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Mount Allen Copper prospect, Mount Hope, Blaxland Co., New South Wales, Australiai
| Regional Level Types | |
|---|---|
| Mount Allen Copper prospect | Prospect (Abandoned) |
| Mount Hope | Mountain |
| Blaxland Co. | County |
| New South Wales | State |
| Australia | Country |
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Latitude & Longitude (WGS84):
32° 44' 33'' South , 145° 51' 52'' East
Latitude & Longitude (decimal):
Type:
Prospect (Abandoned) - last checked 2026
Age:
At least 393.3 ยฑ 1.2 Ma
Geologic Time:
Reference for age:
Gilligan, L.B., Suppel, D.W. (1993) Metallogenic Study and Mineral Deposit Data Sheets: Nymagee 1:250 000 Metallogenic Map (SI/55-2). Geological Survey of New South Wales, Sydney, 171 pages.
Kรถppen climate type:
A former small underground mine with shafts and shallow pits. Operated early 1900s.
Copper mineralisation was at depth, however mined for ironstone flux for the Mount Hope Copper Mine about 16 kilometres to the south, then as a gold mine for a short period.
Carne (1908) states: 'The ironstone flux was carted from Mount Allen, a distance of 10 miles and formed a serious item in the expenditure. A large amount of this flux was used by the New Mount Hope Company before its auriferous nature was discovered which resulted in the Mount Allen Gold Mining Company being formed. Gold mining operations were established and successfully maintained for a time when the gold yields fell below payable proportions. Cyanidation was afterwards resorted to for the large amount of ironstone tailings produced by the battery treatment. The tailings were purchased by the copper company at 7s. per ton for fluxing purposes, but the supply was stopped in view of the new treatment. The purchase, mining and carriage of ironstone flux at the Mount Hope attracted an expenditure of 15s. per ton which should expediate the development of the sulphide resources of Mount Hope.'
According to McQueen (2021) The Mount Allen site was discovered by Richard Jones who sank a shaft and adit but lacked capital so sold the mine to the Mount Hope Copper Company as a source of ironstone flux.
Peter Bergan Febuary 1885 discovered gold in the flux material however lacked capital to develop the mine, so it continued to be mined for flux until 1891. Joseph Reilly formed the Mount Allen Gold Mining Company with John Hutchens appointed the mine manager. The Mount Hope Copper Company received government compensation for the loss of its ironstone flux source. A ten head battery was installed, however much gold was lost to the tailings as it was very fine and muddy water used. There was spasmodic production for the next three years. In November 28 1895 the mine manager's house and office burnt down. In September 1896 the company was reconstructed to access more capital. Mining ceased late 1897 due to the easily available ore being exhausted. The tailings were reprocessed in 1899. In 1901 the Great Central Freehold Mines Ltd purchased the mine however little was done with it. Tributors took out a small amount of gold in 1909. Total production across the entire period was 6,974 oz gold.
The ore was described as gossan and oxidised ore in the upper levels, and deeper pyritic with copper sulphides, and supergene gold enrichment.
Gilligan (1993) lists a Mount Allen Cu, and Mt Allen Au-Fe (Bi, W) P68 and in the metal data cards section separately. They are under different rock types in the same area, however it is possible it's one and the same mine. The reference only describes the second mine (pp 69-70).
The quarry and immediate area shows rhyolitic tuff, sandstone, shale, quartz-magnetite rock, and hematite-magnetite-chlorite siltstone. Low grade gold is distributed erratically in strongly chloritic siltstone up to 90 metres wide. The ironstone is massive hematite and lesser magnetite as lenses the largest 18 metres long, 9 metres wide and over 30 metres deep. Au, Ag and minor Bi, W, Se values were found in the iron ore, and pyrite in the Fe siltstone. Sulphide mineralisation at depth contained pyrite, pyrrhotite and minor chalcopyrite as disseminations and associated with quartz veins. There were minor Pb-Zn values in the overlying volcanics.
Copper mineralisation was at depth, however mined for ironstone flux for the Mount Hope Copper Mine about 16 kilometres to the south, then as a gold mine for a short period.
