Santa Catharina meteorite, Morro do Rócio, São Francisco do Sul, Santa Catarina, Brazili
Regional Level Types | |
---|---|
Santa Catharina meteorite | Meteorite Fall Location |
Morro do Rócio | - not defined - |
São Francisco do Sul | Municipality |
Santa Catarina | State |
Brazil | Country |
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Latitude & Longitude (WGS84):
26° 13' South , 48° 36' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
São Francisco do Sul | 36,224 (2012) | 4.8km |
Joinville | 461,304 (2012) | 26.3km |
Guaratuba | 18,906 (2012) | 37.2km |
Barra Velha | 17,665 (2012) | 46.9km |
Guaramirim | 21,422 (2012) | 49.2km |
Mindat Locality ID:
2827
Long-form identifier:
mindat:1:2:2827:4
GUID (UUID V4):
42ddfc30-a4ac-4c19-954f-bb85cd1cdf9c
Iron Meteorite; Ataxite, Ni-rich (IAB-ung; D)
Found 1875; 7 tons [recognized and recovered].
Several weathered masses, the largest weighing 2,557 kg, were recovered on the island of São Francisco do Sul.
First believed to be a nickel ore, total mass recovered by humans may have been as much as 25,000 kg.
The meteorite is unusual in 3 important respects — it is
(1) unusually nickel rich (~30 wt% of unoxidised portions),
(2) unusually troilite-rich, and
(3) very severely weathered.
What remains of the original metallic structure is a complex polycrystalline network consisting of two or three varieties of Ni-rich metal plus minor kamacite. Schreibersite, troilite, and their multiple weathering products are ubiquitous companions. Indeed, one of these products, the secondary phosphate arupite, was first discovered in Santa Catharina fragments. In some cases, only a limonitic, but Ni-rich mass remains (the 'nickel ore'). At the other extreme, barringerite and schreibersite-enclosed fayalite are mineralogically unusual even for meteorites.
The municipality of São Francisco do Sul was initially named Nossa Senhora da Graça do Rio São Francisco do Sul. For this reason, in the older literature, the name Rio São Francisco is mentioned.
Note: Several sources (both online and offline) claim that "over 2,500 kg" of the original mass is kept in Brazil's National Museum in Rio de Janeiro. However, according to the National Museum itself, this is incorrect. The mass that was originally present weighs "about 2 kg". This error is probably due to a misinterpretation of the "decimal separator" in different languages.
In English, 2.500 means "two and a half", whereas 2,500 means "two thousand five hundred, see https://en.wikipedia.org/wiki/Decimal_separator
Note: In September 2018, the National Museum in Rio de Janeiro burned down and about 90% of its entire collection (of over 20 million specimens/artefacts) was lost. It is not known whether the Santa Catharina meteorite mass that had been present in the museum has survived the fire or not. For more information on the fire, see https://en.wikipedia.org/wiki/National_Museum_of_Brazil_fire
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
21 valid minerals. 1 (TL) - type locality of valid minerals. 1 erroneous literature entry.
Meteorite/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:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Iron | 1.AE.05 | Fe |
ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
ⓘ | Taenite | 1.AE.10 | (Fe,Ni) |
ⓘ | 'Antitaenite' | 1.AE.10 | Fe3Ni |
ⓘ | Tetrataenite | 1.AE.10 | FeNi |
ⓘ | Nickelphosphide | 1.BD.05 | (Ni,Fe)3P |
ⓘ | Schreibersite | 1.BD.05 | (Fe,Ni)3P |
ⓘ | Barringerite ? | 1.BD.10 | (Fe,Ni)2P |
ⓘ | Allabogdanite | 1.BD.15 | (Fe,Ni)2P |
ⓘ | Graphite ? | 1.CB.05a | C |
ⓘ | Sulphur | 1.CC.05 | S8 |
Group 2 - Sulphides and Sulfosalts | |||
ⓘ | Heazlewoodite | 2.BB.05 | Ni3S2 |
ⓘ | Pentlandite | 2.BB.15 | (NixFey)Σ9S8 |
ⓘ | Troilite | 2.CC.10 | FeS |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Goethite | 4.00. | α-Fe3+O(OH) |
ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
ⓘ | Hematite | 4.CB.05 | Fe2O3 |
ⓘ | Akaganeite | 4.DK.05 | (Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2O |
Group 5 - Nitrates and Carbonates | |||
