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Rocky's Reward Mine, Leinster, Leonora Shire, Western Australia, Australiai
| Regional Level Types | |
|---|---|
| Rocky's Reward Mine | Mine (Inactive) |
| Leinster | - not defined - |
| Leonora Shire | Shire |
| Western Australia | State |
| Australia | Country |
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Latitude & Longitude (WGS84):
27° 47' 40'' South , 120° 41' 54'' East
Latitude & Longitude (decimal):
Type:
Mine (Inactive) - last checked 2021
Köppen climate type:
The Rocky's Reward Mine is two kilometres north of the Perseverence Mine, and operated as both an open pit and underground mine. Production started in 1988, with the underground mine closing in 2000, and the open pit in 2009. The abandoned mine is owned by BHP Billiton, under its Nickelwest operations.
The mine contains disseminated and massive sulphides hosted by two thin komatiite horizons, within felsic volcanics and sediments. The sulphides are found in a high strain corridor which is similar to Perseverence. The ultramafic rocks are coarse grained, randomly orientated metamorphic olivine pseudomorphed by serpentinites, with carbonate alteration assemblages on the margins. The ultramafics are hydrothermally altered,and metamorphically recrystallised and serpentinised with the primary igneous textures seldom preserved.
The mineralisation is massive sulphides at 4-6% Ni and heavy disseminated sulphides at 0.7-4% Ni, both dominated by pyrrhotite and pentlandite, with widely dispersed but minor chalcopyrite. In the massive sulphide, the minerals have recrystallised into medium to coarse grained interlocking granoblastic textures, with some relict ductile fabrics in the massive sulphide sheets.
The disseminated sulphides show coarse triangular sulphide aggregates interstitial to the serpentine pseudomorphs after bladed textured metamorphic olivines. Hydrothermal alteration introduced arsenic and produced gersdorffite, cobaltite, and niccolite.
The mineralisation is only found in the ultramafic layers, folded into a steep north trending fold axis, forming two vertically stacked mineral layers, plunging 10-15 degrees north. It is truncated to the west by a steep dipping, north trending strain zone containing abundant remobilised massive sulphide.
The only specimens labelled from the mine for sale in recent years is gold in matrix. This seems unlikely from a nickel deposit, and no geology information could be found about gold at the mine. No historic mine could be located in the area by the name Rocky's Reward, although there are numerous gold ore-bodies in the district, and they may have come from nearby.
The mine contains disseminated and massive sulphides hosted by two thin komatiite horizons, within felsic volcanics and sediments. The sulphides are found in a high strain corridor which is similar to Perseverence. The ultramafic rocks are coarse grained, randomly orientated metamorphic olivine pseudomorphed by serpentinites, with carbonate alteration assemblages on the margins. The ultramafics are hydrothermally altered,and metamorphically recrystallised and serpentinised with the primary igneous textures seldom preserved.
The mineralisation is massive sulphides at 4-6% Ni and heavy disseminated sulphides at 0.7-4% Ni, both dominated by pyrrhotite and pentlandite, with widely dispersed but minor chalcopyrite. In the massive sulphide, the minerals have recrystallised into medium to coarse grained interlocking granoblastic textures, with some relict ductile fabrics in the massive sulphide sheets.
The disseminated sulphides show coarse triangular sulphide aggregates interstitial to the serpentine pseudomorphs after bladed textured metamorphic olivines. Hydrothermal alteration introduced arsenic and produced gersdorffite, cobaltite, and niccolite.
The mineralisation is only found in the ultramafic layers, folded into a steep north trending fold axis, forming two vertically stacked mineral layers, plunging 10-15 degrees north. It is truncated to the west by a steep dipping, north trending strain zone containing abundant remobilised massive sulphide.
The only specimens labelled from the mine for sale in recent years is gold in matrix. This seems unlikely from a nickel deposit, and no geology information could be found about gold at the mine. No historic mine could be located in the area by the name Rocky's Reward, although there are numerous gold ore-bodies in the district, and they may have come from nearby.
