is Finnish (usually from the 3rd grade), while for Finnish-speakers it is Swedish (usually from the 3rd, 5th or 7th grade). Finnish speakers constitute a language minority in Sweden and Norway. Meänkieli and Kven are Finnish dialects spoken in Swedish Lapland and Norwegian Lapland . The Sámi languages are indigenous minority languages in Scandinavia. They belong to their own branch of

680-514: Is a phonotactic structure of alien origin. Although the term Scandinavia used by Pliny the Elder probably originated in the ancient Germanic languages, the modern form Scandinavia does not descend directly from the ancient Germanic term. Rather the word was brought into use in Europe by scholars borrowing the term from ancient sources like Pliny, and was used vaguely for Scania and the southern region of

748-490: 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 (which excludes Denmark but includes a part of northern Finland ). In English usage, Scandinavia is sometimes used as a synonym for Nordic countries . Iceland and

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816-631: Is a ridge of moraine that runs down the center of a valley floor. 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 , Yukon , 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

884-581: Is a term for squire . The female equivalent, Svenja , though seemingly Dutch and Scandinavian, is not common anywhere outside of German-speaking countries. Sven can also be spelled with a "w" - Swen - but is pronounced as Sven. The Icelandic version is Sveinn ( Icelandic pronunciation: [ˈsveitn̥] ); the Faroese version is Sveinur ( Faroese pronunciation: [ˈsvaiːnʊɹ] ). Scandinavia Nordic territories that are not part of Scandinavia: Chronological history Scandinavia

952-407: Is also due to the fact that that Swedish was the dominant language when Finland was part of Sweden. Finnish-speakers had to learn Swedish in order to advance to higher positions. Swedish spoken in today's Finland includes a lot of words that are borrowed from Finnish, whereas the written language remains closer to that of Sweden. Finland is officially bilingual, with Finnish and Swedish having mostly

1020-579: Is based on the degree of mutual comprehensibility between the languages in the two branches. The populations of the Scandinavian countries, with common Scandinavian roots in language, can—at least with some training—understand each other's standard languages as they appear in print and are heard on radio and television. The reason Danish, Swedish and the two official written versions of Norwegian ( Nynorsk and Bokmål ) are traditionally viewed as different languages, rather than dialects of one common language,

1088-547: Is because they have two official written standards, in addition to the habit of strongly holding on to local dialects. The people of Stockholm , Sweden and Copenhagen , Denmark have the greatest difficulty in understanding other Scandinavian languages. In the Faroe Islands and Iceland, learning Danish is mandatory. This causes Faroese people as well as Icelandic people to become bilingual in two very distinct North Germanic languages, making it relatively easy for them to understand

1156-555: Is different from usage in the Scandinavian languages themselves (which use Scandinavia in the narrow meaning), and by the fact that the question of whether a country belongs to Scandinavia is politicised. People from the Nordic world beyond Norway, Denmark and Sweden may be offended at being either included in or excluded from the category of "Scandinavia". Nordic countries is used unambiguously for Denmark, Norway, Sweden, Finland and Iceland, including their associated territories Greenland,

1224-466: Is ordinarily used locally for Denmark, Norway and Sweden as a subset of the Nordic countries (known in Norwegian, Danish , and Swedish as Norden ; Finnish : Pohjoismaat , Icelandic : Norðurlöndin , Faroese : Norðurlond ). However, in English usage, the term Scandinavia is sometimes used as a synonym or near-synonym for what are known locally as Nordic countries . Usage in English

1292-649: Is still a hotly debated issue, both in scholarly discussions and in the nationalistic discourse of various European countries. The form Scadinavia as the original home of the Langobards appears in Paul the Deacon ' Historia Langobardorum , but in other versions of Historia Langobardorum appear the forms Scadan , Scandanan , Scadanan and Scatenauge . Frankish sources used Sconaowe and Aethelweard , an Anglo-Saxon historian, used Scani . In Beowulf ,

1360-659: Is that each is a well-established standard language in its respective country. Danish, Swedish and Norwegian have since medieval times been influenced to varying degrees by Middle Low German and standard German. That influence was due not only to proximity, but also to the rule of Denmark—and later Denmark-Norway—over the German-speaking region of Holstein, and to Sweden's close trade with the Hanseatic League . Norwegians are accustomed to variation and may perceive Danish and Swedish only as slightly more distant dialects. This