Carne (1908) states: 'The ironstone flux was carted from Mount Allen, a distance of 10 miles and formed a serious item in the expenditure. A large amount of this flux was used by the New Mount Hope Company before its auriferous nature was discovered which resulted in the Mount Allen Gold Mining Company being formed. Gold mining operations were established and successfully maintained for a time when the gold yields fell below payable proportions. Cyanidation was afterwards resorted to for the large amount of ironstone tailings produced by the battery treatment. The tailings were purchased by the copper company at 7s. per ton for fluxing purposes, but the supply was stopped in view of the new treatment. The purchase, mining and carriage of ironstone flux at the Mount Hope attracted an expenditure of 15s. per ton which should expediate the development of the sulphide resources of Mount Hope.'
According to McQueen (2021) The Mount Allen site was discovered by Richard Jones who sank a shaft and adit but lacked capital so sold the mine to the Mount Hope Copper Company as a source of ironstone flux.
Peter Bergan Febuary 1885 discovered gold in the flux material however lacked capital to develop the mine, so it continued to be mined for flux until 1891. Joseph Reilly formed the Mount Allen Gold Mining Company with John Hutchens appointed the mine manager. The Mount Hope Copper Company received government compensation for the loss of its ironstone flux source. A ten head battery was installed, however much gold was lost to the tailings as it was very fine and muddy water used. There was spasmodic production for the next three years. In November 28 1895 the mine manager's house and office burnt down. In September 1896 the company was reconstructed to access more capital. Mining ceased late 1897 due to the easily available ore being exhausted. The tailings were reprocessed in 1899. In 1901 the Great Central Freehold Mines Ltd purchased the mine however little was done with it. Tributors took out a small amount of gold in 1909. Total production across the entire period was 6,974 oz gold.
The ore was described as gossan and oxidised ore in the upper levels, and deeper pyritic with copper sulphides, and supergene gold enrichment.
Gilligan (1993) lists a Mount Allen Cu, and Mt Allen Au-Fe (Bi, W) P68 and in the metal data cards section separately. They are under different rock types in the same area, however it is possible it's one and the same mine. The reference only describes the second mine (pp 69-70).
The quarry and immediate area shows rhyolitic tuff, sandstone, shale, quartz-magnetite rock, and hematite-magnetite-chlorite siltstone. Low grade gold is distributed erratically in strongly chloritic siltstone up to 90 metres wide. The ironstone is massive hematite and lesser magnetite as lenses the largest 18 metres long, 9 metres wide and over 30 metres deep. Au, Ag and minor Bi, W, Se values were found in the iron ore, and pyrite in the Fe siltstone. Sulphide mineralisation at depth contained pyrite, pyrrhotite and minor chalcopyrite as disseminations and associated with quartz veins. There were minor Pb-Zn values in the overlying volcanics.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
4 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| โ Azurite Formula: Cu3(CO3)2(OH)2 |
| โ Malachite Formula: Cu2(CO3)(OH)2 |
| โ Native Gold Formula: Au |
| โ Tenorite ? Formula: CuO |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| โ | Native Gold | 1.AA.05 | Au |
| Group 4 - Oxides and Hydroxides | |||
| โ | Tenorite ? | 4.AB.10 | CuO |
| Group 5 - Nitrates and Carbonates | |||
| โ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| โ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | โ Azurite | Cu3(CO3)2(OH)2 |
| H | โ Malachite | Cu2(CO3)(OH)2 |
| C | Carbon | |
| C | โ Azurite | Cu3(CO3)2(OH)2 |
| C | โ Malachite | Cu2(CO3)(OH)2 |
| O | Oxygen | |
| O | โ Azurite | Cu3(CO3)2(OH)2 |
| O | โ Malachite | Cu2(CO3)(OH)2 |
| O | โ Tenorite | CuO |
| Cu | Copper | |
| Cu | โ Azurite | Cu3(CO3)2(OH)2 |
| Cu | โ Malachite | Cu2(CO3)(OH)2 |
| Cu | โ Tenorite | CuO |
| Au | Gold | |
| Au | โ Native Gold | Au |
Other Regions, Features and Areas containing this locality
Australia
- Lachlan OrogenOrogen
- Central NSW - Omeo ProvinceGeologic Province
- Mount Hope Trough
Australian PlateTectonic Plate
- Lachlan Fold Belt
- Stalwell ZoneOrogenic Belt
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