Takaka Terrane (original) (raw)

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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.

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dbo:abstract 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. (en) 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. (it)
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dbo:wikiPageWikiLink dbr:Calcium_carbonate dbr:Cambrian dbr:Basalt dbr:Brachiopod dbr:Devonian dbc:Landforms_of_the_Tasman_District dbc:Paleozoic_Oceania dbr:Early_Ordovician dbr:Conodont dbr:Geology_of_the_Tasman_District dbr:Geomorphology dbc:Geology_of_New_Zealand dbr:Mount_Arthur_(New_Zealand) dbr:Stratigraphy_of_New_Zealand dbr:Cobb_River,_New_Zealand dbr:Middle_Cambrian dbr:Torlesse_Composite_Terrane dbr:Trilobite dbr:Karst dbr:Late_Cambrian dbc:Terranes dbr:Dun_Mountain-Maitai_Terrane dbr:Paleozoic dbr:Batholiths dbr:Harwood_Hole dbr:Back-arc_basin dbr:Tasman_District dbr:Tasman_Sea dbr:Tasmania dbr:Kahurangi_National_Park dbr:Takaka_Hill dbr:Marble dbr:South_Island dbr:Ordovician dbr:Sandstone dbr:Weathering dbr:Terrane dbr:Riuwaka_River dbr:Cave_systems dbr:Glacial dbr:Haerenga_Supergroup dbr:Arthur_Marble dbr:Cameron_Group dbr:Devil_River_Volcanics_Group dbr:Edgecumbe_Group dbr:Ellis_Group,_New_Zealand dbr:Gendarme_Dolerite dbr:Haupiri_Group dbr:Junction_Formation dbr:Mount_Arthur_Group dbr:Mount_Patriarch_Group dbr:Tuhua_Intrusive dbr:Pegasus_Group dbr:Waka_Supergroup
dbp:age dbr:Cambrian dbr:Devonian ~ (en)
dbp:country New Zealand (en)
dbp:mapCaption Cross-section of New Zealand's stratigraphy (en)
dbp:name Takaka Terrane (en)
dbp:namedfor dbr:Takaka_Hill
dbp:period Paleozoic (en)
dbp:prilithology dbr:Basalt dbr:Marble dbr:Sandstone
dbp:region dbr:Tasman_District
dbp:subunits Haupiri, Devil River Volcanics, Mount Patriarch, Mount Arthur, Ellis, Edgecumbe, Cameron & Pegasus Groups (en)
dbp:type dbr:Terrane
dbp:underlies Tuhua Intrusive, Waka & Haerenga Supergroups (en)
dbp:unitof dbr:Stratigraphy_of_New_Zealand Western Province (en)
dbp:wikiPageUsesTemplate dbt:Infobox_rockunit dbt:Coord_missing dbt:Portal dbt:Reflist dbt:Fossil_range
dct:subject dbc:Landforms_of_the_Tasman_District dbc:Paleozoic_Oceania dbc:Geology_of_New_Zealand dbc:Terranes
rdfs:comment 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. (en) 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. (it)
rdfs:label Takaka Terrane (it) Takaka Terrane (en)
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prov:wasDerivedFrom wikipedia-en:Takaka_Terrane?oldid=1047292458&ns=0
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is dbo:wikiPageDisambiguates of dbr:Takaka_(disambiguation)
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