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About: Dunedin Volcano     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatExtinctVolcanoes, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: yago:WikicatVolcanoesOfNewZealandgeo:SpatialThingyago:WikicatShieldVolcanoesyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:Location100027167yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Shape100027807yago:Space113910384yago:Vent109470550yago:WikicatExtinctVolcanoes New Facet based on Instances of this Class

The Dunedin Volcano is an extensively eroded multi-vent shield volcano that was active between 16 and 10 million years ago. It originally extended from the modern city of Dunedin, New Zealand to Aramoana about 25 km away. Extensive erosion has occurred over the last 10 million years and Otago Harbour now fills the oldest parts of the volcano. The remnants of the volcano form the hills around Otago Harbour (including Mount Cargill, Flagstaff, Saddle Hill, Signal Hill, and Otago Peninsula). Volcanism began in a shallow marine environment. The volcano became larger with flows of basalt and minor trachyte creating the bulk of the volcano. The final phase of eruptions are preserved as phonolite domes around Mount Cargill.