1428-510: The European Charter for Regional or Minority Languages . A key ancient description of Scandinavia was provided by Pliny the Elder , though his mentions of Scatinavia and surrounding areas are not always easy to decipher. Writing in the capacity of a Roman admiral, he introduces the northern region by declaring to his Roman readers that there are 23 islands "Romanis armis cognitae" ("known to Roman arms") in this area. According to Pliny,

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1496-479: 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 geography of the region is varied, from the Norwegian fjords in the west and Scandinavian mountains covering parts of Norway and Sweden, to

1564-575: The Icelanders and the Faroese . The term is also used in this ethnic sense, to refer to the modern descendants of the Norse, in studies of linguistics and culture. Additionally the term Scandinavian is used demonymically to refer to all modern inhabitants or citizens of Scandinavian countries. Within Scandinavia the demonymic term primarily refers to inhabitants or citizens of Denmark, Norway and Sweden. In English usage inhabitants or citizens of Iceland,

1632-661: The Savoyard Italian morena ('mound of earth'). Morena in this case was derived from Provençal morre ('snout'), itself from Vulgar Latin * murrum ('rounded object'). The term was introduced into geology by Horace Bénédict de Saussure in 1779. Moraines are landforms composed of glacial till deposited primarily by glacial ice. Glacial till, in turn, is unstratified and unsorted debris ranging in size from silt -sized glacial flour to large boulders. The individual rock fragments are typically sub-angular to rounded in shape. Moraines may be found on

1700-574: The Scandinavian Peninsula since prehistory—the North Germanic languages (Scandinavian languages) and the Uralic languages , Sámi and Finnish . Most people in Scandinavia today speak Scandinavian languages that evolved from Old Norse , originally spoken by ancient Germanic tribes in southern Scandinavia. The Continental Scandinavian languages— Danish , Norwegian and Swedish —form a dialect continuum and are considered mutually intelligible. The Insular Scandinavian languages— Faroese and Icelandic —on

1768-693: The Sámi people in northern Scandinavia. The North Germanic languages of Scandinavia are traditionally divided into an East Scandinavian branch (Danish and Swedish) and a West Scandinavian branch (Norwegian, Icelandic and Faroese), but because of changes appearing in the languages since 1600 the East Scandinavian and West Scandinavian branches are now usually reconfigured into Insular Scandinavian ( ö-nordisk / øy-nordisk ) featuring Icelandic and Faroese and Continental Scandinavian ( Skandinavisk ), comprising Danish, Norwegian and Swedish. The modern division

1836-431: The Uralic language family and are unrelated to the North Germanic languages other than by limited grammatical (particularly lexical) characteristics resulting from prolonged contact. Sámi is divided into several languages or dialects. Consonant gradation is a feature in both Finnish and northern Sámi dialects, but it is not present in southern Sámi, which is considered to have a different language history. According to

1904-460: The "clarissima" ("most famous") of the region's islands is Scatinavia , of unknown size. There live the Hilleviones . The belief that Scandinavia was an island became widespread among classical authors during the 1st century and dominated descriptions of Scandinavia in classical texts during the centuries that followed. Pliny begins his description of the route to Scatinavia by referring to

1972-519: The Faroe Islands and Finland are sometimes included as well. English general dictionaries often define the noun Scandinavian demonymically as meaning any inhabitant of Scandinavia (which might be narrowly conceived or broadly conceived). There is a certain ambiguity and political contestation as to which peoples should be referred to as Scandinavian in this broader sense. Sámi people who live in Norway and Sweden are generally included as Scandinavians in

2040-674: The Faroe Islands and the Åland Islands. The geological term Fennoscandia (sometimes Fennoscandinavia ) refers to the Fennoscandian Shield (or Baltic Shield ), which includes the Scandinavian Peninsula, Finland and Karelia , and excludes Denmark and other parts of the wider Nordic world. The terms Fennoscandia and Fennoscandinavia are sometimes used in a political sense to refer to Norway, Sweden, Denmark, and Finland. The term Scandinavian may be used with two principal meanings, in an ethnic or cultural sense and as

2108-519: The Finnish population. The coastal province of Ostrobothnia has a Swedish-speaking majority, whereas plenty of areas on this coastline are nearly unilingually Finnish, like the region of Satakunta . Åland, an autonomous province of Finland situated in the Baltic Sea between Finland and Sweden, are entirely Swedish-speaking. Children are taught the other official language at school: for Swedish-speakers this

