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    <!-- http://purl.obolibrary.org/obo/ENVO_00001998 -->

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        <rdfs:label>soil</rdfs:label>
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        <rdfs:label xml:lang="en">frost action process</rdfs:label>
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        <rdfs:label xml:lang="en">cryoturbation of soil</rdfs:label>
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        <dc:date rdf:datatype="http://www.w3.org/2001/XMLSchema#dateTime">2019-06-24T17:44:01Z</dc:date>
        <rdfs:comment>The processes that form irregular structures in earth materials characterized by folded, broken and dislocated beds, and lenses of unconsolidated deposits, including organic horizons and even bedrock.  These processes include deep frost penetration, frost action, frost heaving, thaw settlement and all differential movements, including expansion and contraction due to temperature changes and the growth and disappearance of ground ice bodies, whether perennial or seasonal.  Low temperatures alone are not enough to produce cryoturbation; the water-ice phase change is necessary.  Cryoturbation is an important process in the development of patterned ground.</rdfs:comment>
        <ns3:IAO_0000115>A frost action process during which soil is displaced.</ns3:IAO_0000115>
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