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This change in compression formed the Baetic Cordillera on the Mediterranean coast in the Middle Miocene. Basins were inverted and raised up in the Iberian Central System, and also the Alboran Basin. The crust still continues to fold in these areas since the Pliocene. Some coastal areas have been uplifted hundreds of meters in the Pliocene.
Europe in 1000, with most European states already formed. The Holy Roman Empire emerged around 800, as Charlemagne, King of the Franks and part of the Carolingian dynasty, was crowned by the pope as emperor. His empire based in modern France, the Low Countries and Germany expanded into modern Hungary, Italy, Bohemia, Lower Saxony
These people would become the Gallaeci (a group of Celtic tribes), and they would be conquered by the Roman Empire in the first and second centuries AD. As the Roman Empire declined, Galicia would be conquered and ruled by various Germanic tribes, notably the Suebi and Visigoths, until the 9th century. Then the Muslim conquest of Iberia reached ...
A cordillera is a small chain and/or network system of mountain ranges, such as those in the west coast of the Americas. The term is borrowed from Spanish , where the word comes from cordilla , a diminutive of cuerda ('rope').
The inhabitants of the empire, now generally termed Byzantines, thought of themselves as Romans (Romaioi).Their Islamic neighbours similarly called their empire the "land of the Romans" (Bilād al-Rūm), but the people of medieval Western Europe preferred to call them "Greeks" (Graeci), due to having a contested legacy to Roman identity and to associate negative connotations from ancient Latin ...
Baltica is a paleocontinent that formed in the Paleoproterozoic and now constitutes northwestern Eurasia, or Europe north of the Trans-European Suture Zone and west of the Ural Mountains. The thick core of Baltica, the East European Craton, is more than three billion years old and formed part of the Rodinia supercontinent at c. 1 Ga. [1]
The Scandinavian Monetary Union was a monetary union formed by Sweden and Denmark on 5 May 1873, by fixing their currencies against the gold standard at par to each other. Norway, which was in union with Sweden entered the union two years later, in 1875 by pegging its currency to gold at the same level as Denmark and Sweden (.403 grams [2] ).
The Rhenohercynian basin, a back-arc basin, formed at the southern margin of Euramerica just after the Caledonian orogeny. According to these authors, a small rim from Euramerica rifted off when this basin formed. The basin closed when these Caledonian deformed terranes were accreted again to Laurussia during the Hercynian orogeny. [45]