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Statements

Subject Item

dbr:Geology_of_Taranaki

rdfs:label

Geology of Taranaki

rdfs:comment

The Taranaki Region of New Zealand is built upon the Median Batholith in the West, and Greywacke Rocks in the East. However, no rocks older than Miocene times are visible at the surface. The dominant feature of the Taranaki Region is the andesitic stratovolcano of Mount Taranaki, which is only about 130,000 years old. The dissected hill country to the East of the , and West of the Central Volcanic Plateau (Ruapehu and Tongariro) is composed of soft Miocene to Pleistocene sandstone and mudstone. The coastal lowlands around Wanganui to the South have well-developed Quaternary marine terraces, and coastal sand dunes.

foaf:depiction

n8:Mt_Taranaki.jpg

dcterms:subject

dbc:Taranaki dbc:Geology_of_New_Zealand_by_region

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959095685

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dbr:Maui_gas_field dbr:New_Zealand dbr:Miocene dbr:Taranaki_Peninsula dbr:Greywacke dbr:Geophysical_survey dbr:Tongariro dbr:Manaia,_Taranaki dbr:Paritutu dbr:Eocene dbr:Oil_and_gas_industry_in_New_Zealand dbr:Lahar dbr:Pohokura_field dbr:Limestone dbr:Whanganui_River dbr:Whangaehu_River dbc:Taranaki dbr:Mount_Ruapehu dbr:Taranaki_Region dbr:Marine_terrace dbr:Sandstone dbr:Mudstone dbr:Sugar_Loaf_Islands dbr:Geology_of_New_Zealand dbr:Torlesse_Composite_Terrane dbr:Wanganui dbr:Mount_Tongariro n16:Mt_Taranaki.JPG dbr:Kapuni dbr:Dun_Mountain-Maitai_Terrane dbr:Ophiolite dbr:Pleistocene dbc:Geology_of_New_Zealand_by_region dbr:Mount_Taranaki dbr:Oligocene dbr:New_Plymouth

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n8:Mt_Taranaki.jpg?width=300

dbo:abstract

The Taranaki Region of New Zealand is built upon the Median Batholith in the West, and Greywacke Rocks in the East. However, no rocks older than Miocene times are visible at the surface. The dominant feature of the Taranaki Region is the andesitic stratovolcano of Mount Taranaki, which is only about 130,000 years old. The dissected hill country to the East of the , and West of the Central Volcanic Plateau (Ruapehu and Tongariro) is composed of soft Miocene to Pleistocene sandstone and mudstone. The coastal lowlands around Wanganui to the South have well-developed Quaternary marine terraces, and coastal sand dunes. The Taranaki Basin is the only area in New Zealand with significant known oil and gas deposits, many of them offshore.

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wikipedia-en:Geology_of_Taranaki?oldid=959095685&ns=0

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7747

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wikipedia-en:Geology_of_Taranaki