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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. Pingo - Wikipedia

    en.wikipedia.org/wiki/Pingo

    Frost heaving – Upwards swelling of soil during freezing; Kettle (landform) – Depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters, some are known as pingo ponds especially in Norfolk, England. [22] Laccolith – Mass of igneous rock formed from magma

  4. Frost heave - Wikipedia

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

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  5. 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 ...

  6. Ice lens - Wikipedia

    en.wikipedia.org/wiki/Ice_lens

    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 ...

  7. 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.

  8. Thermokarst - Wikipedia

    en.wikipedia.org/wiki/Thermokarst

    Small domes that form on the surface due to frost heaving with the onset of winter are only temporary features. They collapse during the following summer thaw, leaving a small surface depression. They collapse during the following summer thaw, leaving a small surface depression.

  9. Category:Frost and rime - Wikipedia

    en.wikipedia.org/wiki/Category:Frost_and_rime

    Pages in category "Frost and rime" The following 10 pages are in this category, out of 10 total. ... Frost heaving; Frost point; H. Hair ice; I. Icing (aeronautics) R.