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2176-579: The Rogen moraines look like tigerstripes on aerial photographs . Rogen moraines are named after Lake Rogen in Härjedalen , Sweden , the landform's type locality. Closely related to Rogen moraines, de Geer moraines are till ridges up to 5m high and 10–50m wide running perpendicular to the ice flow. They occur in large groups in low-lying areas. Named for Gerard De Geer , who first described them in 1889, these moraines may have developed from crevasses underneath

2244-556: The Russian Grand Duchy of Finland in 1809 and Norway ( de jure in union with Denmark since 1387, although de facto treated as a province) becoming independent in 1814, but thereafter swiftly forced to accept a personal union with Sweden. The dependent territories Iceland, the Faroe Islands and Greenland, historically part of Norway, remained with Denmark in accordance with the Treaty of Kiel . Sweden and Norway were thus united under

2312-497: The Swedish king Gustav I led Sweden to independence. It also saw numerous wars between the nations, which shaped the modern borders. The most recent union was the union between Sweden and Norway , which ended in 1905. In modern times the region has prospered, with the economies of the countries being amongst the strongest in Europe. Sweden, Denmark, Norway, Iceland, and Finland all maintain welfare systems considered to be generous, with

2380-541: The Swedish monarch, but Finland's inclusion in the Russian Empire excluded any possibility for a political union between Finland and any of the other Nordic countries. The end of the Scandinavian political movement came when Denmark was denied the military support promised from Sweden and Norway to annex the (Danish) Duchy of Schleswig , which together with the (German) Duchy of Holstein had been in personal union with Denmark. The Second war of Schleswig followed in 1864,

2448-706: The Sámi Information Centre of the Sámi Parliament of Sweden , southern Sámi may have originated in an earlier migration from the south into the Scandinavian Peninsula. German is a recognized minority language in Denmark. Recent migrations has added even more languages. Apart from the Sámi languages and the languages of minority groups speaking a variant of the majority language of a neighboring state, Yiddish , Romani Chib/Romanes, Scandoromani and Karelian are amongst those protected in parts of Scandinavia under

2516-491: 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, and most moraines record a continuum of processes. Reworking of moraines may lead to the formation of placer deposits of gold as is the case of southernmost Chile . Moraines can be classified either by origin, location with respect to

2584-408: The base of the ice as lodgment till with a thin and discontinuous upper layer of supraglacial till deposited as the glacier retreats. It typically is found in the areas between end moraines. 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

2652-408: The demonymic sense; the Sámi of Finland may be included in English usage, but usually not in local usage; the Sámi of Russia are not included. However, the use of the term "Scandinavian" with reference to the Sámi is complicated by the historical attempts by Scandinavian majority peoples and governments in Norway and Sweden to assimilate the Sámi people into the Scandinavian culture and languages, making

2720-617: The economic and social policies of the countries being dubbed the " Nordic model ". The geography of Scandinavia is extremely varied. Notable are the Norwegian fjords , the Scandinavian Mountains covering much of Norway and parts of Sweden, the flat, low areas in Denmark and the archipelagos of Finland, Norway and Sweden. Finland and Sweden have many lakes and moraines , legacies of the ice age , which ended about ten millennia ago. The southern regions of Scandinavia, which are also

2788-532: The first Europeans to reach North America. These exploits saw the establishment of the North Sea Empire which comprised large parts of Scandinavia and Great Britain, though it was relatively short-lived. Scandinavia was eventually Christianized , and the coming centuries saw various unions of Scandinavian nations, most notably the Kalmar Union of Denmark, Norway and Sweden, which lasted for over 100 years until

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2856-618: The forms Scedenige and Scedeland are used while the Alfredian translation of Orosius and Wulfstan 's travel accounts used the Old English Sconeg . The earliest Sámi joik texts written down refer to the world as Skadesi-suolu in Northern Sámi and Skađsuâl in Skolt Sámi , meaning " Skaði 's island". Svennung considers the Sámi name to have been introduced as

2924-493: 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: terminal and recessional. Terminal moraines mark the maximum advance of the glacier. Recessional moraines are small ridges left as a glacier pauses during its retreat. After a glacier retreats, the end moraine may be destroyed by postglacial erosion. Recessional moraines are often observed as