ⓘ | Reevesite | 5.DA.50 | Ni6Fe3+2(OH)16(CO3) · 4H2O |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
ⓘ | Honessite | 7.DD.35 | (Ni1-xFe3+x)(OH)2[SO4]x/2 · nH2O |
Group 8 - Phosphates, Arsenates and Vanadates | |||
ⓘ | Sarcopside | 8.AB.15 | Fe2+3(PO4)2 |
ⓘ | Graftonite | 8.AB.20 | Fe2+Fe2+2(PO4)2 |
ⓘ | Arupite (TL) | 8.CE.40 | Ni3(PO4)2 · 8H2O |
Group 9 - Silicates | |||
ⓘ | Fayalite | 9.AC.05 | Fe2+2SiO4 |
Unclassified | |||
ⓘ | 'Limonite' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Akaganeite | (Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2O |
H | ⓘ Arupite | Ni3(PO4)2 · 8H2O |
H | ⓘ Goethite | α-Fe3+O(OH) |
H | ⓘ Honessite | (Ni1-xFex3+)(OH)2[SO4]x/2 · nH2O |
H | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
C | Carbon | |
C | ⓘ Graphite | C |
C | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
O | Oxygen | |
O | ⓘ Akaganeite | (Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2O |
O | ⓘ Arupite | Ni3(PO4)2 · 8H2O |
O | ⓘ Fayalite | Fe22+SiO4 |
O | ⓘ Goethite | α-Fe3+O(OH) |
O | ⓘ Graftonite | Fe2+Fe22+(PO4)2 |
O | ⓘ Hematite | Fe2O3 |
O | ⓘ Honessite | (Ni1-xFex3+)(OH)2[SO4]x/2 · nH2O |
O | ⓘ Magnetite | Fe2+Fe23+O4 |
O | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
O | ⓘ Sarcopside | Fe32+(PO4)2 |
Si | Silicon | |
Si | ⓘ Fayalite | Fe22+SiO4 |
P | Phosphorus | |
P | ⓘ Arupite | Ni3(PO4)2 · 8H2O |
P | ⓘ Barringerite | (Fe,Ni)2P |
P | ⓘ Graftonite | Fe2+Fe22+(PO4)2 |
P | ⓘ Sarcopside | Fe32+(PO4)2 |
P | ⓘ Schreibersite | (Fe,Ni)3P |
P | ⓘ Nickelphosphide | (Ni,Fe)3P |
P | ⓘ Allabogdanite | (Fe,Ni)2P |
S | Sulfur | |
S | ⓘ Heazlewoodite | Ni3S2 |
S | ⓘ Honessite | (Ni1-xFex3+)(OH)2[SO4]x/2 · nH2O |
S | ⓘ Pentlandite | (NixFey)Σ9S8 |
S | ⓘ Sulphur | S8 |
S | ⓘ Troilite | FeS |
Cl | Chlorine | |
Cl | ⓘ Akaganeite | (Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2O |
Fe | Iron | |
Fe | ⓘ Akaganeite | (Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2O |
Fe | ⓘ Barringerite | (Fe,Ni)2P |
Fe | ⓘ Fayalite | Fe22+SiO4 |
Fe | ⓘ Goethite | α-Fe3+O(OH) |
Fe | ⓘ Graftonite | Fe2+Fe22+(PO4)2 |
Fe | ⓘ Hematite | Fe2O3 |
Fe | ⓘ Honessite | (Ni1-xFex3+)(OH)2[SO4]x/2 · nH2O |
Fe | ⓘ Iron | Fe |
Fe | ⓘ Iron var. Kamacite | (Fe,Ni) |
Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
Fe | ⓘ Pentlandite | (NixFey)Σ9S8 |
Fe | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
Fe | ⓘ Sarcopside | Fe32+(PO4)2 |
Fe | ⓘ Schreibersite | (Fe,Ni)3P |
Fe | ⓘ Taenite | (Fe,Ni) |
Fe | ⓘ Tetrataenite | FeNi |
Fe | ⓘ Troilite | FeS |
Fe | ⓘ Antitaenite | Fe3Ni |
Fe | ⓘ Nickelphosphide | (Ni,Fe)3P |
Fe | ⓘ Allabogdanite | (Fe,Ni)2P |
Ni | Nickel | |
Ni | ⓘ Akaganeite | (Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2O |
Ni | ⓘ Arupite | Ni3(PO4)2 · 8H2O |
Ni | ⓘ Barringerite | (Fe,Ni)2P |
Ni | ⓘ Heazlewoodite | Ni3S2 |
Ni | ⓘ Honessite | (Ni1-xFex3+)(OH)2[SO4]x/2 · nH2O |
Ni | ⓘ Iron var. Kamacite | (Fe,Ni) |
Ni | ⓘ Pentlandite | (NixFey)Σ9S8 |
Ni | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
Ni | ⓘ Schreibersite | (Fe,Ni)3P |
Ni | ⓘ Taenite | (Fe,Ni) |
Ni | ⓘ Tetrataenite | FeNi |
Ni | ⓘ Antitaenite | Fe3Ni |
Ni | ⓘ Nickelphosphide | (Ni,Fe)3P |
Ni | ⓘ Allabogdanite | (Fe,Ni)2P |
Other Regions, Features and Areas containing this locality
South America PlateTectonic Plate
- Santos basinBasin
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References
Zhang, J., Williams, D. B., Goldstein, J. I., Clarke, R. S. (1990) Electron microscopy study of the iron meteorite Santa Catharina. Meteoritics, 25 (3) 167-175 doi:10.1111/j.1945-5100.1990.tb00992.x
Van Tassel, R., Dillen, H., Vochten, R., De Grave, E., Hertogen, J. (1992) Een meteoriet vanonder het stof gehaald.. [Dusting off a meteorite..]. Geonieuws, 17 (10) 201-211
Britvin, Sergey N., Shilovskikh, Vladimir V., Pagano, Renato, Vlasenko, Natalia S., Zaitsev, Anatoly N., Krzhizhanovskaya, Maria G., Lozhkin, Maksim S., Zolotarev, Andrey A., Gurzhiy, Vladislav V. (2019) Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P system. Scientific Reports, 9. doi:10.1038/s41598-018-37795-x