Log In
Bagagem River valley, Minas Gerais, Brazili
| Regional Level Types | |
|---|---|
| Bagagem River valley | Valley |
| Minas Gerais | State |
| Brazil | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
18° South , 47° West (est.)
Estimate based on other nearby localities or region boundaries.
Margin of Error:
~16km
Type:
Köppen climate type:
Name(s) in local language(s):
Rio Bagagem
In 1853, a diamond discovered in alluvial deposits of the Bagagem River valley about 60 km SW of Coromandel became the first large Brazilian diamond whose history is fully authenticated. Named “Estrela do Sul” (Star of the South), it weighed 261.9 carats. It was found by a slave, who turned it in and was rewarded with her freedom and granted a lifetime pension. Additional notable stones discovered in the same area include one weighing 122.5 carats (found four years later, in 1857), and others: 118 carats (1929), 108 carats (1940), and 174.5 carats (1954).
A sprawling community grew in the area to provide services for participants in the ensuing diamond rush. First named “Bagagem” (“baggage” in English), it was later renamed after the famous stone, the Estrela do Sul. Just downstream (NW) from Estrela do Sul is the village of São Rita da Estrela that borders several quarries (called “garimpos” in Brazil), and the major digs are readily visible in satellite photos further down the river (generally NNW), all the way to the flooded portion associated with Emborcação Reservoir on the Paranaíba River. Diamond production data are not available for any of those quarries, and one or more of them may be where some of the large stones mentioned above were discovered. The town of Estrela do Sul is close to the main area of alluvial diamond mining, so its geographic coordinates are used for the locality. In fact, Estrela do Sul is where that 261.9 carat stone was discovered. Romaria is a larger town and municipality, but few major quarries were established that far upriver.
Several publications list Romaria as the name of a diamond district, but Romaria and Bagagem River valley both lie within the area that has long been included in the Coromandel diamond district (e.g., see Fig. 1 in Karfunkel et al., 1994), so this area is included in the Coromandel district here, with Romaria mine as a sublocality. The diamond occurrence at the Romaria mine is apparently in a debris flow conglomerate that is lithified, rather than in alluvium, and details on its geology are presented in the Romaria locality description. Fleischer (1998) mentioned that the conglomerate at Romaria extends to Iraí de Minas, which is also considered to be a sublocality of Bagagem River valley.
The discussion of geological circumstances of alluvial diamond occurrences in the locality description for Coromandel district applies to Bagagem River valley.
Geographic coordinates for significant quarries and clusters of quarries along Bagagem River, from Google Earth:
1) several quarries from 18° 51' 28", 47° 37' 51" to 18° 51' 8", 47° 39' 2"
2) 18° 42' 19", 47° 41' 51"
3) large area near Emborcação Reservoir in 18° 41' 14", 47° 41' 49".
A sprawling community grew in the area to provide services for participants in the ensuing diamond rush. First named “Bagagem” (“baggage” in English), it was later renamed after the famous stone, the Estrela do Sul. Just downstream (NW) from Estrela do Sul is the village of São Rita da Estrela that borders several quarries (called “garimpos” in Brazil), and the major digs are readily visible in satellite photos further down the river (generally NNW), all the way to the flooded portion associated with Emborcação Reservoir on the Paranaíba River. Diamond production data are not available for any of those quarries, and one or more of them may be where some of the large stones mentioned above were discovered. The town of Estrela do Sul is close to the main area of alluvial diamond mining, so its geographic coordinates are used for the locality. In fact, Estrela do Sul is where that 261.9 carat stone was discovered. Romaria is a larger town and municipality, but few major quarries were established that far upriver.
Several publications list Romaria as the name of a diamond district, but Romaria and Bagagem River valley both lie within the area that has long been included in the Coromandel diamond district (e.g., see Fig. 1 in Karfunkel et al., 1994), so this area is included in the Coromandel district here, with Romaria mine as a sublocality. The diamond occurrence at the Romaria mine is apparently in a debris flow conglomerate that is lithified, rather than in alluvium, and details on its geology are presented in the Romaria locality description. Fleischer (1998) mentioned that the conglomerate at Romaria extends to Iraí de Minas, which is also considered to be a sublocality of Bagagem River valley.
The discussion of geological circumstances of alluvial diamond occurrences in the locality description for Coromandel district applies to Bagagem River valley.
Geographic coordinates for significant quarries and clusters of quarries along Bagagem River, from Google Earth:
1) several quarries from 18° 51' 28", 47° 37' 51" to 18° 51' 8", 47° 39' 2"
2) 18° 42' 19", 47° 41' 51"
3) large area near Emborcação Reservoir in 18° 41' 14", 47° 41' 49".
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
Mineral list contains entries from the region specified including sub-localities19 valid minerals.
