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Statements

Subject Item
dbr:Geology_of_the_Tasman_District
rdfs:label
Geology of the Tasman District
rdfs:comment
The Tasman Region, and the small adjoining Nelson Region, form one of the more geologically interesting regions of New Zealand. It contains the oldest rocks of anywhere on New Zealand's main islands. It contains all the main terranes that make up New Zealand's basement. These basement rocks include Ultramafic rocks, such as Serpentine and Dunite, and valuable minerals, such as Gold. The Nelson Region is bordered to the south by the Alpine Fault (usually named the Wairau Fault in the Wairau Valley), the main fault forming the boundary between the Pacific Plate and the Indo-Australian Plate, that generated the Southern Alps.
foaf:depiction
n9:Cross_Section_New_Zealand_geology.jpg n9:Cobb_Reservoir_Lake_in_autumn.jpg n9:Mount_Arthur_(New_Zealand)_054.jpg n9:Dun_mountain_Nelson_New_Zealand.jpg n9:Clifftopwalk_NZ_2005.jpg
dcterms:subject
dbc:Tasman_District dbc:Nelson_Region dbc:Geography_of_the_Marlborough_Region dbc:Marlborough_Region dbc:Geology_of_New_Zealand_by_region dbc:Geography_of_the_Nelson_Region dbc:Geography_of_the_Tasman_District
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dbr:GNS_Science dbr:Mudstone dbr:Takaka dbr:Indo-Australian_Plate dbr:Alpine_Fault dbr:Dun_Mountain dbr:Mount_Arthur_(New_Zealand) dbr:Nelson_Region dbr:Awatere_Fault dbr:Gold dbr:Dunite dbc:Tasman_District dbr:Anatoki_Fault dbr:Dun_Mountain-Maitai_Terrane dbr:Pacific_Plate dbr:Wairau_Fault dbr:Marlborough_Fault_System dbr:Tasman_Region dbr:Geology_of_New_Zealand dbc:Nelson_Region dbr:Ultramafic_rock dbr:Harwood_Hole dbr:Cisuralian dbr:Limestone dbc:Geography_of_the_Marlborough_Region dbr:Serpentine_group dbr:Takaka_Terrane n14:Cross_Section_New_Zealand_geology.jpg dbc:Marlborough_Region dbr:D'Urville_Island_(New_Zealand) dbr:Southern_Alps_(New_Zealand) dbr:List_of_rock_formations_of_New_Zealand dbc:Geology_of_New_Zealand_by_region dbc:Geography_of_the_Nelson_Region dbr:Karamea dbr:Stratigraphy_of_New_Zealand dbc:Geography_of_the_Tasman_District dbr:Farewell_Spit
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n15:Ballance_NZ_Geology-V2.pdf
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wikidata:Q5535429 n16:4kiLu
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dbo:thumbnail
n9:Mount_Arthur_(New_Zealand)_054.jpg?width=300
dbp:footer
Clockwise, Mount Arthur marble, Old Man Range near Farewell Spit, Dun Mountain, Cobb Valley
dbp:image
Cobb Reservoir Lake in autumn.jpg Mount Arthur 054.jpg Dun mountain Nelson New Zealand.jpg Clifftopwalk NZ 2005.jpg
dbp:perrow
2
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330
dbo:abstract
The Tasman Region, and the small adjoining Nelson Region, form one of the more geologically interesting regions of New Zealand. It contains the oldest rocks of anywhere on New Zealand's main islands. It contains all the main terranes that make up New Zealand's basement. These basement rocks include Ultramafic rocks, such as Serpentine and Dunite, and valuable minerals, such as Gold. The Nelson Region is bordered to the south by the Alpine Fault (usually named the Wairau Fault in the Wairau Valley), the main fault forming the boundary between the Pacific Plate and the Indo-Australian Plate, that generated the Southern Alps.
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wikipedia-en:Geology_of_the_Tasman_District