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  2. Frost heaving - Wikipedia

    en.wikipedia.org/wiki/Frost_heaving

    Photograph taken 21 March 2010 in Norwich, Vermont. Frost heaving (or a frost heave) is an upwards swelling of soil during freezing conditions caused by an increasing presence of ice as it grows towards the surface, upwards from the depth in the soil where freezing temperatures have penetrated into the soil (the freezing front or freezing boundary).

  3. Ice jacking - Wikipedia

    en.wikipedia.org/wiki/Ice_jacking

    Ice jacking is a continuous process that occurs during the winter in areas near lakes. The process starts when the ice begins to crack. When water then fills in those gaps, the process repeats and continues until there is a wall of ice surrounding the lake's shoreline, sometimes reaching up to three feet.

  4. Periglaciation - Wikipedia

    en.wikipedia.org/wiki/Periglaciation

    A process called frost heaving is responsible for these features. Solifluction lobes – Solifluction lobes are formed when waterlogged soil slips down a slope due to gravity, forming U-shaped lobes. Blockfields or Felsenmeer – Blockfields are areas covered by large angular blocks, traditionally believed to have been created by freeze-thaw ...

  5. Ice segregation - Wikipedia

    en.wikipedia.org/wiki/Ice_segregation

    Ice lens formation resulting in frost heave in cold climates. Frost heave is the process by which the freezing of water-saturated soil causes the deformation and upward thrust of the ground surface. [3] This process can distort and crack pavement, damage the foundations of buildings and displace soil in regular patterns. Moist, fine-grained ...

  6. Palsa - Wikipedia

    en.wikipedia.org/wiki/Palsa

    The overlying soil layer is gradually lifted up by frost heaving. [7] In cross-section, the ice cores of a palsa show layering, which is caused by the successive winter freezing intervals. The pressing out of water from the pores is not crucial, however, since the boggy soil is water-saturated and thus always provides enough water for ice core ...

  7. Nivation - Wikipedia

    en.wikipedia.org/wiki/Nivation

    Nivation is the set of geomorphic processes associated with snow patches.The primary processes are mass wasting and the freeze and thaw cycle, [1] in which fallen snow gets compacted into firn or névé.

  8. Pothole - Wikipedia

    en.wikipedia.org/wiki/Pothole

    Frost heaving can damage pavement. 3. Thawing can weaken soil structure. 4. Traffic can break the pavement. According to the US Army Corps of Engineers's Cold Regions Research and Engineering Laboratory, pothole formation requires two factors to be present at the same time: water and traffic. Water weakens the soil beneath the pavement while ...

  9. Frost heave - Wikipedia

    en.wikipedia.org/?title=Frost_heave&redirect=no

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