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    Ice lenses are bodies of ice formed when moisture, diffused within soil or rock, accumulates in a localized zone. The ice initially accumulates within small collocated pores or pre-existing crack, and, as long as the conditions remain favorable, continues to collect in the ice layer or ice lens, wedging the soil or rock apart.
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    Ice lenses are bodies of ice formed when moisture, diffused within soil or rock, accumulates in a localized zone. The ice initially accumulates within small collocated pores or pre-existing crack, and, as long as the conditions remain favorable, continues to collect in the ice layer or ice lens, wedging the soil or rock apart.
    en.wikipedia.org/wiki/Ice_lens
    An ice lens is a lens, made out of ice, which is meant to focus light onto one point. The idea is to focus sunlight onto dry bits of wood, straw, or paper and start a fire. Some lenses have sides that bulge outwards (convex sides) which bring light rays closer together and focus the light.
    www.pbs.org/weta/roughscience/series3/ice/icelen…
    ice lens a dominantly horizontal, lens-shaped body of ice of any dimension.
    nsidc.org/learn/cryosphere-glossary/ice-lens
    Ice lenses draw water from surrounding soil by capillary action, typically growing up to 1/4 inch to 2 inches in thickness and up to several feet across. Often frost lenses form in multiple layers, adding to the total soil movement in an upwards direction. Ice lenses form in porous silts and also in clays that can support capillary action.
    inspectapedia.com/Energy/Ice-Lensing-Foundatio…
    Ice lenses are a key component in the process of frost heave. They form in soil or rock when moisture present in these materials freezes. Ice lenses lead to frost heaving.
    buyersask.com/frost-heaving-and-ice-lenses-caus…
     
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    Ice lens - Wikipedia

    Ice lenses are bodies of ice formed when moisture, diffused within soil or rock, accumulates in a localized zone. The ice initially accumulates within small collocated pores or pre-existing crack, and, as long as the conditions remain favorable, continues to collect in the ice layer or ice lens, … See more

    Common frost heaving
    Frost heave is the process by which the freezing of water-saturated soil causes the deformation and upward thrust of the ground surface. This … See more

    Understanding the phenomena image
    Ice lens growth in rock image

    The formation of an ice sphere can happen when an object is about 0.5–1.0 ft above where the water reaches repeatedly. The … See more

    Overview image
    Ice sphere formation image

    The basic condition for ice segregation and frost heaving is existence of a region in soil or porous rock which is relatively permeable, is in a temperature range which allows the … See more

    Rocks routinely contain pores of varying size and shape, regardless of origin or location. Rock voids are essentially small cracks, and serve … See more

     
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  5. Ice Lensing, Frost Heaves vs. Frozen Soil Pressures

    WEBHere we explain the difference between the vertical lift of frost heaves and ice lensing (or frost lenses) and we include details of the construction of …

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    • The Physics of Frost Heave and Ice-Lens Growth

      WEBFeb 21, 2013 · The principle cause of frost heave is the formation of segregated iceice lenses—in freezing soil columns. Despite much experimental and theoretical work, there remain many questions about …

    • Experimental constraints on the kinetics of ice lens initiation and …

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    • Ice Lensing, Thermal Diffusion and Water Migration in …

      WEBAn analysis of the diffusion and ice nucleation processes suggests conditions under which ice lensing can be expected; in particular, it is shown that multiple ice lenses cannot form unless the soil thermal …

    • Frost heave | Journal of Glaciology | Cambridge Core

      WEBWith the intermolecular forces that ultimately produce macroscopic frost heave properly accounted for, a simple treatment of freezing in porous media can be used to delineate the parameter regimes in which: (1) a …

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