Detailed Mineral List:
| ⓘ Almandine Formula: Fe2+3Al2(SiO4)3 |
| ⓘ Anatase Formula: TiO2 |
| ⓘ Diamond Formula: C |
| ⓘ Epidote Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ Goethite Formula: Fe3+O(OH) |
| ⓘ Gorceixite Formula: BaAl3(PO4)(PO3OH)(OH)6 Description: Occurs abundantly as pebbles (favas) in the river. |
| ⓘ Grossular Formula: Ca3Al2(SiO4)3 |
| ⓘ Hematite Formula: Fe2O3 |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Kaolinite Formula: Al2(Si2O5)(OH)4 |
| ⓘ Kyanite Formula: Al2(SiO4)O |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ 'Monazite Group' Formula: REE(PO4) |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Illite Formula: K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| ⓘ Opal Formula: SiO2 · nH2O |
| ⓘ Perovskite Formula: CaTiO3 |
| ⓘ Pyrope Formula: Mg3Al2(SiO4)3 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Rutile Formula: TiO2 |
| ⓘ 'Tourmaline' Formula: AD3G6(T6O18)(BO3)3X3Z |
| ⓘ Zircon Formula: Zr(SiO4) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Diamond | 1.CB.10a | C |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Goethite | 4.00. | Fe3+O(OH) |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Perovskite | 4.CC.30 | CaTiO3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Opal | 4.DA.10 | SiO2 · nH2O |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| ⓘ | Anatase | 4.DD.05 | TiO2 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Gorceixite | 8.BL.10 | BaAl3(PO4)(PO3OH)(OH)6 |
| Group 9 - Silicates | |||
| ⓘ | Almandine | 9.AD.25 | Fe2+3Al2(SiO4)3 |
| ⓘ | Grossular | 9.AD.25 | Ca3Al2(SiO4)3 |
| ⓘ | Pyrope | 9.AD.25 | Mg3Al2(SiO4)3 |
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Kyanite | 9.AF.15 | Al2(SiO4)O |
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Muscovite var. Illite | 9.EC.15 | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| ⓘ | 9.EC.15 | KAl2(AlSi3O10)(OH)2 | |
| ⓘ | Kaolinite | 9.ED.05 | Al2(Si2O5)(OH)4 |
| Unclassified | |||
| ⓘ | 'Monazite Group' | - | REE(PO4) |
| ⓘ | 'Tourmaline' | - | AD3G6(T6O18)(BO3)3X3Z |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Goethite | Fe3+O(OH) |
| H | ⓘ Gorceixite | BaAl3(PO4)(PO3OH)(OH)6 |
| H | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| H | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Opal | SiO2 · nH2O |
| B | Boron | |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| C | Carbon | |
| C | ⓘ Diamond | C |
| O | Oxygen | |
| O | ⓘ Anatase | TiO2 |
| O | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Goethite | Fe3+O(OH) |
| O | ⓘ Gorceixite | BaAl3(PO4)(PO3OH)(OH)6 |
| O | ⓘ Grossular | Ca3Al2(SiO4)3 |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| O | ⓘ Kyanite | Al2(SiO4)O |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Monazite Group | REE(PO4) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Opal | SiO2 · nH2O |
| O | ⓘ Perovskite | CaTiO3 |
| O | ⓘ Pyrope | Mg3Al2(SiO4)3 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | ⓘ Zircon | Zr(SiO4) |
| Mg | Magnesium | |
| Mg | ⓘ Pyrope | Mg3Al2(SiO4)3 |
| Al | Aluminium | |
| Al | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Gorceixite | BaAl3(PO4)(PO3OH)(OH)6 |
| Al | ⓘ Grossular | Ca3Al2(SiO4)3 |
| Al | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Al | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Al | ⓘ Kyanite | Al2(SiO4)O |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Pyrope | Mg3Al2(SiO4)3 |
| Si | Silicon | |
| Si | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Grossular | Ca3Al2(SiO4)3 |
| Si | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Si | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Si | ⓘ Kyanite | Al2(SiO4)O |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Opal | SiO2 · nH2O |
| Si | ⓘ Pyrope | Mg3Al2(SiO4)3 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Zircon | Zr(SiO4) |
| P | Phosphorus | |
| P | ⓘ Gorceixite | BaAl3(PO4)(PO3OH)(OH)6 |
| P | ⓘ Monazite Group | REE(PO4) |
| K | Potassium | |
| K | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Grossular | Ca3Al2(SiO4)3 |
| Ca | ⓘ Perovskite | CaTiO3 |
| Ti | Titanium | |
| Ti | ⓘ Anatase | TiO2 |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Ti | ⓘ Perovskite | CaTiO3 |
| Ti | ⓘ Rutile | TiO2 |
| Fe | Iron | |
| Fe | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Goethite | Fe3+O(OH) |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Ba | Barium | |
| Ba | ⓘ Gorceixite | BaAl3(PO4)(PO3OH)(OH)6 |
Localities in this Region
- Minas Gerais
Other Regions, Features and Areas that Intersect
Brazil
- Minas Gerais
- Coromandel mining districtMining District
South AmericaContinent
South America PlateTectonic Plate
- Parana basinBasin
- Tocantins ProvinceOrogenic Belt
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
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
References
Sauer, Jules Roger (1982) Brazil - Paradise of Gemstones. Gemological Institute of America (GIA). 135 pp.p. 18, as "the Estrela do Sul region"





Bagagem River valley, Minas Gerais, Brazil