About: Dunedin Volcano

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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.

Attributes	Values
rdf:type	yago:WikicatVolcanoesOfNewZealand geo:SpatialThing yago:WikicatShieldVolcanoes yago:Abstraction100002137 yago:AmorphousShape113867492 yago:Attribute100024264 yago:Crack109258715 yago:Location100027167 yago:Object100002684 yago:Opening109379111 yago:PhysicalEntity100001930 yago:YagoGeoEntity yago:YagoLegalActorGeo yago:YagoPermanentlyLocatedEntity yago:Shape100027807 yago:Space113910384 yago:Vent109470550 yago:WikicatExtinctVolcanoes
rdfs:label	Dunedin Volcano (en)
rdfs:comment	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. (en)
name	Dunedin Volcano (en)
geo:lat	-45.848000 (xsd:float)
geo:long	170.636002 (xsd:float)
foaf:depiction
dct:subject	Geography of Dunedin Landforms of Otago Extinct volcanoes Miocene shield volcanoes Polygenetic shield volcanoes Shield volcanoes of New Zealand
Wikipage page ID	35365265 (xsd:integer)
Wikipage revision ID	1094302785 (xsd:integer)
Link from a Wikipage to another Wikipage	Basalt Geography of Dunedin Landforms of Otago Saddle Hill (New Zealand) Mount Cargill Aramoana Signal Hill (New Zealand) Banks Peninsula Volcano Extinct volcanoes Miocene shield volcanoes Polygenetic shield volcanoes Dunedin Dunedin Botanic Garden Flagstaff (Otago) Shield volcanoes of New Zealand Breccia Otago Harbour Otago Peninsula Blackhead (New Zealand) Trachyte St Clair, New Zealand New Zealand Second Beach (New Zealand) Shield volcano Phonolite
Link from a Wikipage to an external page	https://www.youtube.com/watch%3Fv=6n5wNAShgvI
sameAs	Dunedin Volcano Dunedin Volcano Dunedin Volcano Dunedin Volcano
dbp:wikiPageUsesTemplate	dbt:Infobox_rockunit dbt:Otago-geo-stub dbt:Coord dbt:Reflist dbt:Use_dmy_dates dbt:Volcano-stub
thumbnail	wiki-commons:Special:FilePath/Organ_pipes_columnar_joints_Dunedin.jpg?width=300
age	16 (xsd:integer)
country	New Zealand (en)
period	Miocene (en)
region	Otago (en)
type	Igneous (en)
georss:point	-45.848 170.636
has abstract	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. Traces of the old Dunedin Volcano are best seen in the Dunedin Botanic Garden's geology walk, the cliffs at Aramoana and the geomorphology of Mount Cargill which has preserved lava domes. Basaltic columns are also to be found as prominent features above Second Beach at St Clair and at Blackhead. This 'Dunedin Volcano Animation' shows various locations around Dunedin with information on age of the rocks and general evolution of the Dunedin Volcano and more distant volcanism. . (en)
namedfor	Dunedin
overlies	Waipuna Bay Formation (en)
prilithology	Basalt, trachyte, phonolite and breccia (en)
prov:wasDerivedFrom	wikipedia-en:Dunedin_Volcano?oldid=1094302785&ns=0
page length (characters) of wiki page	4144 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Dunedin_Volcano
geo:geometry	POINT(170.63600158691 -45.847999572754)
is Link from a Wikipage to another Wikipage of	Quarantine Island (New Zealand) Volcanism of New Zealand List of mountains of New Zealand by height List of shield volcanoes Geology of New Zealand Mount Cargill Stratigraphy of New Zealand Banks Peninsula Volcano Lawyers Head Dunedin Botanic Garden Flagstaff (Otago) Otago Harbour Otago Peninsula

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