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  2. Geology of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Antarctica

    The frozen continent of Antarctica was the last continent humanity set foot on. The first documented landings made below the Antarctic Circle took place in 1820, when Admiral Fabian Gottlieb von Bellingshausen and the crew of the Vostok and Mirny, as part of the Russian Antarctic Expedition, made land at Peter I Island and Alexander Island.

  3. 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 ]

  4. Antarctic lakes - Wikipedia

    en.wikipedia.org/wiki/Antarctic_lakes

    Antarctica also has some relatively small regions that are clear of ice and snow, and there are some surface lakes in these regions. They called for on the ground seismic studies, or drilling, to determine a more reliable number. These lakes are buried beneath deep layers of glacial ice.

  5. Geography of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Antarctica

    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; subglacial lakes of liquid water also occur (e.g., Lake ...

  6. Antarctic Peninsula - Wikipedia

    en.wikipedia.org/wiki/Antarctic_Peninsula

    At this time, the Antarctic Peninsula formed as the bedrock islands underlying it were overridden and joined by an ice sheet in the early Pliocene about 5.3–3.6 Ma. During the Quaternary period, the size of the West Antarctic Ice Sheet has fluctuated in response to glacial–interglacial cycles. During glacial epochs, this ice sheet was ...

  7. Abiotic component - Wikipedia

    en.wikipedia.org/wiki/Abiotic_component

    Abiotic components include physical conditions and non-living resources that affect living organisms in terms of growth, maintenance, and reproduction. Resources are distinguished as substances or objects in the environment required by one organism and consumed or otherwise made unavailable for use by other organisms.

  8. Scientists identify new Antarctic ice sheet ‘tipping point ...

    www.aol.com/scientists-identify-antarctic-ice...

    The Antarctic ice sheet is melting in a new, worrying way that scientific models used to project future sea level rise have not taken into account, suggesting current projections could be ...

  9. Tundra - Wikipedia

    en.wikipedia.org/wiki/Tundra

    In contrast with the Arctic tundra, the Antarctic tundra lacks a large mammal fauna, mostly due to its physical isolation from the other continents. Sea mammals and sea birds, including seals and penguins, inhabit areas near the shore, and some small mammals, like rabbits and cats, have been introduced by humans to some of the subantarctic islands.