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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. Frost heave - Wikipedia

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

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4. Category:Frost and rime - Wikipedia

   en.wikipedia.org/wiki/Category:Frost_and_rime

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5. 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.

6. 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 ...

7. 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 ...

8. 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 ...

9. Talk:Frost heaving - Wikipedia

   en.wikipedia.org/wiki/Talk:Frost_heaving

   Frost heaving is within the scope of WikiProject Soil, which collaborates on Soil and related articles on Wikipedia. If you would like to participate, you can choose to edit this article, or visit the project page for more information.