{ "items" : [
    { "id" : "http://dbpedia.org/resource/Opal_Cone"
      "properties" : {
        "http://www.w3.org/2000/01/rdf-schema#comment" : [ "Opal Cone is a cinder cone located on the southeast flank of Mount Garibaldi in the Coast Mountains of British Columbia, Canada. It is the source of a 15 km long broad dacite lava flow with prominent wrinkled ridges. The lava flow is unusually long for a silicic lava flow. Opal Cone is a member of the Cascade Volcanoes, but it is located in the Garibaldi Ranges in the Coast Mountains and not in the Cascade Range proper." ] ,
        "http://xmlns.com/foaf/0.1/name" : [ "Opal Cone" ] ,
        "http://xmlns.com/foaf/0.1/depiction" : [ "http://commons.wikimedia.org/wiki/Special:FilePath/Elfin_Lakes%2C_Opal_Cone.jpg" ] ,
        "http://dbpedia.org/ontology/elevation" : [ 1736 ] ,
        "http://dbpedia.org/ontology/eruptionYear" : [ "9300Z" ] ,
        "http://dbpedia.org/ontology/locatedInArea" : [ "http://dbpedia.org/resource/Canada",
          "http://dbpedia.org/resource/British_Columbia",
          "http://dbpedia.org/resource/Garibaldi_Provincial_Park" ] ,
        "http://dbpedia.org/ontology/mountainRange" : [ "http://dbpedia.org/resource/Garibaldi_Ranges" ] ,
        "http://dbpedia.org/ontology/nationalTopographicSystemMapNumber" : [ "NTS92.G/15" ] ,
        "http://dbpedia.org/ontology/prominence" : [ 86 ] ,
        "http://dbpedia.org/ontology/thumbnail" : [ "http://commons.wikimedia.org/wiki/Special:FilePath/Elfin_Lakes%2C_Opal_Cone.jpg?width=300" ] ,
        "http://dbpedia.org/ontology/type" : [ "http://dbpedia.org/resource/Cinder_cone"] } } }
