Goldichite
About Goldichite
Unique Identifiers
IMA Classification of Goldichite
Classification of Goldichite
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
C : Sulfates (selenates, etc.) without additional anions, with H2O
C : With medium-sized and large cations
29 : HYDRATED ACID AND NORMAL SULFATES
5 : AB(XO4)2·xH2O
25 : Sulphates
11 : Sulphates of Fe and other metals
Mineral Symbols
Symbol | Source | Reference |
---|---|---|
Gol | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Goldichite
On {100}
Optical Data of Goldichite
Based on recorded range of RI values above.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars.
Y= colorless to pale yellow
Z= very pale yellow
Chemistry of Goldichite
Crystallography of Goldichite
β = 101.68(7)°
{011}.
Crystallographic forms of Goldichite
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0000264 | Goldichite | Graeber E J, Rosenzweig A (1971) The crystal structures of yavapaiite, KFe(SO4)2, and goldichite, KFe(SO4)2.4H2O American Mineralogist 56 1917-1933 | ![]() | 1971 | 0 | 293 |
X-Ray Powder Diffraction
d-spacing | Intensity |
---|---|
3.068 Å | (100) |
7.35 Å | (90) |
10.29 Å | (80) |
6.85 Å | (70) |
4.00 Å | (60) |
3.403 Å | (60) |
2.656 Å | (60) |
Geological Environment
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 7: Great Oxidation Event | <2.4 |
45a : [Sulfates, arsenates, selenates, antimonates] | |
47a : [Near-surface hydration of prior minerals] | |
47b : [Sulfates and sulfites] | |
Stage 10b: Anthropogenic minerals | <10 Ka |
55 : Anthropogenic mine minerals |
Type Occurrence of Goldichite
Other Language Names for Goldichite
Common Associates
29 photos of Goldichite associated with Coquimbite | AlFe3(SO4)6(H2O)12 · 6H2O |
16 photos of Goldichite associated with Römerite | Fe2+Fe3+2(SO4)4 · 14H2O |
10 photos of Goldichite associated with Halotrichite | FeAl2(SO4)4 · 22H2O |
9 photos of Goldichite associated with Voltaite | K2Fe2+5Fe3+3Al(SO4)12 · 18H2O |
4 photos of Goldichite associated with Ferricopiapite | Fe3+0.67Fe3+4(SO4)6(OH)2 · 20H2O |
3 photos of Goldichite associated with Krausite | KFe(SO4)2 · H2O |
2 photos of Goldichite associated with Copiapite | Fe2+Fe3+4(SO4)6(OH)2 · 20H2O |
1 photo of Goldichite associated with Melanterite | Fe2+(H2O)6SO4 · H2O |
1 photo of Goldichite associated with Pickeringite | MgAl2(SO4)4 · 22H2O |
Related Minerals - Strunz-mindat Grouping
7.CC. | Cobaltoblödite | Na2Co(SO4)2 · 4H2O |
7.CC. | Andychristyite | PbCu2+Te6+O5(H2O) |
7.CC. | Ammoniovoltaite | (NH4)2Fe2+5Fe3+3Al(SO4)12(H2O)18 |
7.CC.05 | Krausite | KFe(SO4)2 · H2O |
7.CC.10 | Tamarugite | NaAl(SO4)2 · 6H2O |
7.CC.15 | Mendozite | NaAl(SO4)2 · 11H2O |
7.CC.15 | Kalinite | KAl(SO4)2 · 11H2O |
7.CC.20 | Alum-(Na) | NaAl(SO4)2 · 12H2O |
7.CC.20 | Lonecreekite | (NH4)Fe3+(SO4)2 · 12H2O |
7.CC.20 | Alum-(K) | KAl(SO4)2 · 12H2O |
7.CC.20 | Tschermigite | (NH4)Al(SO4)2 · 12H2O |
7.CC.20 | Lanmuchangite | Tl+Al(SO4)2 · 12H2O |
