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Hill 267, Stewart Island, Southland District, Southland Region, South Island, New Zealand

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Latitude & Longitude (WGS84): 46° 52' 38'' South , 167° 50' 44'' East
Latitude & Longitude (decimal): -46.87741,167.84567
KΓΆppen climate type:Cfb : Temperate oceanic climate


Named after the height of the hill the mineralisation is found around. Located in central Stewart Island, half-way between Paterson Inlet and the west coast of the island.

Strongly altered and deeply weathered leucogranite is riddled with cavities. Mineralisation outcrops over a 3 square kilometre area, as part of the regional Freshwater Fault system, trending north-west to south-east across the island.

The altered granite consists of quartz, muscovite, Fe Oxides, relict pyrite and molybdenite, and molybdenite intergrown with muscovite, W, Nb, and V bearing rutile, relict magmatic zircon, monazite, and trace tourmaline. The cavities are filled with Fe oxide and quartz, with locally relict pyrite and molybdenite. The altered granite contains 2-10 times the background Ag, Cu, and Se, and 10-100 times Mo, W, and Bi compared to the unaltered granite.

There is minor local enrichment of Au, Te, Se, Sn, and Mg, although no further species is mentioned. Mineralisation was concentrated in a roof of a pluton, now expressed as the range crest. Unaltered local granite consists of coarse equigranular two feldspar I-type leuco granodiorite, and leucogranite, with minor biotite, magnetite, and trace ilmenite.


Mineral List


8 valid minerals.

Rock Types Recorded

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Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Mesozoic - Paleozoic
66 - 541 Ma



ID: 3188901
Paleozoic-Mesozoic intrusive rocks

Age: Phanerozoic (66 - 541 Ma)

Lithology: Intrusive igneous rocks

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Mississippian
323.2 - 358.9 Ma



ID: 1310851
Tobin Suite

Age: Mississippian (323.2 - 358.9 Ma)

Stratigraphic Name: Tobin Suite

Description: Variably foliated biotite granite, leucogranite, granodiorite and tonalite.

Comments: Western Province (Tuhua Intrusives) Rocks

Lithology: Granite, leucogranite, granodiorite, tonalite

Reference: Edbrooke, S.W., Heron, D.W., Forsyth, P.J., Jongens, R. (compilers). Geology Map of New Zealand 1:1 000 000. GNS Science Geological Map 2. [12]

Visean
330.9 - 346.7 Ma



ID: 1356625
Ruggedy Granite (Tobin Suite)

Age: Mississippian (330.9 - 346.7 Ma)

Stratigraphic Name: Ruggedy Granite

Description: Coarse massive homogenous biotite granite and leucogranite.

Comments: Basement (Median Batholith) igneous rocks. Age based on U Pb dating

Lithology: Major:: {granite},Minor:: {leucogranite}

Reference: Heron, D.W. . Geology Map of New Zealand 1:250 000. GNS Science Geological Map 1. [13]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

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Allibone, A.H., MacKenzie, D., Turnbull, R, Turnbull, A., Craw, D. (2016) Polymetallic mineralisation associated with carboniferous I-type granitoids in Central Stewart Island New Zealand, New Zealand Journal of Geology and Geophysics, 59:3, 436-456.

 
Mineral and/or Locality  
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