<?xml version="1.0"?>
<?xml-stylesheet type="text/xsl" href="https://ontobee.org/ontology/view/ENVO?iri=http://purl.obolibrary.org/obo/ENVO_01000734"?>
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     xml:base="http://www.w3.org/2002/07/owl"
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    <!-- 
    ///////////////////////////////////////////////////////////////////////////////////////
    //
    // Annotation properties
    //
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    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000115"/>
    


    <!-- 
    ///////////////////////////////////////////////////////////////////////////////////////
    //
    // Datatypes
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    <!-- 
    ///////////////////////////////////////////////////////////////////////////////////////
    //
    // Classes
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    <!-- http://purl.obolibrary.org/obo/ENVO_01000525 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01000525">
        <rdfs:label xml:lang="en">rock intrusion</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/ENVO_01000734 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01000734">
        <rdfs:label xml:lang="en">laccolith</rdfs:label>
        <rdfs:subClassOf rdf:resource="http://purl.obolibrary.org/obo/ENVO_01000525"/>
        <ns2:IAO_0000115>A sheet intrusion (or concordant pluton) that has been injected between two layers of sedimentary rock. The pressure of the magma is high enough that the overlying strata are forced upward, giving the laccolith a dome or mushroom-like form with a generally planar base.</ns2:IAO_0000115>
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<!-- Generated by the OWL API (version 3.2.4.1806) http://owlapi.sourceforge.net -->



