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Statements

Subject Item
dbr:Northland_Allochthon
dbo:wikiPageWikiLink
dbr:Geology_of_the_Northland_Region
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dbr:Geology_of_the_Northland_Region
Subject Item
dbr:Geology_of_New_Zealand
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dbr:Geology_of_the_Northland_Region
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dbr:Geology_of_the_Auckland_Region
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dbr:Geology_of_the_Northland_Region
Subject Item
dbr:Geology_of_the_Northland_Region
rdfs:label
Geology of the Northland Region
rdfs:comment
New Zealand's Northland Region is built upon a basement consisting mainly of greywacke rocks, which are exposed on the eastern side of the peninsula. In-place Eocene coal measures crop out at Kamo, near Whangarei, and Oligocene limestone crops out at Hikurangi, near Whangarei.
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1121458764
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dbr:Whangarei dbr:Pillow_lava dbr:Halloysite dbr:Kaikohe dbr:Ngawha_Springs dbr:Kamo,_New_Zealand dbr:Ngawha_geothermal_field dbr:Cretaceous dbr:Triassic dbr:Volcanic_belt dbr:Northland_Region dbr:Dun_Mountain-Maitai_Terrane n8:90mile_beach_nz_landsatimage.jpg dbr:Obduction dbr:Oligocene dbr:Greywacke dbr:Miocene dbr:Sandstone dbr:Stratovolcano dbr:Year dbc:Northland_Region dbr:Tied_island dbr:Earthquake dbr:Quaternary dbr:Argillite dbr:Chert dbr:Auckland_Region dbr:Kiripaka dbr:Natural_gas dbr:Tsunami dbr:Quartz dbr:Petroleum dbr:Strike-slip_tectonics dbr:Northland_Peninsula dbr:Kaipara_Harbour dbr:Subduction dbr:Cape_Reinga dbr:Lava n8:North_Auckland_Peninsula.png dbr:Waipu,_New_Zealand dbr:Parakai dbr:Sand_dune dbr:Basalt dbr:Lithification dbc:Geology_of_New_Zealand_by_region dbr:Waiwera dbr:Volcanic_rock dbr:Dacite dbr:Limestone dbr:Transgression_(geology) dbr:King_Country dbr:Waikato dbr:Mudstone dbr:Taranaki dbr:Waro_Limestone_Scenic_Reserve dbr:Auckland dbr:Basement_(geology) dbr:Andesite dbr:Jurassic dbr:Bay_of_Islands dbr:Eocene n8:Bream_Head_end.jpg dbr:Terrane dbr:Permian dbr:Kerikeri dbr:Ahipara dbr:Geology_of_New_Zealand dbr:Allochthon dbr:Tombolo dbr:Aupouri_Peninsula
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n13:northland_mineral_resource_assessment.pdf
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n7:North_Auckland_Peninsula.png?width=300
dbo:abstract
New Zealand's Northland Region is built upon a basement consisting mainly of greywacke rocks, which are exposed on the eastern side of the peninsula. In-place Eocene coal measures crop out at Kamo, near Whangarei, and Oligocene limestone crops out at Hikurangi, near Whangarei. A subduction zone is believed to have existed to the northeast of Northland in early Miocene times, causing the Northland Allochthon to thrust over much of the peninsula and volcanic belts to develop on either side of the peninsula. Intra-plate basaltic volcanic activity has occurred around Kaikohe, the Bay of Islands, and Whangarei since late Miocene times. Sand dunes sourced from volcanoes further south occupy much of the western coast, and the Aupouri Peninsula joins previously separate islands to the mainland to form a large tombolo.
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wikipedia-en:Geology_of_the_Northland_Region
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dbr:Northland_Region
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dbr:Geology_of_the_Northland_Region
Subject Item
dbr:Auckland_regional_faults
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dbr:Geology_of_the_Northland_Region
Subject Item
dbr:Geology_of_Northland_Region,_New_Zealand
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dbr:Geology_of_the_Northland_Region
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dbr:Geology_of_the_Northland_Region
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dbr:Geology_of_the_Northland_Region,_New_Zealand
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dbr:Geology_of_the_Northland_Region
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dbr:Geology_of_the_Northland_Region
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dbr:Geology_of_the_Northland_Region