Topics similar to or like Siberia (continent)

Ancient craton in the heart of Siberia. Wikipedia

Siberia
Extensive geographical region spanning much of Northern Asia. Siberia has been part of modern Russia since the latter half of the 16th century. Wikipedia
Laurentia
Large continental craton that forms the ancient geological core of North America. Now in the form of North America, although originally it also included the cratonic areas of Greenland and also the northwestern part of Scotland, known as the Hebridean Terrane. Wikipedia
Anabar Shield
Shield in Siberia. Exposed basement of the Siberian Craton. Wikipedia
São Francisco Craton
Ancient craton in the eastern part of South America. The craton crops out in the Brazilian states of Minas Gerais and Bahia. Wikipedia
Geology of Russia
The geology of Russia, the world's largest country, which extends over much of northern Eurasia, consists of several stable cratons and sedimentary platforms bounded by orogenic (mountain) belts. On the East European craton, at the heart of which is a complex of igneous and metamorphic rocks dating back to the Precambrian. Wikipedia
Anabar Plateau
Mountain plateau in Krasnoyarsk Krai and the Sakha Republic , Siberia, Russia. In a latitude dominated by permafrost. Wikipedia

Sentences

The Central Siberian Plateau is an ancient craton (sometimes named Angaraland) that formed an independent continent before the Permian (see the Siberian continent).Siberia-Wikipedia
The world at the time was dominated by two continents known as Pangaea and Siberia, surrounded by a global ocean called Panthalassa.Permian-Wikipedia
Gondwana was not considered a supercontinent by the earliest definition, since the landmasses of Baltica, Laurentia, and Siberia were separated from it.Gondwana-Wikipedia
Other minor oceans were the Paleo-Tethys Ocean, Proto-Tethys Ocean, Rheic Ocean, and Ural Ocean (which was closed during the collision with Siberia and Baltica).Devonian-Wikipedia
At the end of the Proterozoic, the supercontinent Pannotia had broken apart into the smaller continents Laurentia, Baltica, Siberia and Gondwana.History of Earth-Wikipedia
These events caused Proto-Tethys Ocean, a precursor of Paleo-Tethys, to shrink, until the Late Carboniferous, when the Chinese blocks collided with Siberia.Paleo-Tethys Ocean-Wikipedia

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