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
12 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 References: |
| ⓘ Cobaltite Formula: CoAsS |
| ⓘ 'Fayalite-Forsterite Series' References: |
| ⓘ Gersdorffite Formula: NiAsS |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 References: Ben GrguricIdentified by Ben Grguric: Optical Analysis, XRD, SEM-EDS |
| ⓘ Millerite Formula: NiS |
| ⓘ Mountkeithite Formula: [(Mg1-xFe3+x)(OH)2][SO4]x/2 · nH2O References: Ben GrguricIdentified by Ben Grguric: Optical Analysis, XRD, SEM-EDS |
| ⓘ Nickeline Formula: NiAs |
| ⓘ Pentlandite Formula: (NixFey)Σ9S8 |
| ⓘ Pyrrhotite Formula: Fe1-xS |
| ⓘ 'Serpentine Subgroup' Formula: D3[Si2O5](OH)4 References: Ben GrguricIdentified by Ben Grguric: Optical Analysis, XRD, SEM-EDS |
| ⓘ Takovite Formula: Ni6Al2(OH)16[CO3] · 4H2O References: Sorrell, Steve (n.d.) Personal communication.Identification: Dealer/Collection Label |
| ⓘ Violarite Formula: Fe2+Ni3+2S4 References: Ben GrguricIdentified by Ben Grguric: Optical Analysis, XRD, SEM-EDS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Pentlandite | 2.BB.15 | (NixFey)Σ9S8 |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Nickeline | 2.CC.05 | NiAs |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Millerite | 2.CC.20 | NiS |
| ⓘ | Violarite | 2.DA.05 | Fe2+Ni3+2S4 |
| ⓘ | Cobaltite | 2.EB.25 | CoAsS |
| ⓘ | Gersdorffite | 2.EB.25 | NiAsS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Takovite | 5.DA.50 | Ni6Al2(OH)16[CO3] · 4H2O |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Mountkeithite | 7.DD.35 | [(Mg1-xFe3+x)(OH)2][SO4]x/2 · nH2O |
| Unclassified | |||
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Serpentine Subgroup' | - | D3[Si2O5](OH)4 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Mountkeithite | [(Mg1-xFex3+)(OH)2][SO4]x/2 · nH2O |
| H | ⓘ Takovite | Ni6Al2(OH)16[CO3] · 4H2O |
| H | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| C | Carbon | |
| C | ⓘ Takovite | Ni6Al2(OH)16[CO3] · 4H2O |
| O | Oxygen | |
| O | ⓘ Chromite | Fe2+Cr23+O4 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Mountkeithite | [(Mg1-xFex3+)(OH)2][SO4]x/2 · nH2O |
| O | ⓘ Takovite | Ni6Al2(OH)16[CO3] · 4H2O |
| O | ⓘ Fayalite-Forsterite Series | |
| O | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| Mg | Magnesium | |
| Mg | ⓘ Mountkeithite | [(Mg1-xFex3+)(OH)2][SO4]x/2 · nH2O |
| Mg | ⓘ Fayalite-Forsterite Series | |
| Al | Aluminium | |
| Al | ⓘ Takovite | Ni6Al2(OH)16[CO3] · 4H2O |
| Si | Silicon | |
| Si | ⓘ Fayalite-Forsterite Series | |
| Si | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| S | Sulfur | |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Cobaltite | CoAsS |
| S | ⓘ Gersdorffite | NiAsS |
| S | ⓘ Millerite | NiS |
| S | ⓘ Mountkeithite | [(Mg1-xFex3+)(OH)2][SO4]x/2 · nH2O |
| S | ⓘ Pentlandite | (NixFey)Σ9S8 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Violarite | Fe2+Ni23+S4 |
| Cr | Chromium | |
| Cr | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | Iron | |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Mountkeithite | [(Mg1-xFex3+)(OH)2][SO4]x/2 · nH2O |
| Fe | ⓘ Pentlandite | (NixFey)Σ9S8 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Violarite | Fe2+Ni23+S4 |
| Fe | ⓘ Fayalite-Forsterite Series | |
| Co | Cobalt | |
| Co | ⓘ Cobaltite | CoAsS |
| Ni | Nickel | |
| Ni | ⓘ Gersdorffite | NiAsS |
| Ni | ⓘ Millerite | NiS |
| Ni | ⓘ Nickeline | NiAs |
| Ni | ⓘ Pentlandite | (NixFey)Σ9S8 |
| Ni | ⓘ Takovite | Ni6Al2(OH)16[CO3] · 4H2O |
| Ni | ⓘ Violarite | Fe2+Ni23+S4 |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| As | Arsenic | |
| As | ⓘ Cobaltite | CoAsS |
| As | ⓘ Gersdorffite | NiAsS |
| As | ⓘ Nickeline | NiAs |
Other Regions, Features and Areas containing this locality
Australia
- Western Australia
- Mount Keith Nickel Metallogenic ProvinceGeologic Province
- West Australian ElementCraton
- Yilgarn CratonCraton
Australian PlateTectonic Plate
- West Australian Craton
- Eastern Yilgarn CratonCraton
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
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References
Barnes, Stephen J., Gole, Martin J., Hill, Robin E. T. (1988) The Agnew nickel deposit, Western Australia: Part II. Sulfide geochemistry, with emphasis on the platinum-group elements. Economic Geology, 83 (3). 537-550 doi:10.2113/gsecongeo.83.3.537



Rocky's Reward Mine, Leinster, Leonora Shire, Western Australia, Australia