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  2. Blue ice (glacial) - Wikipedia

    en.wikipedia.org/wiki/Blue_ice_(glacial)

    A large piece of compressed ice, or a glacier, similarly appears blue. The blue color is sometimes wrongly attributed to Rayleigh scattering, which is responsible for the color of the sky. Rather, water ice is blue for the same reason that large quantities of liquid water are blue: it is a result of an overtone of an oxygen–hydrogen (O−H ...

  3. Congelation ice - Wikipedia

    en.wikipedia.org/wiki/Congelation_ice

    Snow ice is white due to the presence of air bubbles. Black ice grows downward from the bottom of the existing ice surface. The growth rate of the ice is proportional to the rate that heat is transferred from the water below the ice surface to the air above the ice surface. [4] The total ice thickness can be approximated from Stefan's equation.

  4. Perito Moreno Glacier - Wikipedia

    en.wikipedia.org/wiki/Perito_Moreno_Glacier

    Aerial view of the glacier, taken two weeks before the 2004 rupture. The Perito Moreno (Spanish: Glaciar Perito Moreno), Francisco Gormaz or Bismarck Glacier [1] is a glacier located in Los Glaciares National Park in southwest Santa Cruz Province, Argentina, and originated in the Magallanes Region in Chile, being also part of the Bernardo O'Higgins National Park.

  5. This video of ice shards stacking up on Lake Superior is ...

    www.aol.com/news/2016-02-22-this-video-of-ice...

    Image: YouTube. Mother nature, you've done it again.. A mesmerizing video of ice shattering on frozen Lake Superior in Minnesota is making the rounds on social media -- and it isn't exactly hard ...

  6. Blue iceberg - Wikipedia

    en.wikipedia.org/wiki/Blue_iceberg

    Blue iceberg observed by tourists along the coast of Alaska, 2010. A blue iceberg is visible after the ice from above the water melts, causing the smooth portion of ice from below the water to overturn. [1] [2] The rare blue ice is formed from the compression of pure snow, which then develops into glacial ice. [3] [4]

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  9. Glacial stream - Wikipedia

    en.wikipedia.org/wiki/Glacial_stream

    In the summer, glacial streams experience high stream flow because of ice melt. [8] The high flow is characterized by high turbidity and sediment transport, which reduces the biomass of the resident periphyton. [8] At the end of summer, ice melt is reduced and stream flow decreases, causing an increase in the periphyton population. [8]