Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q5039522> ?p ?o }
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- Q5039522 subject Q7778060.
- Q5039522 subject Q8178858.
- Q5039522 subject Q8345927.
- Q5039522 subject Q8639117.
- Q5039522 subject Q8683750.
- Q5039522 subject Q8818133.
- Q5039522 subject Q8823362.
- Q5039522 subject Q8904137.
- Q5039522 abstract "Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation (25 to 10 ka). Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to hyaloclastite deposits from the base upward. Locally the sections are capped by subaerial basaltic lava flows. Samples of the glassy pillow basalts and hyaloclastites along with crystalline basalt flows were collected at Caribou Tuya. The volcano is believed to have formed and last erupted during the Pleistocene Epoch.".
- Q5039522 country Q16.
- Q5039522 elevation "1770.0".
- Q5039522 locatedInArea Q16.
- Q5039522 locatedInArea Q1974.
- Q5039522 locatedInArea Q3153780.
- Q5039522 mountainRange Q14874778.
- Q5039522 province Q1974.
- Q5039522 type Q943137.
- Q5039522 wikiPageWikiLink Q1136513.
- Q5039522 wikiPageWikiLink Q14874778.
- Q5039522 wikiPageWikiLink Q16.
- Q5039522 wikiPageWikiLink Q17118379.
- Q5039522 wikiPageWikiLink Q1974.
- Q5039522 wikiPageWikiLink Q2458815.
- Q5039522 wikiPageWikiLink Q25546.
- Q5039522 wikiPageWikiLink Q40157.
- Q5039522 wikiPageWikiLink Q43338.
- Q5039522 wikiPageWikiLink Q4804418.
- Q5039522 wikiPageWikiLink Q502339.
- Q5039522 wikiPageWikiLink Q577.
- Q5039522 wikiPageWikiLink Q6592495.
- Q5039522 wikiPageWikiLink Q7058262.
- Q5039522 wikiPageWikiLink Q7568681.
- Q5039522 wikiPageWikiLink Q7778060.
- Q5039522 wikiPageWikiLink Q7940035.
- Q5039522 wikiPageWikiLink Q7940088.
- Q5039522 wikiPageWikiLink Q8178858.
- Q5039522 wikiPageWikiLink Q8345927.
- Q5039522 wikiPageWikiLink Q8639117.
- Q5039522 wikiPageWikiLink Q8683750.
- Q5039522 wikiPageWikiLink Q8818133.
- Q5039522 wikiPageWikiLink Q8823362.
- Q5039522 wikiPageWikiLink Q8904137.
- Q5039522 wikiPageWikiLink Q943137.
- Q5039522 wikiPageWikiLink Q964204.
- Q5039522 elevationM "1770".
- Q5039522 location Q16.
- Q5039522 location Q1974.
- Q5039522 name "Caribou Tuya".
- Q5039522 range Q14874778.
- Q5039522 type Q943137.
- Q5039522 point "59.23638888888889 -130.5625".
- Q5039522 type Mountain.
- Q5039522 type Place.
- Q5039522 type Location.
- Q5039522 type Mountain.
- Q5039522 type NaturalPlace.
- Q5039522 type Place.
- Q5039522 type Thing.
- Q5039522 type SpatialThing.
- Q5039522 type Q8502.
- Q5039522 comment "Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation (25 to 10 ka). Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to hyaloclastite deposits from the base upward. Locally the sections are capped by subaerial basaltic lava flows.".
- Q5039522 label "Caribou Tuya".
- Q5039522 lat "59.23638888888889".
- Q5039522 long "-130.5625".
- Q5039522 name "Caribou Tuya".