Hillcrest South Gold Mine, Jumbulyer Goldfield, Mount Magnet, Mount Magnet Shire, Western Australia, Australiai
Regional Level Types | |
---|---|
Hillcrest South Gold Mine | Mine |
Jumbulyer Goldfield | Ore Field |
Mount Magnet | Mountain |
Mount Magnet Shire | Shire |
Western Australia | State |
Australia | Country |
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Latitude & Longitude (WGS84):
28° 7' 16'' South , 117° 48' 36'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Mount Magnet | 457 (2012) | 7.3km |
Mindat Locality ID:
264657
Long-form identifier:
mindat:1:2:264657:5
GUID (UUID V4):
2fc8c871-f2d7-4bce-afa8-827d74de21cf
The only report found was from 1928. It is described as being located approximately 750 metres south of the Hillcrest Mine. It is owned at this time by a Constable Wright and J. Combes. Total production from the mine up to this point was 300 tonnes for 105 oz at 7 dwt per tonne. There is a shaft to 120 feet. The article indicates the shaft was only being sunk further down to gain water, it is assumed for gold production from the higher levels. The Mindat co-ordinates are approximate, and no major workings can be seen.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
3 valid minerals.
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Gold | 1.AA.05 | Au |
Group 2 - Sulphides and Sulfosalts | |||
ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
ⓘ | Pyrite | 2.EB.05a | FeS2 |
List of minerals for each chemical element
S | Sulfur | |
---|---|---|
S | ⓘ Pyrite | FeS2 |
S | ⓘ Pyrrhotite | Fe1-xS |
Fe | Iron | |
Fe | ⓘ Pyrite | FeS2 |
Fe | ⓘ Pyrrhotite | Fe1-xS |
Au | Gold | |
Au | ⓘ Gold | Au |
Other Regions, Features and Areas containing this locality
Australia
- Western Australia
- West Australian ElementCraton
- Yilgarn CratonCraton
Australian PlateTectonic Plate
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