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  2. Würm glaciation - Wikipedia

    en.wikipedia.org/wiki/Würm_glaciation

    The Würm glaciation, shown in ice core data from the Antarctica and Greenland Moraines and gravel beds formed in the Würm glaciation near Leutkirch, Westallgäu, Germany, Zeil castle can be seen on the left. The corresponding ice age in North and Central Europe is known as the Weichselian glaciation, after the German name for the Vistula river.

  3. Phases of ice - Wikipedia

    en.wikipedia.org/wiki/Phases_of_ice

    Phase space of ice I h with respect to other ice phases. Virtually all ice in the biosphere is ice I h (pronounced: ice one h, also known as ice-phase-one). Ice I h exhibits many peculiar properties that are relevant to the existence of life and regulation of global climate. [138] For instance, its density is lower than that of liquid water.

  4. Last Glacial Period - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Period

    A chronology of climatic events of importance for the Last Glacial Period, about the last 120,000 years The Last Glacial Period caused a much lower global sea level.. The Last Glacial Period (LGP), also known as the Last glacial cycle, occurred from the end of the Last Interglacial to the beginning of the Holocene, c. 115,000 – c. 11,700 years ago, and thus corresponds to most of the ...

  5. Greenhouse and icehouse Earth - Wikipedia

    en.wikipedia.org/wiki/Greenhouse_and_icehouse_Earth

    Throughout Earth's climate history (Paleoclimate) its climate has fluctuated between two primary states: greenhouse and icehouse Earth. [1] Both climate states last for millions of years and should not be confused with the much smaller glacial and interglacial periods, which occur as alternating phases within an icehouse period (known as an ice age) and tend to last less than one million years ...

  6. Weichselian glaciation - Wikipedia

    en.wikipedia.org/wiki/Weichselian_glaciation

    The Fennoscandian Ice Sheet of the Weichselian glaciation most likely grew out of a mountain glaciation of small ice fields and ice caps in the Scandinavian Mountains.The initial glaciation of the Scandinavian Mountains would have been enabled by moisture coming from the Atlantic Ocean and the mountains high altitude.

  7. Timeline of glaciation - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_glaciation

    A less severe cold period or ice age is shown during the Jurassic-Cretaceous (150 Ma). There have been five or six major ice ages in the history of Earth over the past 3 billion years. The Late Cenozoic Ice Age began 34 million years ago, its latest phase being the Quaternary glaciation, in progress since 2.58 million years ago.

  8. CityVille Castle Rescue Goals: Everything you need to know - AOL

    www.aol.com/2012/12/17/cityville-castle-rescue...

    CityVille's Winter event has expanded this week via the release of the Ice Castle and its four goals. These goals will see you expanding your city, repairing the Ice Castle itself, and even ...

  9. Eisriesenwelt - Wikipedia

    en.wikipedia.org/wiki/Eisriesenwelt

    The ice formations in the cave were formed by thawing snow which drained into the cave and froze during winter. [4] Since the entrance to the caves is open year-round, chilly winter winds blow into the cave and freeze the snow inside. In summer, a cold wind from inside the cave blows toward the entrance and prevents the formations from melting.