Billietite
About Billietite
Billiet was in the resistance during WWII but was arrested and placed in a concentration camp.
Billiet died on May 3 1945 when the transport ship SS Cap Arcona, which was housing prisoners from the Nazi Neuengamme concentration camp, was sunk by Allied Forces in the Bay of Lübeck.
Unique Identifiers
Similar Names
| Bellidoite | A valid IMA mineral species | Cu2Se |
IMA Classification of Billietite
Classification of Billietite
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
G : Uranyl Hydroxides
B : With additional cations (K, Ca, Ba, Pb, etc.); with mainly UO2(O,OH)5 pentagonal polyhedra
5 : OXIDES CONTAINING URANIUM OR THORIUM
7 : AX6O19·xH2O
7 : Oxides and Hydroxides
16 : Oxides of U
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Bil | 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 Billietite
on {001}, imperfect on {110} and {010}
Optical Data of Billietite
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.
Orientation: X = c, Y = a, Z = b
Chemistry of Billietite
Crystallography of Billietite
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Big Balls | Small Balls | Just Balls | Spacefill
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| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0006120 | Billietite | Finch R J, Burns P C, Hawthorne F C, Ewing R C (2006) Refinement of the crystal structure of billietite, Ba [(UO2)6 O4 (OH)6] (H2O)8 The Canadian Mineralogist 44 1197-1205 | ![]() | 2006 | Shaba, Democratic Republic of Congo | 0 | 293 |
| 0001133 | Billietite | Pagoaga M K, Appleman D E, Stewart J M (1987) Crystal structures and crystal chemistry of the uranyl oxide hydrates becquerelite, billietite, and protasite match those published American Mineralogist 72 1230-1238 | ![]() | 1987 | Shinkolobwe mine, Shaba, Zaire | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 7.53 Å | (10) |
| 3.77 Å | (9) |
| 3.17 Å | (8) |
| 2.03 Å | (6) |
| 3.54 Å | (5) |
| 2.49 Å | (4) |
| 2.56 Å | (3) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47f : [Uranyl (U⁶⁺) minerals] |
Type Occurrence of Billietite
National Museum of Natural History, Washington, D.C., USA (No. 160496)
Other Language Names for Billietite
Common Associates
| 32 photos of Billietite associated with Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
| 15 photos of Billietite associated with Rutherfordine | (UO2)CO3 |
| 10 photos of Billietite associated with Uraninite | UO2 |
| 9 photos of Billietite associated with Becquerelite | Ca(UO2)6O4(OH)6 · 8H2O |
| 9 photos of Billietite associated with Cuprosklodowskite | Cu(UO2)2(SiO3OH)2 · 6H2O |
| 8 photos of Billietite associated with Vandenbrandeite | Cu(UO2)(OH)4 |
| 7 photos of Billietite associated with Malachite | Cu2(CO3)(OH)2 |
| 5 photos of Billietite associated with Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| 4 photos of Billietite associated with Sklodowskite | Mg(UO2)2(SiO3OH)2 · 6H2O |
| 4 photos of Billietite associated with Roubaultite | Cu2(UO2)3(CO3)2O2(OH)2 · 4H2O |
Related Minerals - Strunz-mindat Grouping
| 4.GB.05 | Rameauite | K2Ca(UO2)6O6(OH)4 · 6H2O |
| 4.GB.05 | Agrinierite | K2(Ca,Sr)[(UO2)3O3(OH)2]2 · 5H2O |
| 4.GB.05 | Compreignacite | K2(UO2)6O4(OH)6 · 7H2O |
