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  2. See it: Rare 'hair ice' photographed in Washington state - AOL

    www.aol.com/see-rare-hair-ice-photographed...

    Hair ice only forms in very specific conditions, on the rotting wood, the Met Office said, and where it's slightly below 32 degrees Farenheit and the air is moist. The fungus that causes the hair ...

  3. Mysterious hair ice phenomenon explained - AOL

    www.aol.com/news/2015-07-25-mysterious-hair-ice...

    Hair ice looks like incredibly fine, billowing strands massed together. Lasting merely hours or only a few days before melting, its exact cause has been a mystery for nearly 100 years.

  4. Hair Loss: How Much is Normal? And When Should You See Your ...

    www.aol.com/hair-loss-much-normal-see-202600672.html

    Stress: Stress-induced hair loss is known as telogen effluvium, and it typically occurs a few months after a stressful event, like an illness, a breakup, or the loss of a loved one. With this, you ...

  5. Thwaites Glacier - Wikipedia

    en.wikipedia.org/wiki/Thwaites_Glacier

    In 2001, an analysis of radar interferometry data from the Earth Remote Sensing Satellites 1 and 2 by Eric Rignot revealed that the grounding line of Thwaites Glacier had retreated by 1.4 km (0.87 mi) between 1992 and 1996, while its strongly negative mass balance (annual loss of around 16 billion tonnes of ice, equivalent to 17 cubic ...

  6. Traction alopecia - Wikipedia

    en.wikipedia.org/wiki/Traction_alopecia

    Traction alopecia is a type of alopecia or hair loss caused by a chronic pulling force being applied to the hair. [1] It commonly results from a person frequently wearing their hair in a particularly tight ponytail, pigtails, or braids with increased likelihood when hair is chemically relaxed as this compromises the hair shaft's tensile strength resulting in hair breakage.

  7. Ice shelf - Wikipedia

    en.wikipedia.org/wiki/Ice_shelf

    The floating ice shelf is in the left foreground, and the grounding line is visible as an abrupt change in surface slope due to flexure caused by the buoyancy force where the ice reaches flotation. An ice shelf is a large platform of glacial ice floating on the ocean, fed by one or multiple tributary glaciers.