2992-442: 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, and the location on the glacier in which the moraine is formed. Moraine forming processes may be loosely divided into passive and active . Passive processes involve the placing of chaotic supraglacial sediments onto

3060-401: The goddess Skaði may have once been a personification of the geographical region of Scandinavia or associated with the underworld. Another possibility is that all or part of the segments of the name came from the pre-Germanic Mesolithic people inhabiting the region. In modernity, Scandinavia is a peninsula, but between approximately 10,300 and 9,500 years ago the southern part of Scandinavia

3128-449: The ice sheet. The Kvarken has a very high density of de Geer moraines. End moraines, or terminal moraines , are ridges of unconsolidated debris deposited at the snout or end of the glacier. They usually 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

3196-463: The inclusion of the Sámi as "Scandinavians" controversial among many Sámi. Modern Sámi politicians and organizations often stress the status of the Sámi as a people separate from and equal to the Scandinavians, with their own language and culture, and are apprehensive about being included as "Scandinavians" in light of earlier Scandinavian assimilation policies. Two language groups have coexisted on

3264-417: The landscape with limited reworking, typically 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 often composed of till and reworked proglacial sediment. Moraine may also form by

3332-428: The language of the church and law courts remained Icelandic. The Scandinavian languages are (as a language family) unrelated to Finnish and the Sámi languages , which as Uralic languages are distantly related each other. Owing to the close proximity, there is still a great deal of borrowing from the Swedish and Norwegian languages in Finnish and the Sámi. The long history of linguistic influence of Swedish on Finnish

3400-515: The low and flat areas of Denmark in the south, as well as archipelagos and lakes in the east. Most of the population in the region live in the more temperate southern regions, with the northern parts having long, cold winters. The region became notable during the Viking Age , when Scandinavian peoples participated in large-scale raiding, conquest, colonization and trading mostly throughout Europe. They also used their longships for exploration, becoming

3468-652: The middle of the 19th century, between the First Schleswig War (1848–1850) and the Second Schleswig War (1864). The Swedish king also proposed a unification of Denmark, Norway and Sweden into a single united kingdom. The background for the proposal was the tumultuous events during the Napoleonic Wars in the beginning of the century. This war resulted in Finland (formerly the eastern third of Sweden) becoming

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3536-507: The most populous regions, have a temperate climate . Scandinavia extends north of the Arctic Circle , but has relatively mild weather for its latitude due to the Gulf Stream . Many of the Scandinavian mountains have an alpine tundra climate. The climate varies from north to south and from west to east: a marine west coast climate ( Cfb ) typical of western Europe dominates in Denmark,

3604-588: The mountain of Saevo ( mons Saevo ibi ), the Codanus Bay ("Codanus sinus") and the Cimbrian promontory. The geographical features have been identified in various ways. By some scholars, Saevo is thought to be the mountainous Norwegian coast at the entrance to Skagerrak and the Cimbrian peninsula is thought to be Skagen , the north tip of Jutland , Denmark. As described, Saevo and Scatinavia can also be

3672-585: The northwestern coast. A small area along the northern coast east of the North Cape has tundra climate (Et) as a result of a lack of summer warmth. The Scandinavian Mountains block the mild and moist air coming from the southwest, thus northern Sweden and the Finnmarksvidda plateau in Norway receive little precipitation and have cold winters. Large areas in the Scandinavian mountains have alpine tundra climate. The warmest temperature ever recorded in Scandinavia

3740-415: The old Sámi belief about living on an island and state that the wolf is known as suolu gievra , meaning "the strong one on the island". The Sámi place name Sulliidčielbma means "the island's threshold" and Suoločielgi means "the island's back". In recent substrate studies, Sámi linguists have examined the initial cluster sk - in words used in the Sámi languages and concluded that sk -

3808-490: The other are only partially intelligible to speakers of the continental Scandinavian languages. The Uralic languages are linguistically unrelated to the Scandinavian languages. Finnish is the majority language in Finland, and a recognized minority language in Sweden. Meänkieli and Kven , sometimes considered as dialects of Finnish, are recognized minority languages in Sweden and Norway, respectively. The Sámi languages are indigenous minority languages in Scandinavia, spoken by

