Uppland is a historical province or landskap on the eastern coast of Sweden, just north of Stockholm, the capital. It borders Södermanland, Västmanland and Gästrikland. It is also bounded by lake Mälaren and the Baltic Sea.
The name literally means up land, a name which is commonly encountered in especially older English literature as Upland. Its Latinised form, which is occasionally used, is Uplandia.
Fyrisån (Swedish pronunciation: [ˈfŷːrɪsˌoːn], "the Fyris river") is a river in the Swedish province of Uppland, which passes through the city of Uppsala and ends in Lake Mälaren.
The "Sala" river in Uppland was changed in the 17th century in memory of the Fyrisvellir battle, mentioned in the Icelandic sagas, as it was the belief that the marshy plains called "Föret" was the site of the famous Battle of Fýrisvellir in the late 10th century.
Danegeld (/ˈdeɪnɡɛld/; literally "Dane yield") was a tax raised to pay tribute or protection money to the Viking raiders to save a land from being ravaged. It was called the geld or gafol in eleventh-century sources. It was characteristic of royal policy in both England and Francia during the ninth through eleventh centuries, collected both as tributary, to buy off the attackers, and as stipendiary, to pay the defensive forces. The term Danegeld did not appear until the late eleventh century. In Anglo-Saxon England tribute payments to the Danes was known as gafol and the levy raised to support the standing army, for the defence of the realm, was known as heregeld (army-tax).
Mälaren (UK: /ˈmɛlərɛn/ MEL-ər-en, US: /ˈmeɪlɑːrən/ MAY-lar-ən, Swedish: [ˈmɛ̂ːlarɛn] or [ˈmɛ̂ːlaɳ]), historically referred to as Lake Malar in English, is the third-largest freshwater lake in Sweden (after Vänern and Vättern). Its area is 1,140 km (440 sq mi) and its greatest depth is 64 m (210 ft). Mälaren spans 120 km (74.6 mi) from east to west. The lake drains, from south-west to north-east, into the Baltic Sea through its natural outlets Norrström and Söderström (as it flows around Stadsholmen island) and through the artificial Södertälje Canal and Hammarbyleden waterway. The easternmost bay of Mälaren, in central Stockholm, is called Riddarfjärden. The lake is located in Svealand and bounded by the provinces of Uppland, Södermanland and Västmanland. The two largest islands in Mälaren are Selaön (91 km (35.1 sq mi)) and Svartsjölandet (79 km (30.5 sq mi)). Mälaren is low-lying and mostly relatively shallow.
Being a quite narrow and shallow lake, Mälaren has bridge crossings between Eskilstuna and Västerås with two crossings on the western end at Kvicksund and three separate bridges between Strängnäs and Enköping in the central part of the lake. On the eastern end, the entirety of Ekerö Municipality is set on islands within Mälaren. That urban area also has a bridge connection to the mainland in Stockholm along with bridges between various islands in the municipality.
The First Swedish Crusade was a possibly mythical military expedition in the 1150s to Southwestern Finland by Swedish King Eric IX and English Bishop Henry of Uppsala.
The earliest written sources of the crusade are from the late 13th century. The main sources of the crusade, the legend of Saint Erik and the legend of Saint Henry, describe the crusade as caused by the multiple raids of pagan Finns on Sweden.
In Scandinavian prehistory, sometimes specifically Swedish prehistory, the Vendel Period, or Vendel Age (Swedish: Vendeltiden; c. 540–790 AD) appears between the Migration Period and the Viking Age. The name is taken from the rich boat inhumation cemetery at Vendel parish church, Uppland. Unlike the preceding and succeeding eras, the Vendel Period left very few precious metal artifacts or runic inscriptions. Instead, it is extremely rich in animal art on copper-alloy objects. It is also known for guldgubbar, tiny embossed gold foil images, and elaborate helmets with embossed decoration similar to the one found at Sutton Hoo in England.
During the period, Swedish expeditions began to explore the waterways of territories which later became Russia, Ukraine, and Belarus. The Elder Futhark writing system was abandoned in favor of the Younger Futhark, virtually simultaneously over the whole of Scandinavia. Some runestones survive, most notably those at Rök and Sparlösa, both from c. 800. Other written sources are few and hard to interpret: a few Icelandic sagas, the tale of Beowulf, and accounts from some southern European writers. Earlier Swedish historians tried to make use of these to create a coherent history, but this effort has largely been abandoned, and the period is now mostly studied by archaeologists.
59°31′30″N 18°24′30″E / 59.52488°N 18.40820°E
Roslagen is a coastal area in eastern Uppland in Sweden. It constitutes the northern part of the Stockholm archipelago and extends north along the coast. The old designation for the area was Roden.
In Old Norse sources, such as sagas and runestones, Serkland (also Særkland, Srklant, Sirklant, Serklat, etc.) was the "land of the Serkir", usually identified with the Saracens.
The exact etymology is disputed. Serk- may derive from "Saracen"; from sericum, Latin for "silk", implying a connection with the Silk Road; from the Khazar fortress of Sarkel; or from serkr, shirt or gown, i.e., "land of the gown-wearers". In all cases it refers to a land in the East. Originally, it referred to the land south of the Caspian Sea, but it gradually expanded to cover all Islamic lands, including parts of Africa (and possibly even Muslim Sicily).
An esker, eskar, eschar, or os, sometimes called an asar, osar, or serpent kame, is a long, winding ridge of stratified sand and gravel, examples of which occur in glaciated and formerly glaciated regions of Europe and North America. They are most often formed by the deposition of sediment at the bottom of ice-walled channels within or beneath a former glacier. As a glacier retreats, the channel walls melt while the accumulated sediment remains, slumping into ridges as the only remaining evidence of the former channel path. They represent an unusual form of sedimentation where the location of the former channel is higher than the surrounding landform. Eskers are frequently several kilometres long and, because of their uniform shape, look like railway embankments.