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    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000115"/>
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    <!-- http://purl.obolibrary.org/obo/ENVO_00000461 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_00000461">
        <rdfs:label>pseudocrater</rdfs:label>
        <rdfs:subClassOf rdf:resource="http://purl.obolibrary.org/obo/ENVO_00000514"/>
        <oboInOwl:hasDbXref>https://en.wikipedia.org/wiki/Pseudocrater</oboInOwl:hasDbXref>
        <oboInOwl:hasExactSynonym>rootless vent</oboInOwl:hasExactSynonym>
        <ns3:IAO_0000115>A volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted. A pseudocrater is characterised by the absence of any magma conduit which connects below the surface of the earth. Pseudocraters are formed by steam explosions as flowing hot lava crosses over a wet surface, such as a swamp, a lake, or a pond. The explosive gases break through the lava surface in a manner similar to a phreatic eruption, and the tephra builds up crater-like forms which can appear very similar to real volcanic craters.</ns3:IAO_0000115>
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    <!-- http://purl.obolibrary.org/obo/ENVO_00000514 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_00000514">
        <rdfs:label>crater</rdfs:label>
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