{ "items" : [
    { "id" : "_:b1216949"
      "properties" : {
        "http://www.w3.org/1999/02/22-rdf-syntax-ns#type" : [ "http://www.w3.org/2002/07/owl#Axiom" ] ,
        "http://www.geneontology.org/formats/oboInOwl#hasDbXref" : [ "Wikipedia:Volcanic_cone" ] ,
        "http://www.w3.org/2002/07/owl#annotatedProperty" : [ "http://purl.obolibrary.org/obo/IAO_0000115" ] ,
        "http://www.w3.org/2002/07/owl#annotatedSource" : [ "http://purl.obolibrary.org/obo/ENVO_00000399" ] ,
        "http://www.w3.org/2002/07/owl#annotatedTarget" : [ "A cone that is composed of particles of silt to sand size. Explosive eruptions from a vent where the magma is interacting with groundwater or the sea (as in an eruption off the coast) produce steam and are called phreatic. The interaction between the magma, expanding steam, and volcanic gases results in the ejection of mostly small particles called ash. Fallen ash has the consistency of flour. The unconsolidated ash forms an ash cone which becomes a tuff cone or tuff ring once the ash consolidates."] } } }
