<?xml version="1.0"?>
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    <!-- http://purl.obolibrary.org/obo/ENVO_01000062 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01000062">
        <rdfs:label rdf:datatype="http://www.w3.org/2001/XMLSchema#string">marine benthic storm</rdfs:label>
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        <oboInOwl:creation_date rdf:datatype="http://www.w3.org/2001/XMLSchema#string">2010-03-16T12:16:11Z</oboInOwl:creation_date>
        <ns2:IAO_0000115 rdf:datatype="http://www.w3.org/2001/XMLSchema#string">Benthic storms are strong benthic (near bottom) currents transporting sediment, created by the input of energy (largely kinetic) to the seabed. In regions with high mesoscale eddy activity, benthic storms are frequent and can create isohaline and isothermal conditions extending as much as 1000m above the seafloor.</ns2:IAO_0000115>
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