| 4.GB.10 | Becquerelite | Ca(UO2)6O4(OH)6 · 8H2O |
| 4.GB.10 | Protasite | Ba(UO2)3O3(OH)2 · 3H2O |
| 4.GB.15 | Richetite | (Fe3+,Mg)Pb 8.6(UO2)36O36(OH)24 · 41H2O |
| 4.GB.20 | Calciouranoite | (Ca,Ba,Pb)U2O7 · 5H2O |
| 4.GB.20 | Bauranoite | Ba(UO2)2(OH)6 · 1-2H2O |
| 4.GB.20 | Metacalciouranoite | (Ca,Ba,Pb,K2)U2O7 · 2H2O |
| 4.GB.25 | Fourmarierite | Pb(UO2)4O3(OH)4 · 4H2O |
| 4.GB.30 | Wölsendorfite | Pb7(UO2)14O19(OH)4 · 12H2O |
| 4.GB.35 | Masuyite | Pb(UO2)3O3(OH)2 · 3H2O |
| 4.GB.40 | Vandendriesscheite | PbU7O22 · 12H2O |
| 4.GB.40 | Metavandendriesscheite | PbU7O22 · nH2O n < 12 |
| 4.GB.45 | Vandenbrandeite | Cu(UO2)(OH)4 |
| 4.GB.50 | Sayrite | Pb2(UO2)5O6(OH)2 · 4H2O |
| 4.GB.55 | Curite | Pb3(H2O)2[(UO2)4O4(OH)3]2 |
| 4.GB.60 | Iriginite | (UO2)Mo2O7 · 3H2O |
| 4.GB.65 | Uranosphaerite | Bi(UO2)O2(OH) |
| 4.GB.70 | Holfertite | CaxU6+2-xTi(O8-xOH4x) · 3H2O |
| 4.GB.75 | Carlosbarbosaite | (UO2)2Nb2O6(OH)2 · 2H2O |
| 4.GB.80 | Gauthierite | KPb[(UO2)7O5(OH)7] · 8H2O |
| 4.GB.85 | Kroupaite | KPb0.5[(UO2)8O4(OH)10] · 10H2O |
| 4.GB.90 | Leesite | K(H2O)2[(UO2)4O2(OH)5] · 3H2O |
| 4.GB.95 | Shinkolobweite | Pb1.333[U5+O(OH)(UO2)5O4.67(OH)5.33](H2O)5 |
| 4.GB.95 | Nollmotzite | Mg[U5+(U6+O2)2O4F3] · 4H2O |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 71.5663% | 17,891,575 | α, β, γ |
| Thorium (Th) | 0.0000% | 0 | α, β, γ |
| Potassium (K) | 0.0000% | 0 | 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 Billietite
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References for Billietite
Localities for Billietite
Showing 44 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
All localities listed without proper references should be considered as questionable.
Australia | |
| Brugger et al. (2003) +1 other reference |
Brazil | |
| Pires et al. (2014) |
China | |
| Dahlkamp (2009) |
Czech Republic | |
| Pauliš P. et al. (Kutna Hora, issue 1) |
| Collected by Jan Hloušek +2 other references |
| Pauliš P. et al. (Kutna Hora, issue 1) |
| Pauliš P. et al. (Kutna Hora, issue 1) |
DR Congo (TL) | |
| 304 [278]. +5 other references |
| KMMA | |
| KMMA +1 other reference |
| Thorne (n.d.) +1 other reference |
| Anthony (1997) +1 other reference |
France | |
| Meisser (2012) |
| Denis Vernet - personnal |
| OLLIC Pascal Collection +1 other reference |
| - (1998) |
| - (1998) +1 other reference | |
| - (1998) |
| Haas (n.d.) |
| Anthony (1997) |
| "minéraux uranifères +2 other references |
| Bariand et al. (1993) +2 other references |
Germany | |
| Kolitsch (1997) +1 other reference |
| |
| |
| |
| Walenta (1992) |
| Collection Elmar Lackner |
| Anthony (1997) +1 other reference | |
| N. Jb. Miner. Abh. 115 (1971) |
| Schnorrer-Köhler (1991) +1 other reference |
Italy | |
| Ciriotti et al. (2010) |
| Campostrini I. (2013) |
| Campostrini et al. (2006) |
Peru | |
| Li (2016) |
Spain | |
| Abella et al. (2009) |
Sweden | |
| |
Switzerland | |
| |
| Stalder et al. (1998) |
| Meisser (2012) | |
| Wulser P.A. et al. 2005 |
USA | |
| Lapham et al. (1976) |
| Anthony (1997) |
| Min News 16:1 p1 |






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The
Shinkolobwe Mine, Shinkolobwe, Kambove Territory, Haut-Katanga, DR Congo