{ "items" : [
    { "id" : "http://dbpedia.org/resource/Kula_(volcano)"
      "properties" : {
        "http://www.w3.org/2000/01/rdf-schema#comment" : [ "Kula is a volcanic field located in western Turkey. Kula field consists of a broad area of cinder cones and maars. It is the westernmost volcano of Turkey. The volcanic character of the area was recognized in antiquity, when it was named Katekaumene (the burned lands) from the appearance of the environment, which was mostly suited for viticulture. Volcanism began in the Miocene and over three stages continued in the Holocene." ] ,
        "http://xmlns.com/foaf/0.1/name" : [ "Kula" ] ,
        "http://xmlns.com/foaf/0.1/depiction" : [ "http://commons.wikimedia.org/wiki/Special:FilePath/The_scoria_cone_at_the_Kula_Volcano.JPG" ] ,
        "http://dbpedia.org/ontology/elevation" : [ 750 ] ,
        "http://dbpedia.org/ontology/locatedInArea" : [ "http://dbpedia.org/resource/Turkey",
          "http://dbpedia.org/resource/Manisa_Province" ] ,
        "http://dbpedia.org/ontology/otherName" : [ "Katekaumene" ] ,
        "http://dbpedia.org/ontology/thumbnail" : [ "http://commons.wikimedia.org/wiki/Special:FilePath/The_scoria_cone_at_the_Kula_Volcano.JPG?width=300" ] ,
        "http://dbpedia.org/ontology/type" : [ "http://dbpedia.org/resource/Cinder_cone",
          "http://dbpedia.org/resource/Volcanic_field"] } } }
