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Sukari gold mine, Marsa Alam, Red Sea Governorate, Egypti
| Regional Level Types | |
|---|---|
| Sukari gold mine | Mine (Active) |
| Marsa Alam | Municipal District |
| Red Sea Governorate | Governorate |
| Egypt | Country |
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Latitude & Longitude (WGS84):
24° 56' 49'' North , 34° 42' 58'' East
Latitude & Longitude (decimal):
Type:
Mine (Active) - last checked 2024
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Marsa Alam | 10,000 (2014) | 21.7km |
Other/historical names associated with this locality:
Sukari Mine; Sukkari Gold mine
Located 15 km west of the Red Sea coast (23 km west of the coastal town of Marsa Alam) in the southern central Eastern Desert of Egypt, on Sukari Hill.
Gold was worked by the Pharaohs and the Romans.
Estimated resources: 18.8 Mt at 2.41 g/t Au.
Sukari consists of four primary zones that contain varying degrees of ore: Amun, Ra, Gazelle, and Pharaoh. The open pit is based on the Main and Hapi ore zones which have been drilled extensively in the Amun and Ra/ Gazelle areas revealing various high-grade zones.
The epi-mesothermal mineralization is associated with stacked quartz veins and stockworks (repeated veining and leaching followed by leaching) in an altered granodiorite/rhyodacite porphyry.
The mine comprises both an open pit and underground operations.
The mine is half owned by Centamin Plc which operates the mine through its wholly owned subsidiary Pharoah Gold Mines NL (the other half is owned by the Egyptian Mineral Resources Authority. The mine is within an overall mining concession comprising some 160km2.
Important prosepcts within the mine area include: Sukari North; V_Shear East; Wadi El Alam; Wadi Um Tunduba, Kurdeman East; Kurdeman North; Horus South; and Sami South.
Gold was worked by the Pharaohs and the Romans.
Estimated resources: 18.8 Mt at 2.41 g/t Au.
Sukari consists of four primary zones that contain varying degrees of ore: Amun, Ra, Gazelle, and Pharaoh. The open pit is based on the Main and Hapi ore zones which have been drilled extensively in the Amun and Ra/ Gazelle areas revealing various high-grade zones.
The epi-mesothermal mineralization is associated with stacked quartz veins and stockworks (repeated veining and leaching followed by leaching) in an altered granodiorite/rhyodacite porphyry.
The mine comprises both an open pit and underground operations.
The mine is half owned by Centamin Plc which operates the mine through its wholly owned subsidiary Pharoah Gold Mines NL (the other half is owned by the Egyptian Mineral Resources Authority. The mine is within an overall mining concession comprising some 160km2.
Important prosepcts within the mine area include: Sukari North; V_Shear East; Wadi El Alam; Wadi Um Tunduba, Kurdeman East; Kurdeman North; Horus South; and Sami South.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded from this region.Mineral List
Mineral list contains entries from the region specified including sub-localities16 valid minerals.
Rock Types Recorded
Rock list contains entries from the region specified including sub-localities
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Albite Formula: Na(AlSi3O8) |
| ⓘ Ankerite Formula: Ca(Fe2+,Mg)(CO3)2 |
| ⓘ Arsenopyrite Formula: FeAsS |
| ⓘ Calcite Formula: CaCO3 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Dolomite Formula: CaMg(CO3)2 |
| ⓘ Galena Formula: PbS |
| ⓘ Graphite Formula: C |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ 'Monazite Group' Formula: REE(PO4) |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Native Gold Formula: Au |
| ⓘ Pyrite Formula: FeS2 Description: Arsenian pyrite. |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Quartz var. Milky Quartz Formula: SiO2 |
| ⓘ Quartz var. Smoky Quartz Formula: SiO2 |
| ⓘ Sphalerite Formula: ZnS |
| ⓘ Talc Formula: Mg3Si4O10(OH)2 |
| ⓘ Zircon Formula: Zr(SiO4) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
| ⓘ | Graphite | 1.CB.05a | C |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | var. Smoky Quartz | 4.DA.05 | SiO2 |
| ⓘ | var. Milky Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Ankerite | 5.AB.10 | Ca(Fe2+,Mg)(CO3)2 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| Group 9 - Silicates | |||
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Talc | 9.EC.05 | Mg3Si4O10(OH)2 |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Monazite Group' | - | REE(PO4) |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Talc | Mg3Si4O10(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Graphite | C |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Monazite Group | REE(PO4) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Quartz var. Smoky Quartz | SiO2 |
| O | ⓘ Talc | Mg3Si4O10(OH)2 |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Quartz var. Milky Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Mg | Magnesium | |
| Mg | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Mg | ⓘ Talc | Mg3Si4O10(OH)2 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Quartz var. Smoky Quartz | SiO2 |
| Si | ⓘ Talc | Mg3Si4O10(OH)2 |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Quartz var. Milky Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| P | Phosphorus | |
| P | ⓘ Monazite Group | REE(PO4) |
| S | Sulfur | |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Sphalerite | ZnS |
| K | Potassium | |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Fe | Iron | |
| Fe | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Au | Gold | |
| Au | ⓘ Native Gold | Au |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
Other Databases
| Wikipedia: | https://en.wikipedia.org/wiki/Sukari_mine |
|---|---|
| Wikidata ID: | Q2178849 |
Localities in this Region
- Red Sea Governorate
- Marsa Alam
- Red Sea Governorate
- Marsa Alam
- Sukari gold mine
- Marsa Alam
Other Regions, Features and Areas containing this locality
AfricaContinent
- Sahara DesertDesert
African PlateTectonic Plate
Arabian Plate
- Arabian-Nubian ShieldShield
- East Desert TerraneVolcanic Arc
- Nubian ShieldShield
Egypt
- Eastern DesertDesert
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References
Helmy, HassanM., Kaindl, Reinhard, Fritz, Harald, Loizenbauer, Jürgen (2004) The Sukari Gold Mine, Eastern Desert - Egypt: structural setting, mineralogy and fluid inclusion study. Mineralium Deposita, 39 (4). 495-511 doi:10.1007/s00126-004-0426-z
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