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  2. Housewrap - Wikipedia

    en.wikipedia.org/wiki/Housewrap

    Housewrap (or house wrap), also known by the genericized trademark homewrap (or home wrap), generally denotes a modern synthetic material used to protect buildings. Housewrap functions as a weather-resistant barrier , preventing rain or other forms of moisture from getting into the wall assembly while allowing water vapor to pass to the exterior.

  3. If You Have Frost in Your Freezer, This Is What It Means - AOL

    www.aol.com/lifestyle/frost-freezer-means...

    The post If You Have Frost in Your Freezer, This Is What It Means appeared first on Reader's Digest. It can impact food quality, cause a nasty odor, and weaken your freezer’s efficiency. But ...

  4. Basement - Wikipedia

    en.wikipedia.org/wiki/Basement

    An underground crawl space (as the name implies) is a type of basement in which one cannot stand up—the height may be as little as one foot (30 cm), and the surface is often soil. Crawl spaces offer a convenient access to pipes, substructures and a variety of other areas that may be difficult or expensive to access otherwise.

  5. Hesco bastion - Wikipedia

    en.wikipedia.org/wiki/Hesco_bastion

    The Concertainer, [1] known colloquially as the Hesco barrier [2] or Hesco bastion, [3] with HESCO being the brand name of the manufacturer, is a modern gabion primarily used for flood control and military fortifications. [4]

  6. Auto-defrost - Wikipedia

    en.wikipedia.org/wiki/Auto-defrost

    Air circulation helps sublimate any ice or frost that may form on frozen items in the freezer compartment. While defrosting, this fan is stopped to prevent heated-up air from reaching the food compartment. Instead of the traditional cooling elements being embedded in the freezer liner, auto-defrost elements are behind or beneath the liner.

  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).

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