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  2. Frost heaving - Wikipedia

    en.wikipedia.org/wiki/Frost_heaving

    The dominant cause of soil displacement in frost heaving is the development of ice lenses. During frost heave, one or more soil-free ice lenses grow, and their growth displaces the soil above them. These lenses grow by the continual addition of water from a groundwater source that is lower in the soil and below the freezing line in the soil.

  3. Ice dam (roof) - Wikipedia

    en.wikipedia.org/wiki/Ice_dam_(roof)

    Ice dam forming on slate roof. An ice dam is an ice build-up on the eaves of sloped roofs of heated buildings that results from melting snow under a snow pack reaching the eave and freezing there. Freezing at the eave impedes the drainage of meltwater, which adds to the ice dam and causes backup of the meltwater, which may cause water leakage ...

  4. Frost weathering - Wikipedia

    en.wikipedia.org/wiki/Frost_weathering

    The ice crystal growth weakens the rocks which, in time, break up. [3] It is caused by the expansion of ice when water freezes, putting considerable stress on the walls of containment. This is actually a very common process in all humid, temperate areas where there is exposed rock, especially porous rocks like sandstone .

  5. Scrub Hub: What are ice dams and how big of a problem are ...

    www.aol.com/scrub-hub-ice-dams-big-102956174.html

    For this edition of the Scrub Hub, we are looking at ice dams: What are they, what causes them, and what problems are they making worse?

  6. Icicle - Wikipedia

    en.wikipedia.org/wiki/Icicle

    The wall of this ice tube is about 0.1 mm (0.004 in) and the width 5 mm (0.2 in). As a result of this growth process, the interior of a growing icicle is liquid water. The growth of an icicle both in length and in width can be calculated and is a complicated function of air temperature, wind speed, and the water flux into the icicle. [ 3 ]

  7. Penultimate Glacial Period - Wikipedia

    en.wikipedia.org/wiki/Penultimate_Glacial_Period

    This eccentricity causes greater seasonal impacts than normal because it limits the amount of sunlight that reaches the earth's surface, lowering the temperature. [6] Due to this, northern insolation (the amount of sunlight that reaches the surface) is reduced, meaning that during summer, less heat is exposed to the snows of the winter, which ...

  8. Deglaciation - Wikipedia

    en.wikipedia.org/wiki/Deglaciation

    Mapped extent of the Laurentide Ice Sheet during deglaciation has been prepared by Dyke et al. [21] Cycles of deglaciation are driven by various factors, with the main driver being changes in incoming summer solar radiation, or insolation, in the Northern Hemisphere. But, as not all of the rises in insolation throughout time caused deglaciation ...

  9. Freezing rain - Wikipedia

    en.wikipedia.org/wiki/Freezing_rain

    The ice that forms on roadways makes vehicle travel dangerous. Unlike snow, wet ice provides almost no traction, and vehicles will slide even on gentle slopes. Because freezing rain does not hit the ground as an ice pellet (called "sleet") but still as a rain droplet, it conforms to the shape of the ground, or object such as a tree branch or car.