<?xml version="1.0"?>
<?xml-stylesheet type="text/xsl" href="https://ontobee.org/ontology/view/MICRO?iri=http://purl.obolibrary.org/obo/ENVO_00000134"?>
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    <!-- 
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    <!-- http://purl.obolibrary.org/obo/ENVO_00000134 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_00000134">
        <rdfs:label rdf:datatype="http://www.w3.org/2001/XMLSchema#string">permafrost</rdfs:label>
        <rdfs:subClassOf rdf:resource="http://purl.obolibrary.org/obo/ENVO_00001998"/>
        <oboInOwl:hasOBONamespace rdf:datatype="http://www.w3.org/2001/XMLSchema#string">ENVO</oboInOwl:hasOBONamespace>
        <oboInOwl:id rdf:datatype="http://www.w3.org/2001/XMLSchema#string">ENVO:00000134</oboInOwl:id>
        <oboInOwl:hasDbXref rdf:datatype="http://www.w3.org/2001/XMLSchema#string">EcoLexicon:permafrost</oboInOwl:hasDbXref>
        <oboInOwl:hasDbXref rdf:datatype="http://www.w3.org/2001/XMLSchema#string">LTER:408</oboInOwl:hasDbXref>
        <oboInOwl:hasExactSynonym rdf:datatype="http://www.w3.org/2001/XMLSchema#string">Permafrost</oboInOwl:hasExactSynonym>
        <ns2:IAO_0000115 rdf:datatype="http://www.w3.org/2001/XMLSchema#string">Soil at or below the freezing point of water (0C or 32F) for two or more years. Ice is not always present, as may be in the case of nonporous bedrock, but it frequently occurs and it may be in amounts exceeding the potential hydraulic saturation of the ground material.</ns2:IAO_0000115>
        <oboInOwl:hasDbXref rdf:datatype="http://www.w3.org/2001/XMLSchema#string">Wikipedia:Permafrost</oboInOwl:hasDbXref>
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    <!-- http://purl.obolibrary.org/obo/ENVO_00001998 -->

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<!-- Generated by the OWL API (version 3.2.4.1806) http://owlapi.sourceforge.net -->



