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  2. Frost line - Wikipedia

    en.wikipedia.org/wiki/Frost_line

    The frost line—also known as frost depth or freezing depth—is most commonly the depth to which the groundwater in soil is expected to freeze. The frost depth depends on the climatic conditions of an area, the heat transfer properties of the soil and adjacent materials, and on nearby heat sources.

  3. Thaw depth - Wikipedia

    en.wikipedia.org/wiki/Thaw_depth

    The active layer thickness is the maximum thaw depth over a period of two years. The layer of soil over the thaw depth is called the active layer, while the soil below is called permafrost. The term frost front refers to the varying position of the thaw line during the periods of freezing/thawing.

  4. Active layer - Wikipedia

    en.wikipedia.org/wiki/Active_layer

    The middle zone is permanently frozen as "permafrost". And the bottom layer is where the geothermal temperature is above freezing. Note the importance of the vertical 0 °C line: It denotes the bottom of the active layer in the seasonally variable temperature zone and the bottom limit of permafrost as the temperature increases with depth.

  5. How to Protect Your Flowers From Frost So They Can ... - AOL

    www.aol.com/protect-flowers-frost-survive-cold...

    “Below 31 degrees is considered a freeze," she says. "Anything under 26 degrees is a hard freeze.” Keeping an eye on your USDA Hardiness Zone Map will help you stay prepared for falling ...

  6. Permafrost - Wikipedia

    en.wikipedia.org/wiki/Permafrost

    Permafrost temperature profile. Permafrost occupies the middle zone, with the active layer above it, while geothermal activity keeps the lowest layer above freezing. The vertical 0 °C or 32 °F line denotes the average annual temperature that is crucial for the upper and lower limit of the permafrost zone, while the red lines represent seasonal temperature changes and seasonal temperature ...

  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. Frost advisory, freeze warning issued for several Ohio counties

    www.aol.com/frost-advisory-freeze-warning-issued...

    The National Weather Service in Wilmington has issued a frost advisory and freeze warning for several Ohio counties from midnight until 9:00 a.m.

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