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  2. The Thaw (2009 film) - Wikipedia

    en.wikipedia.org/wiki/The_Thaw_(2009_film)

    The film begins with a video documentary by Dr. David Kruipen , a research scientist on Banks Island, in the Canadian Arctic and the outbreak of a pandemic, with 400 dead and 10,000 infected. This is followed by a flashback to when David, his assistant Jane ( Anne Marie DeLuise ) and two other researchers tranquilize a polar bear , then ...

  3. Regelation - Wikipedia

    en.wikipedia.org/wiki/Regelation

    Regelation is the phenomenon of ice melting under pressure and refreezing when the pressure is reduced. This can be demonstrated by looping a fine wire around a block of ice, with a heavy weight attached to it. The pressure exerted on the ice slowly melts it locally, permitting the wire to pass through the entire block.

  4. Snow science - Wikipedia

    en.wikipedia.org/wiki/Snow_science

    Melt Forms (MF) – Range from clustered round grains of wet snow through melt-freeze rounded polycrystals when water in veins freezes to loosely bonded, fully rounded single crystals and polycrystals.to polycrystals from a surface layer of wet snow that refroze after having been wetted by melt or rainfall. Ice Formations (IF) – Encompass the ...

  5. Glaciology - Wikipedia

    en.wikipedia.org/wiki/Glaciology

    ' study of ice ') is the scientific study of glaciers, or, more generally, ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics , geology , physical geography , geomorphology , climatology , meteorology , hydrology , biology , and ecology .

  6. Art in nature: Late-winter melting, refreezing cooks up ice ...

    www.aol.com/news/art-nature-winter-melting...

    The cycle of ice melting and refreezing along a river's bank can create beautiful natural sculptures. Art in nature: Late-winter melting, refreezing cooks up ice pancakes, marbles and more Skip to ...

  7. Plucking (glaciation) - Wikipedia

    en.wikipedia.org/wiki/Plucking_(glaciation)

    As a glacier moves down a valley, friction causes the basal ice of the glacier to melt and infiltrate joints (cracks) in the bedrock. The freezing and thawing action of the ice enlarges, widens, or causes further cracks in the bedrock as it changes volume across the ice/water phase transition (a form of hydraulic wedging), gradually loosening ...

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