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    <!-- 
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    <!-- http://purl.obolibrary.org/obo/BFO_0000050 -->

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        <rdf:type rdf:resource="http://www.w3.org/2002/07/owl#TransitiveProperty"/>
        <rdfs:label xml:lang="en">part of</rdfs:label>
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    <!-- http://purl.obolibrary.org/obo/ENVO_00000015 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_00000015">
        <rdfs:label>ocean</rdfs:label>
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    <!-- http://purl.obolibrary.org/obo/ENVO_00000406 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_00000406">
        <rdfs:label>mid-ocean ridge</rdfs:label>
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        <ns4:IAO_0000115>An underwater mountain range, formed by plate tectonics. This uplifting of the ocean floor occurs when convection currents rise in the mantle beneath the oceanic crust and create magma where two tectonic plates meet at a divergent boundary. The mid-ocean ridges of the world are connected and form a single global mid-oceanic ridge system that is part of every ocean.</ns4:IAO_0000115>
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    <!-- http://purl.obolibrary.org/obo/ENVO_00000550 -->

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