7.CC.25 | Zincovoltaite | K2Zn5Fe3+3Al(SO4)12 · 18H2O |
7.CC.25 | Voltaite | K2Fe2+5Fe3+3Al(SO4)12 · 18H2O |
7.CC.25 | Magnesiovoltaite | K2Mg5Fe3+3Al(SO4)12 · 18H2O |
7.CC.25 | Pertlikite | K2(Fe2+,Mg)2(Mg,Fe3+)4Fe3+2Al(SO4)12 · 18H2O |
7.CC.25 | Ammoniomagnesiovoltaite | (NH4)2Mg2+5Fe3+3Al(SO4)12 · 18H2O |
7.CC.30 | Kröhnkite | Na2Cu(SO4)2 · 2H2O |
7.CC.35 | Ferrinatrite | Na3Fe(SO4)3 · 3H2O |
7.CC.45 | Löweite | Na12Mg7(SO4)13 · 15H2O |
7.CC.50 | Nickelblödite | Na2Ni(SO4)2 · 4H2O |
7.CC.50 | Blödite | Na2Mg(SO4)2 · 4H2O |
7.CC.50 | Changoite | Na2Zn(SO4)2 · 4H2O |
7.CC.55 | Leonite | K2Mg(SO4)2 · 4H2O |
7.CC.55 | Mereiterite | K2Fe(SO4)2 · 4H2O |
7.CC.60 | Nickelpicromerite | K2Ni(SO4)2 · 6H2O |
7.CC.60 | Nickelboussingaultite | (NH4)2Ni(SO4)2 · 6H2O |
7.CC.60 | Katerinopoulosite | (NH4)2Zn(SO4)2 · 6H2O |
7.CC.60 | Picromerite | K2Mg(SO4)2 · 6H2O |
7.CC.60 | Cyanochroite | K2Cu(SO4)2 · 6H2O |
7.CC.60 | Mohrite | (NH4)2Fe(SO4)2 · 6H2O |
7.CC.60 | Boussingaultite | (NH4)2Mg(SO4)2 · 6H2O |
7.CC.65 | Polyhalite | K2Ca2Mg(SO4)4 · 2H2O |
7.CC.70 | Leightonite | K2Ca2Cu(SO4)4 · 2H2O |
7.CC.75 | Amarillite | NaFe(SO4)2 · 6H2O |
7.CC.80 | Konyaite | Na2Mg(SO4)2 · 5H2O |
7.CC.85 | Wattevilleite | Na2Ca(SO4)2 · 4H2O (?) |
7.CC.85 | Xocolatlite | Ca2Mn4+2(Te6+O6)2 · H2O |
7.CC.90 | Eckhardite | (Ca,Pb)Cu2+Te6+O5(H2O) |
Radioactivity
Element | % Content | Activity (Bq/kg) | Radiation Type |
---|---|---|---|
Uranium (U) | 0.0000% | 0 | α, β, γ |
Thorium (Th) | 0.0000% | 0 | α, β, γ |
Potassium (K) | 10.8870% | 3,375 | β, γ |
For comparison:
- Banana: ~15 Bq per fruit
- Granite: 1,000–3,000 Bq/kg
- EU exemption limit: 10,000 Bq/kg
Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.
Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!
Activity: –
Distance | Dose rate | Risk |
---|---|---|
1 cm | ||
10 cm | ||
1 m |
The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).
D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield
Other Information
Internet Links for Goldichite
Please feel free to link to this page.
References for Goldichite
Localities for Goldichite
Locality List




All localities listed without proper references should be considered as questionable.
Argentina | |
| rruff.geo.arizona.edu (n.d.) +1 other reference |
Canada | |
| Schindler et al. (2012) |
Caribbean Netherlands | |
Anthony et al. (2016) | |
Chile | |
| Samples analysed by Tony Kampf of LAC ... |
| Peter G. Seroka collection |
China | |
| Cai et al. (2009) |
Greece | |
| Rieck (n.d.) |
| Kolitsch et al. (2014) |
Rieck (n.d.) | |
| Rieck (n.d.) |
Italy | |
| De Michele (1974) |
| Biagioni et al. (2019) +1 other reference |
Peru | |
| Roth et al. (2012) |
Portugal | |
| Flahaut et al. (2018, September) |
Russia | |
| maurice.strahlen.org (2004) |
USA | |
| Bullock (1981) |
| Rosenzweig et al. (1955) +1 other reference |
Javier Mine, Huac-huas District, Lucanas Province, Ayacucho, Peru