@prefix foaf:	<http://xmlns.com/foaf/0.1/> .
@prefix wikipedia-en:	<http://en.wikipedia.org/wiki/> .
@prefix dbr:	<http://dbpedia.org/resource/> .
wikipedia-en:Campanario_Formation	foaf:primaryTopic	dbr:Campanario_Formation .
@prefix dbo:	<http://dbpedia.org/ontology/> .
dbr:Campanario	dbo:wikiPageWikiLink	dbr:Campanario_Formation ;
	dbo:wikiPageDisambiguates	dbr:Campanario_Formation .
<http://dbpedia.org/resource/Laguna_del_Maule_(volcano)>	dbo:wikiPageWikiLink	dbr:Campanario_Formation .
dbr:Trapa-Trapa_Formation	dbo:wikiPageWikiLink	dbr:Campanario_Formation .
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dbr:Trapa-Trapa_Formation	dbp:underlies	dbr:Campanario_Formation .
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@prefix geo:	<http://www.w3.org/2003/01/geo/wgs84_pos#> .
dbr:Campanario_Formation	rdf:type	geo:SpatialThing .
@prefix rdfs:	<http://www.w3.org/2000/01/rdf-schema#> .
dbr:Campanario_Formation	rdfs:label	"Campanario Formation"@en ;
	rdfs:comment	"Campanario Formation (Spanish: Formaci\u00F3n Campanario) is a Miocene geological formation in the high Andes of Central Chile and northern Neuqu\u00E9n Province in Argentina. The formation crops out around the upper parts of the basins of Maule and \u00D1uble rivers."@en .
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dbr:Campanario_Formation	geo:lat	"-36.0"^^xsd:float ;
	geo:long	"-71.599998"^^xsd:float .
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dbr:Campanario_Formation	dcterms:subject	dbc:Tuff_formations ,
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		dbc:Neogene_Chile ,
		dbc:Miocene_Series_of_South_America ,
		dbc:Geologic_formations_of_Argentina ,
		dbc:Neogene_Argentina ,
		<http://dbpedia.org/resource/Category:Geology_of_Biob\u00EDo_Region> ,
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		<http://dbpedia.org/resource/Category:Geology_of_Neuqu\u00E9n_Province> ,
		dbc:Pliocene_Series_of_South_America ;
	dbo:abstract	"Campanario Formation (Spanish: Formaci\u00F3n Campanario) is a Miocene geological formation in the high Andes of Central Chile and northern Neuqu\u00E9n Province in Argentina. The formation crops out around the upper parts of the basins of Maule and \u00D1uble rivers."@en ;
	dbo:wikiPageWikiLink	dbr:Maule_River ,
		<http://dbpedia.org/resource/Category:Geology_of_Neuqu\u00E9n_Province> ,
		dbr:Maule_Region ,
		dbr:Tuff ,
		<http://dbpedia.org/resource/Category:Geology_of_Biob\u00EDo_Region> ,
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		dbr:Itata_River ,
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		dbr:Miocene ,
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		dbr:Lava ,
		dbr:Andesite ,
		dbc:Neogene_Argentina ,
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		dbc:Pliocene_Series_of_South_America .
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	dbo:wikiPageRevisionID	1080830656 ;
	dbp:country	"Chile, Argentina"@en ;
	dbo:wikiPageLength	"2274"^^xsd:nonNegativeInteger ;
	dbo:wikiPageID	53128162 ;
	dbp:name	"Campanario Formation"@en .
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dbr:Campanario_Formation	owl:sameAs	dbr:Campanario_Formation .
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dbr:Campanario_Formation	owl:sameAs	yago-res:Campanario_Formation ,
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dbr:Campanario_Formation	owl:sameAs	wikidata:Q30591162 .
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dbr:Campanario_Formation	georss:point	"-36.0 -71.6" .
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dbr:Campanario_Formation	prov:wasDerivedFrom	<http://en.wikipedia.org/wiki/Campanario_Formation?oldid=1080830656&ns=0> ;
	dbp:type	dbr:Geological_formation ;
	foaf:isPrimaryTopicOf	wikipedia-en:Campanario_Formation .
@prefix ogcgs:	<http://www.opengis.net/ont/geosparql#> .
dbr:Campanario_Formation	geo:geometry	"POINT(-71.599998474121 -36)"^^ogcgs:wktLiteral ;
	dbp:prilithology	"Tuff, breccia, welded tuff, andesite lava, dacite lava"@en ;
	dbp:namedby	"Robert E. Drake"@en ;
	dbp:yearTs	1974 ;
	dbp:period	"Pliocene"@en ;
	dbp:age	dbr:Miocene ,
		dbr:Pliocene ;
	dbp:region	<http://dbpedia.org/resource/Neuqu\u00E9n_Province> ,
		"Maule & B\u00EDo B\u00EDo Regions"@en .  <script>parent.window.postMessage('ixistenz.url:http://dbpedia.org/data/Campanario_Formation.ttl', '*'); </script> <div id='browserdiffcontainer' style='position: fixed; right: 10px; top: 10vh; min-width: 60px;  border: 1px solid white; background: rgb(251, 189, 0);; opacity: 0.9; font-family: helvetica, arial, sans serif;  font-size: 12px; z-index: 20001; padding-bottom: 20px;'><div onclick="toggle('browserdiffcontainerlist'); return false;" style='background: rgb(151, 89, 0);; color: white; '><strong>&nbsp; <span class='glyphicon glyphicon-minus'></span> NODES</strong></div><div id='browserdiffcontainerlist' style='padding-left: 10px; padding-right: 5px; max-height: 50vh; overflow: auto; '></div></div>
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