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  2. Antarctic microorganism - Wikipedia

    en.wikipedia.org/wiki/Antarctic_microorganism

    Antarctica is one of the most physically and chemically extreme terrestrial environments to be inhabited by lifeforms. [1] The largest plants are mosses, and the largest animals that do not leave the continent are a few species of insects. Microbiome on the High Antarctic Plateau

  3. Antarctica - Wikipedia

    en.wikipedia.org/wiki/Antarctica

    A speculative representation of Antarctica labelled as ' Terra Australis Incognita ' on Jan Janssonius's Zeekaart van het Zuidpoolgebied (1657), Het Scheepvaartmuseum The name given to the continent originates from the word antarctic, which comes from Middle French antartique or antarctique (' opposite to the Arctic ') and, in turn, the Latin antarcticus (' opposite to the north ').

  4. Antarctic realm - Wikipedia

    en.wikipedia.org/wiki/Antarctic_Realm

    Antarctica was also part of the ancient supercontinent of Gondwanaland, which gradually broke up by continental drift starting 110 million years ago. The separation of South America from Antarctica 30–35 million years ago allowed the Antarctic Circumpolar Current to form, which isolated Antarctica climatically and caused it to become much colder.

  5. Category:Biota of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Category:Biota_of_Antarctica

    Antarctica (inside the inner line) and the Subantarctic zone (between the two lines) as defined in the WGSRPD The main article for this category is Biota of Antarctica . This category is for articles about the native biota of Antarctica .

  6. Geography of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Antarctica

    Antarctica is the largest ice desert in the world. Some 98% of Antarctica is covered by the Antarctic ice sheet , the world's largest ice sheet and also its largest reservoir of fresh water . Averaging at least 1.6 km thick, the ice is so massive that it has depressed the continental bedrock in some areas more than 2.5 km below sea level ...

  7. Geology of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Antarctica

    The geology of Antarctica covers the geological development of the continent through the Archean, Proterozoic and Phanerozoic eons. The geological study of Antarctica has been greatly hindered by the fact that nearly all of the continent is continuously covered with a thick layer of ice.

  8. Geology of the Antarctic Peninsula - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Antarctic...

    Development of the Bransfield Rift, depicting trench rollback and upwelling of displaced mantle material. [ 2 ] The last and most recent stage in the evolution of the Antarctic Peninsula subduction zone is the opening of the Bransfield Rift , [ 2 ] [ 5 ] creating the Bransfield back-arc basin from the Oligocene to the present day. [ 2 ]

  9. East Antarctica - Wikipedia

    en.wikipedia.org/wiki/East_Antarctica

    Map of Antarctica with Eastern Antarctica seen to the right. Image of a variety of ice types off the coast of East Antarctica. East Antarctica, also called Greater Antarctica, constitutes the majority (two-thirds) of the Antarctic continent, lying primarily in the Eastern Hemisphere south of the Indian Ocean, and separated from West Antarctica by the Transantarctic Mountains.

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