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Statements

Subject Item
dbr:Thaw_Hill
rdf:type
owl:Thing yago:YagoLegalActorGeo yago:Shape100027807 yago:YagoPermanentlyLocatedEntity yago:YagoGeoEntity yago:Space113910384 yago:Object100002684 dbo:Location schema:Place yago:Vent109470550 dbo:Mountain yago:Location100027167 yago:WikicatPleistoceneVolcanoes yago:PhysicalEntity100001930 yago:Opening109379111 dbo:Place yago:Abstraction100002137 yago:AmorphousShape113867492 yago:Crack109258715 yago:Attribute100024264
rdfs:label
Thaw Hill
rdfs:comment
Thaw Hill is a cinder cone in northwestern British Columbia, Canada. It is one of the volcanoes in the central portion of the Mount Edziza volcanic complex and last erupted during the Pleistocene period.
dcterms:subject
dbc:Pleistocene_volcanoes dbc:Northern_Cordilleran_Volcanic_Province
dbo:wikiPageID
23422688
dbo:wikiPageRevisionID
905445221
dbo:wikiPageWikiLink
dbr:Pleistocene dbr:Volcanology_of_Canada dbr:Canada dbr:Mount_Edziza_volcanic_complex dbc:Pleistocene_volcanoes dbr:List_of_Northern_Cordilleran_volcanoes dbc:Northern_Cordilleran_Volcanic_Province dbr:Cinder_cone dbr:British_Columbia dbr:List_of_volcanoes_in_Canada dbr:Volcanology_of_Western_Canada
owl:sameAs
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dbo:abstract
Thaw Hill is a cinder cone in northwestern British Columbia, Canada. It is one of the volcanoes in the central portion of the Mount Edziza volcanic complex and last erupted during the Pleistocene period.
gold:hypernym
dbr:Cone
prov:wasDerivedFrom
wikipedia-en:Thaw_Hill?oldid=905445221&ns=0
dbo:wikiPageLength
873
dbo:country
dbr:Canada
dbo:locatedInArea
dbr:British_Columbia_Interior
dbo:province
dbr:British_Columbia
foaf:isPrimaryTopicOf
wikipedia-en:Thaw_Hill