{ "items" : [
    { "id" : "http://dbpedia.org/resource/Tao-Rusyr_Caldera"
      "properties" : {
        "http://www.w3.org/2000/01/rdf-schema#comment" : [ "Tao-Rusyr Caldera (Russian: Тао-Русыр) is a stratovolcano located at the southern end of Onekotan Island, Kuril Islands, Russia. It has 7.5 km wide caldera formed during a catastrophic eruption less than 10,000 years ago (reported ages range from 5550 to 9400 Before Present). The waters of Kal'tsevoe Lake fill the caldera, along with a large symmetrical andesitic cone, Krenitsyn Peak, that rises as an island within the lake." ] ,
        "http://xmlns.com/foaf/0.1/name" : [ "Tao-Rusyr Caldera" ] ,
        "http://xmlns.com/foaf/0.1/depiction" : [ "http://commons.wikimedia.org/wiki/Special:FilePath/OnekotanIslandNASA.jpg" ] ,
        "http://dbpedia.org/ontology/elevation" : [ 1325 ] ,
        "http://dbpedia.org/ontology/eruptionYear" : [ "1952Z" ] ,
        "http://dbpedia.org/ontology/locatedInArea" : [ "http://dbpedia.org/resource/Kuril_Islands",
          "http://dbpedia.org/resource/Russia",
          "http://dbpedia.org/resource/Onekotan" ] ,
        "http://dbpedia.org/ontology/thumbnail" : [ "http://commons.wikimedia.org/wiki/Special:FilePath/OnekotanIslandNASA.jpg?width=300" ] ,
        "http://dbpedia.org/ontology/type" : [ "http://dbpedia.org/resource/Caldera",
          "http://dbpedia.org/resource/Stratovolcano"] } } }
