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Golden Crown Gold Mine, Day Dawn Goldfield, Cue, Cue Shire, Western Australia, Australia

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Latitude & Longitude (WGS84): 27° 27' 57'' South , 117° 51' 7'' East
Latitude & Longitude (decimal): -27.46608,117.85209
GeoHash:G#: qe5g9zcq8
Locality type:Mine
Köppen climate type:BWh : Hot deserts climate


Underground gold mine opened in 1986. Now relinquished.
Located 7 km S of Cue.

The mine is 500 metres south of the more well known Great Fingall Mine on the Day Dawn gold field. The first reports of mining found at Golden Crown was in 1896. Early 1896 the mine was purchased by a British syndicate called the British Coolgardie Mining Trust Company with J Lucas Balfour as mine manager and employing 20 men. Shortly after a rich lode was located and specimens were placed on display in Cue. The syndicate had purchased the Golden Crown and Golden Crown North leases, each 12 acres. Substantial money appears to have been invested into the mine at this time.

At this point the property was described as containing four shafts to the water level at 18 metres from the surface. Various drives were noted from the shafts accessing the lode up to 1.5 metres wide showing rich gold in a quartz reef. Mining was noted at the site till 1900, then all falls silent.

It is hard to believe what appears to be a rich mine was abandoned at this time. Western Australian newspapers are used as a reference as they once reported mining activities in the State in great detail. In 1938 a report surfaced that Western Mining controlled the leases, but had decided to surrender them. Neighbouring Great Fingall was noted at this time as being abandoned and derelict. Drilling was conducted at Golden Crown with promising results, but the cost of dewatering the mine and establishing new equipment etc was considered too great. They state the mine had been abandoned for a long time.

Cue Shire stated Golden Crown was operational in 2004, and I suspect at other times too (1986) but no information could be found. In 2010, a local mining company reported discovering visible gold below the resource boundary. This was at the southern portion of the main reef in quartz splays and wall rock alteration of the main reef. It states Golden Crown up to that point had produced 288 000 ounces of gold. Shortly after several gold specimens in grey quartz became available through an American dealer, probably from this discovery. This was largely because the exploration company is also a local specimen miner.

Gold is hosted at Golden Crown by a large quartz vein in a major fracture through a sill. Strong hydrothermal chlorite, and carbonate alteration occurs. Mineralisation is vein related rather than lode related. Gold bearing quartz veins are found in sheared mafic and ultramafic volcanics and sills. There is a second parallel mineralised reef 700 metres to the south-west, which cuts a dolerite sill at right angles, with the best gold found in the granophyric phase of the dolerite.


Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


14 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

Neoarchean - Mesoarchean
2500 - 3200 Ma



ID: 3188304
Archean volcanic rocks

Age: Archean (2500 - 3200 Ma)

Comments: Yilgarn Craton

Lithology: Greenstone belt; mafic-ultramafic volcanic 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]

Archean
2500 - 4000 Ma



ID: 873953
metamorphosed ultramafic rocks 74286

Age: Archean (2500 - 4000 Ma)

Description: Metamorphosed komatiite, pyroxenite, chlorite-tremolite schist, talc-chlorite schist, anthophyllite-tremolite-talc rock; olivine-cummingtonite schist; talc-carbonate-tremolite-chlorite rock, serpentinite; amphibole schist after pyroxenite

Comments: igneous ultramafic volcanic; meta-igneous ultramafic intrusive; synthesis of multiple published descriptions

Lithology: Igneous ultramafic volcanic; meta-igneous ultramafic intrusive

Reference: Raymond, O.L., Liu, S., Gallagher, R., Zhang, W., Highet, L.M. Surface Geology of Australia 1:1 million scale dataset 2012 edition. Commonwealth of Australia (Geoscience Australia). [5]

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

Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
Mock, C., Elliott, B.G., Ewers, G.R., Lorenz, R.P. (1987), Gold Deposits of Western Australia, BMR, Datafile (MINDEP), Resource Deposit 3, Department of Primary Industries and Energy, Bureau of Mineral Resources Geology and Geophysics, Commonwealth Government of Australia, 1987
The West Australian newspaper (Perth) (1896): Mining News (13 Feb 1896)
The Kalgoorlie Miner newspaper (1938): Great Fingall Reserve Abandoned by Western Mining (04 Jan 1938)
The Western Mail newspapers (Perth) (1897): Cue (22 Jan 1897)

External Links


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