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- Frost_line abstract "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. For example, snow cover and asphalt insulate the ground and homes can heat the ground (see also heat island). The line varies by latitude, it is deeper closer to the poles. It ranges in the United States from about zero to six feet. Below that depth, the temperature varies, but is always above 0 °C (32 °F).Alternatively, in Arctic and Antarctic locations the freezing depth is so deep that it becomes year-round permafrost, and the term "thaw depth" is used instead. Finally, in tropical regions, frost line may refer to the vertical geographic elevation below which frost does not occur.Frost front refers to the varying position of the frost line during seasonal periods of freezing and thawing.".
- Frost_line wikiPageID "760027".
- Frost_line wikiPageLength "4088".
- Frost_line wikiPageOutDegree "27".
- Frost_line wikiPageRevisionID "658921950".
- Frost_line wikiPageWikiLink Antarctic.
- Frost_line wikiPageWikiLink Arctic.
- Frost_line wikiPageWikiLink Asphalt.
- Frost_line wikiPageWikiLink Building_code.
- Frost_line wikiPageWikiLink Canada.
- Frost_line wikiPageWikiLink Category:Foundations_(buildings_and_structures).
- Frost_line wikiPageWikiLink Category:Glaciology.
- Frost_line wikiPageWikiLink Category:Ground_freezing.
- Frost_line wikiPageWikiLink Category:Soil.
- Frost_line wikiPageWikiLink Climate.
- Frost_line wikiPageWikiLink Elevation.
- Frost_line wikiPageWikiLink Frost.
- Frost_line wikiPageWikiLink Frost_heaving.
- Frost_line wikiPageWikiLink Groundwater.
- Frost_line wikiPageWikiLink Heat_island.
- Frost_line wikiPageWikiLink Heat_transfer.
- Frost_line wikiPageWikiLink Minnesota.
- Frost_line wikiPageWikiLink Ontario.
- Frost_line wikiPageWikiLink Ottawa.
- Frost_line wikiPageWikiLink Permafrost.
- Frost_line wikiPageWikiLink Snow.
- Frost_line wikiPageWikiLink Snow_cover.
- Frost_line wikiPageWikiLink Snow_line.
- Frost_line wikiPageWikiLink Soil.
- Frost_line wikiPageWikiLink Thaw_depth.
- Frost_line wikiPageWikiLink Thermal_insulation.
- Frost_line wikiPageWikiLink USA.
- Frost_line wikiPageWikiLink United_States.
- Frost_line wikiPageWikiLink Urban_heat_island.
- Frost_line wikiPageWikiLink Windsor,_Ontario.
- Frost_line wikiPageWikiLinkText "Frost line".
- Frost_line wikiPageWikiLinkText "Frost".
- Frost_line wikiPageWikiLinkText "frost line".
- Frost_line wikiPageWikiLinkText "soil frost".
- Frost_line hasPhotoCollection Frost_line.
- Frost_line wikiPageUsesTemplate Template:Convert.
- Frost_line wikiPageUsesTemplate Template:Distinguish2.
- Frost_line wikiPageUsesTemplate Template:Glaciology-stub.
- Frost_line wikiPageUsesTemplate Template:Other_uses.
- Frost_line wikiPageUsesTemplate Template:Reflist.
- Frost_line subject Category:Foundations_(buildings_and_structures).
- Frost_line subject Category:Glaciology.
- Frost_line subject Category:Ground_freezing.
- Frost_line subject Category:Soil.
- Frost_line type Science.
- Frost_line type Subfield.
- Frost_line type Thing.
- Frost_line comment "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. For example, snow cover and asphalt insulate the ground and homes can heat the ground (see also heat island). The line varies by latitude, it is deeper closer to the poles.".
- Frost_line label "Frost line".
- Frost_line differentFrom Snow_line.
- Frost_line sameAs Frostgrenze.
- Frost_line sameAs Profondità_di_congelamento.
- Frost_line sameAs m.0391b2.
- Frost_line sameAs Q1470555.
- Frost_line sameAs Q1470555.
- Frost_line wasDerivedFrom Frost_line?oldid=658921950.
- Frost_line isPrimaryTopicOf Frost_line.