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Baltica redirects here. For the Russian beer, see Baltika Breweries

Baltica in 550 mya (green)
Baltica in 550 mya (green)

Baltica is a name applied by geologists to a Late Proterozoic-Early Palaeozoic continent that now includes the East European craton of northwestern Eurasia. Russian beer (Russian пиво &ndash Pivo in Russia beer is number two alcoholic drink after Vodka, but is seen by many as a healthier almost non-alcoholic alternative Baltika redirects here For the football club see FC Baltika Kaliningrad Baltika Brewery () is the largest brewery In Astronomy, Geology, and Paleontology, mya or " mya " is an abbreviation for "million years ago". The Proterozoic (ˌproʊtərəˈzoʊɪk is a geological eon representing a period before the first abundant complex life on Earth. The Paleozoic or Palaeozoic Era (from the Greek palaio (παλαιο "old" and zoe (ζωη "life" meaning "ancient life" A continent is one of several large Landmasses on Earth. They are generally identified by Convention rather than any strict criteria with seven regions The East European craton is the core of the Baltica proto- plate and consists of three crustal regions/segments Fennoscandia to the northwest Volgo-Uralia For the superstate in George Orwell 's novel see Nations of Nineteen Eighty-Four. Baltica was created as an entity not earlier than 1. 8 billion years ago. Before this time, the three segments/continents that now comprise the East European craton were in different places on the globe. Baltica existed on a tectonic plate called the Baltic Plate. Plate tectonics (from Greek τέκτων tektōn "builder" or "mason" describes the large scale motions of Earth 's Lithosphere The Baltic Plate was an ancient Tectonic plate that existed from the Cambrian period to the Carboniferous period.

Partial history of Baltica in chronological order

See also

The Baltic Shield (sometimes referred to as the Fennoscandian Shield) is located in Fennoscandia ( Norway, Sweden and Finland) northwest The Baltic Plate was an ancient Tectonic plate that existed from the Cambrian period to the Carboniferous period.
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