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Duweishat gold mine, Northern State, Sudani
| Regional Level Types | |
|---|---|
| Duweishat gold mine | Mine (Abandoned) |
| Northern State | State |
| Sudan | Country |
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Latitude & Longitude (WGS84):
21° 21' 55'' North , 30° 58' 48'' East
Latitude & Longitude (decimal):
Type:
Mine (Abandoned) - last checked 2023
Köppen climate type:
## Ancient and Historic Mining
Gold mining in the Duweishat area dates back to antiquity, with significant Egyptian activity during the 2nd and 3rd millennia BC. Archaeological evidence reveals organized workshop sites built with dry-stone architecture for processing gold-bearing quartz, indicating considerable technical knowledge and local labor involvement. The presence of Nubian-style ceramics and mining installations points to the participation of regional populations alongside Egyptians, with mining continuing intermittently through medieval times.[1]
## Modern Investigations and Decline
In the late 20th century, Duweishat attracted geological interest for its mineral wealth. Survey missions throughout the 1970s and 1980s documented old pits, extraction scars, and relics of earlier mining phases. Despite attempts to revive larger-scale operations, logistical and organizational challenges led mining authorities to classify the site as abandoned by the early 21st century. The area nevertheless remains notable for its varied minerals, including gold, arsenopyrite, pyrite, quartz, staurolite, and others.[2][1]
## Resurgence of Artisanal Mining in the Present Day
Although officially listed as “abandoned,” recent satellite imagery and local field observations (2023–2025) reveal widespread ground disturbance and newly-dug pits at the Duweishat site. These features are typical of artisanal or small-scale gold mining, often carried out by local miners rather than large companies. Such activities revive historic patterns: individuals and informal groups have returned to previously exploited lodes, using manual methods to extract accessible gold. Regional economic pressures, rising gold prices, and improved access drive this renewed interest, even outside formal reporting channels.[2]
## Archaeological and Environmental Significance
Duweishat is recognized as an important archaeological location that encapsulates ancient Egyptian, Nubian, and medieval mining techniques, as well as the transition to modern, informal artisanal extraction. The resurgence of mining—unregulated and often resource-driven—raises new social and environmental concerns about site preservation, mercury use, and local welfare.[1][2]
***
In summary, Duweishat’s history tracks from ancient state-organized mining, through cycles of medieval and formal extraction, to a current revival of artisanal mining visible in recent satellite images and on-ground signs—reflecting Sudan’s broader gold mining story.[1][2]
[1](https://digitallibrary.un.org/record/119382/files/DP_UN_RAB-80-014_1--DP_UN_RAB-80-014_2-EN.pdf)
[2](https://www.mindat.org/loc-312536.html)
[3](https://www.mindat.org/loc-312535.html)
(A.I. generated by Perplexicity.ai)
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
14 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Arsenopyrite Formula: FeAsS |
| ⓘ Aurostibite Formula: AuSb2 |
| ⓘ Bornite Formula: Cu5FeS4 References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Chalcocite Formula: Cu2S |
| ⓘ Chalcopyrite Formula: CuFeS2 References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Covellite Formula: CuS References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Famatinite Formula: Cu3SbS4 References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Galena Formula: PbS |
| ⓘ Goethite Formula: Fe3+O(OH) References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Native Gold Formula: Au References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Native Gold var. Electrum Formula: (Au,Ag) References: Dr. Günter Grundmann collectionIdentified by Dr. Günter Grundmann: Polarised-light microscopy |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Staurolite Formula: Fe2+2Al9Si4O23(OH) |
| ⓘ 'Tennantite Subgroup' Formula: Cu6(Cu4C2+2)As4S12S |
| ⓘ 'Tetrahedrite Subgroup' Formula: Cu6(Cu4C2+2)Sb4S12S |
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold var. Electrum | 1.AA.05 | (Au,Ag) |
| ⓘ | 1.AA.05 | Au | |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Aurostibite | 2.EB.05a | AuSb2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | 'Tennantite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)As4S12S |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| ⓘ | Famatinite | 2.KA.10 | Cu3SbS4 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Goethite | 4.00. | Fe3+O(OH) |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 9 - Silicates | |||
| ⓘ | Staurolite | 9.AF.30 | Fe2+2Al9Si4O23(OH) |
List of minerals for each chemical element
Other Regions, Features and Areas containing this locality
AfricaContinent
African PlateTectonic Plate
- Arabian-Nubian Shield
- Bayuda TerraneVolcanic Arc
Arabian Plate
- Nubian ShieldShield
North Africa
- Sahara DesertDesert
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Duweishat gold mine, Northern State, Sudan