3876-519: The other two Mainland Scandinavian languages. Although Iceland was under the political control of Denmark until a much later date (1918), very little influence and borrowing from Danish has occurred in the Icelandic language. Icelandic remained the preferred language among the ruling classes in Iceland. Danish was not used for official communications, most of the royal officials were of Icelandic descent and

3944-428: The peninsula. The term was popularised by the linguistic and cultural Scandinavist movement , which asserted the common heritage and cultural unity of the Scandinavian countries and rose to prominence in the 1830s. The popular usage of the term in Sweden, Denmark and Norway as a unifying concept became established in the 19th century through poems such as Hans Christian Andersen 's "I am a Scandinavian" of 1839. After

4012-568: The region can also be found in Pytheas , Pomponius Mela , Tacitus , Ptolemy , Procopius and Jordanes , usually in the form of Scandza . It is believed that the name used by Pliny may be of West Germanic origin, originally denoting Scania. According to some scholars, the Germanic stem can be reconstructed as * skaðan- , meaning "danger" or "damage". The second segment of the name has been reconstructed as * awjō , meaning "land on

4080-471: 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 or from tributary streams flowing into the valley, or may be subglacial debris carried to the surface of the glacier, melted out, and transported to the glacier margin. Lateral moraines can rise up to 140 meters (460 ft) over

4148-464: The same place. Pliny mentions Scandinavia one more time: in Book VIII he says that the animal called achlis (given in the accusative, achlin , which is not Latin) was born on the island of Scandinavia. The animal grazes, has a big upper lip and some mythical attributes. Moraine The word moraine is borrowed from French moraine [mɔ.ʁɛn] , which in turn is derived from

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4216-563: The same status at national level. Finland's majority population are Finns , whose mother tongue is either Finnish (approximately 95%), Swedish or both. The Swedish-speakers live mainly on the coastline starting from approximately the city of Porvoo (Sw: Borgå) (in the Gulf of Finland) up to the city of Kokkola (Sw: Karleby) (in the Bay of Bothnia). The Swedish-speaking population is spread out in pockets in this coastal stretch and constitutes approximately 5% of

4284-406: The southernmost part of Sweden and along the west coast of Norway reaching north to 65°N, with orographic lift giving more mm/year precipitation (<5000 mm) in some areas in western Norway. The central part – from Oslo to Stockholm – has a humid continental climate (Dfb), which gradually gives way to subarctic climate (Dfc) further north and cool marine west coast climate (Cfc) along

4352-629: The southernmost province of Sweden) are both thought to go back to the Proto-Germanic compound * Skaðin-awjō (the ð represented in Latin by t or d ), which appears later in Old English as Scedenig and in Old Norse as Skáney . The earliest identified source for the name Scandinavia is Pliny the Elder 's Natural History , dated to the 1st century AD. Various references to

4420-419: The surface in the ablation zone , melting of surface ice or from debris that falls onto the glacier from valley sidewalls. Washboard moraines , also known as minor or corrugated moraines , are low-amplitude geomorphic features caused by glaciers. They consist of low-relief ridges, 1 to 2 meters (3 ft 3 in to 6 ft 7 in) in height and around 100 meters (330 ft) apart, accumulated at

4488-402: The valley floor, can be up to 3 kilometers (1.9 mi) long, and are steeper close to the glacier margin (up to 80 degrees) than further away (where slopes are typically 29 to 36 degrees. Ground moraines are till-covered areas with irregular topography and no ridges, often forming gently rolling hills or plains, with relief of less than 10 meters (33 ft). Ground moraine is accumulated at

4556-575: The water" or "island". The name Scandinavia would then mean "dangerous island", which is considered to refer to the treacherous sandbanks surrounding Scania. Skanör in Scania, with its long Falsterbo reef, has the same stem ( skan ) combined with - ör , which means "sandbanks". Alternatively, Sca(n)dinavia and Skáney , along with the Old Norse goddess name Skaði , may be related to Proto-Germanic * skaðwa- (meaning "shadow"). John McKinnell comments that this etymology suggests that

4624-607: Was an island separated from the northern peninsula, with water exiting the Baltic Sea through the area where Stockholm is now located. The Latin names in Pliny's text gave rise to different forms in medieval Germanic texts. In Jordanes' history of the Goths (AD 551), the form Scandza is the name used for their original home, separated by sea from the land of Europe (chapter 1, 4). Where Jordanes meant to locate this quasi-legendary island

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