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Statements

Subject Item
dbr:Takaka_Terrane
rdfs:label
Takaka Terrane Takaka Terrane
rdfs:comment
Il Takaka Terrane affiora nei monti del distretto di Tasman, nella provincia occidentale della Nuova Zelanda. Il terrane è costituito per lo più da marmo e rocce vulcaniche, ma ha una composizione molto variabile. The Takaka Terrane is a Paleozoic terrane that outcrops in the South Island of New Zealand. It is most extensively exposed within the Kahurangi National Park in the Tasman District. The terrane is mostly made up of marble and volcanic rocks but is highly variable in composition. It ranges in age from mid-Cambrian to Devonian time (510–400 Ma), including New Zealand's oldest rocks, which are found in the Cobb Valley in north-west Nelson. The Cobb Valley is also the location of "Trilobite Rock" a glacial dropstone made from the moulted exoskeletons of trilobites. Asbestos was mined in the Cobb Valley from the Takaka Terrene between the late 1880s and 1917. The Takaka Terrane is highly deformed and has been intruded by many batholiths.
dbp:name
Takaka Terrane
foaf:depiction
n9:NZ010415_Takaka_Hill_Walkway_02.jpg n9:Cross_Section_New_Zealand_geology.jpg
dcterms:subject
dbc:Paleozoic_Oceania dbc:Terranes dbc:Geology_of_New_Zealand dbc:Landforms_of_the_Tasman_District
dbo:wikiPageID
59008696
dbo:wikiPageRevisionID
1047292458
dbo:wikiPageWikiLink
dbr:Harwood_Hole dbr:Gendarme_Dolerite dbr:Terrane dbr:Paleozoic dbr:Torlesse_Composite_Terrane dbr:Early_Ordovician dbr:Ordovician dbr:Karst dbr:Batholiths dbr:Cameron_Group dbr:Cambrian dbr:Calcium_carbonate dbc:Paleozoic_Oceania dbr:Middle_Cambrian dbc:Terranes dbr:Trilobite dbr:Dun_Mountain-Maitai_Terrane dbr:Conodont dbr:Haupiri_Group dbr:Riuwaka_River dbr:Pegasus_Group dbr:Cobb_River,_New_Zealand dbr:Mount_Arthur_(New_Zealand) dbr:Tasman_District dbr:Geology_of_the_Tasman_District dbr:Mount_Arthur_Group dbr:Mount_Patriarch_Group dbr:Glacial dbr:Late_Cambrian dbr:Devil_River_Volcanics_Group dbr:Weathering dbc:Geology_of_New_Zealand dbc:Landforms_of_the_Tasman_District dbr:Devonian dbr:Back-arc_basin dbr:Brachiopod dbr:Arthur_Marble dbr:Waka_Supergroup dbr:Tasman_Sea dbr:Kahurangi_National_Park dbr:Tasmania dbr:Marble dbr:Edgecumbe_Group dbr:Stratigraphy_of_New_Zealand dbr:Ellis_Group,_New_Zealand dbr:South_Island dbr:Basalt dbr:Tuhua_Intrusive dbr:Haerenga_Supergroup dbr:Junction_Formation dbr:Geomorphology dbr:Sandstone dbr:Cave_systems dbr:Takaka_Hill
owl:sameAs
dbpedia-it:Takaka_Terrane wikidata:Q60752538 n14:9NQJL
dbp:subunits
Haupiri, Devil River Volcanics, Mount Patriarch, Mount Arthur, Ellis, Edgecumbe, Cameron & Pegasus Groups
dbp:underlies
Tuhua Intrusive, Waka & Haerenga Supergroups
dbp:unitof
dbr:Stratigraphy_of_New_Zealand Western Province
dbp:wikiPageUsesTemplate
dbt:Infobox_rockunit dbt:Coord_missing dbt:Fossil_range dbt:Portal dbt:Reflist
dbo:thumbnail
n9:NZ010415_Takaka_Hill_Walkway_02.jpg?width=300
dbp:age
~ dbr:Devonian dbr:Cambrian
dbp:country
New Zealand
dbp:mapCaption
Cross-section of New Zealand's stratigraphy
dbp:period
Paleozoic
dbp:region
dbr:Tasman_District
dbp:type
dbr:Terrane
dbo:abstract
Il Takaka Terrane affiora nei monti del distretto di Tasman, nella provincia occidentale della Nuova Zelanda. Il terrane è costituito per lo più da marmo e rocce vulcaniche, ma ha una composizione molto variabile. L'età varia dal Cambriano al Devoniano (510-400 milioni di anni fa) e include le rocce più antiche della Nuova Zelanda, ritrovate nella Cobb Valley, nella parte nordoccidentale della provincia di Nelson. Nella valle del fiume Cobb si trova anche la "Trilobite Rock" (roccia delle trilobiti), un ammasso roccioso di origine glaciale formato dagli esoscheletri delle trilobiti. Nella Cobb valley, tra il 1880 e il 1917, veniva estratto l'asbesto appartenente al Takaka Terrane. Il terrane è oggi fortemente deformato ed è stato intruso da molte batoliti. The Takaka Terrane is a Paleozoic terrane that outcrops in the South Island of New Zealand. It is most extensively exposed within the Kahurangi National Park in the Tasman District. The terrane is mostly made up of marble and volcanic rocks but is highly variable in composition. It ranges in age from mid-Cambrian to Devonian time (510–400 Ma), including New Zealand's oldest rocks, which are found in the Cobb Valley in north-west Nelson. The Cobb Valley is also the location of "Trilobite Rock" a glacial dropstone made from the moulted exoskeletons of trilobites. Asbestos was mined in the Cobb Valley from the Takaka Terrene between the late 1880s and 1917. The Takaka Terrane is highly deformed and has been intruded by many batholiths.
dbp:namedfor
dbr:Takaka_Hill
dbp:prilithology
dbr:Basalt dbr:Marble dbr:Sandstone
prov:wasDerivedFrom
wikipedia-en:Takaka_Terrane?oldid=1047292458&ns=0
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5182
foaf:isPrimaryTopicOf
wikipedia-en:Takaka_Terrane