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  2. Frost damage (construction) - Wikipedia

    en.wikipedia.org/wiki/Frost_damage_(construction)

    Visible frost damage develops after an accumulation of micro-cracks as a result of several freeze-thaw cycles. [ 1 ] [ 2 ] Frost damage can be prevented by the use of frost-proof materials, i.e. , a material which has sufficient closed pores, by which the volume increase caused by the freezing of water in capillary pores can be absorbed by the ...

  3. Frost damage - Wikipedia

    en.wikipedia.org/wiki/Frost_damage

    Frost damage may refer to: Frost damage (construction) , damage to constructions caused by the freezing of the moisture in the materials. Frost damage (biology) , which is damage to plants and fruits caused by frost.

  4. Schoharie Creek Bridge collapse - Wikipedia

    en.wikipedia.org/wiki/Schoharie_Creek_Bridge...

    In the spring and summer of 1955, the pier plinths began to show vertical cracks ranging from 0.12 to 0.20 in (3 to 5 mm), as a result of high tensile stresses in the concrete plinth. Almost a year later, on October 16, 1955, the bridge was damaged by a flood. In 1957, plinth reinforcement was added to each of the four piers.

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  6. Here Are the Best Ways to Protect Your Plants from Frost - AOL

    www.aol.com/best-ways-protect-plants-frost...

    Plants that are most susceptible to frost damage include tender annuals such as tomatoes, peppers, and basil. Delicate perennials , young seedlings, and tropical plants like hibiscus and citrus ...

  7. 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).

  8. Cryoseism - Wikipedia

    en.wikipedia.org/wiki/Cryoseism

    Most frost quakes are associated with minor snow cover on the ground without a significant amount of snow to insulate the ground (i.e., less than 6 inches (15 cm)) A rapid temperature drop from approximately freezing to near or below −18 °C (0 °F), which ordinarily occurred on a timescale of 16 to 48 hours. [1]

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