Eylettersite
About Eylettersite
Unique Identifiers
IMA Classification of Eylettersite
Classification of Eylettersite
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
L : With medium-sized and large cations, (OH, etc.):RO4 = 3:1
41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
5 : (AB)2(XO4)Zq
17 : Silicates Containing other Anions
6 : Silicates with phosphate
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Eyl | 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 Eylettersite
Optical Data of Eylettersite
Chemistry of Eylettersite
The type material contains minor Pb replacing Th, and minor Si replacing P.
Crystallography of Eylettersite
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 2.95 Å | (100) |
| 3.51 Å | (60) |
| 5.70 Å | (55) |
| 2.187 Å | (40) |
| 1.899 Å | (30) |
| 1.748 Å | (20) |
| 2.848 Å | (15) |
Type Occurrence of Eylettersite
National Museum of Natural History, Washington, D.C.,
USA, 136443
Synonyms of Eylettersite
Other Language Names for Eylettersite
Relationship of Eylettersite to other Species
| Arsenobenauite | SrFe3+3(AsO4)(AsO3OH)(OH)6 | Trig. 3m(32/m) : R3m |
| Benauite | SrFe3+3(PO4)(PO3OH)(OH)6 | Trig. 3m(32/m) : R3m |
| Crandallite | CaAl3(PO4)(PO3OH)(OH)6 | Trig. 3m(32/m) : R3m |
| Florencite-(Ce) | CeAl3(PO4)2(OH)6 | Trig. 3m(32/m) : R3m |
| Florencite-(La) | LaAl3(PO4)2(OH)6 | Trig. 3m(32/m) : R3m |
| Florencite-(Nd) | NdAl3(PO4)2(OH)6 | Trig. 3m(32/m) : R3m |
| Florencite-(Sm) | SmAl3(PO4)2(OH)6 | Trig. 3m(32/m) : R3m |
| Galloplumbogummite | Pb(Ga,Al,Ge)3(PO4)2(OH)6 | Trig. 3m : R3m |
| Gorceixite | BaAl3(PO4)(PO3OH)(OH)6 | Mon. m : Bm |
| Goyazite | SrAl3(PO4)(PO3OH)(OH)6 | Trig. 3m(32/m) : R3m |
| Kintoreite | PbFe3(PO4)(PO3OH)(OH)6 | Trig. 3m(32/m) : R3m |
| 'Kintoreite-2c' | PbFe3+3(PO4)2(OH,H2O)6 | |
| Plumbogummite | PbAl3(PO4)(PO3OH)(OH)6 | Trig. 3m(32/m) : R3m |
| Springcreekite | BaV3+3(PO4)2(OH,H2O)6 | Trig. 3m(32/m) : R3m |
| 'UM2006-23-PO:AlBiCaFeH' | (Ca,Bi)(Fe,Al)3(PO4)(PO3OH)(OH)6 | |
| 'Unnamed (As-analogue of Zaïrite)' | (Bi,Pb)Fe3+3(AsO4)2(OH)6 | |
| Waylandite | BiAl3(PO4)2(OH)6 | Trig. 3m(32/m) : R3m |
| Zaïrite | BiFe3+3(PO4)2(OH)6 | Trig. 3m(32/m) : R3m |
Common Associates
| 2 photos of Eylettersite associated with Mundite | Al(UO2)3(PO4)2(OH)3 · 5.5H2O |
| 2 photos of Eylettersite associated with Threadgoldite | Al(UO2)2(PO4)2(OH) · 8H2O |
| 2 photos of Eylettersite associated with Phuralumite | Al2[(UO2)3(PO4)2O(OH)](OH)3(H2O)9 |
| 1 photo of Eylettersite associated with Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| 1 photo of Eylettersite associated with Microcline | K(AlSi3O8) |
| 1 photo of Eylettersite associated with Quartz | SiO2 |
Related Minerals - Strunz-mindat Grouping
| 8.BL. | Kiryuite | NaMnAl(PO4)F3 |
| 8.BL. | Metaheimite | PbCu2(AsO4)(OH)3 |
| 8.BL. | Graulichite-(La) | LaFe3+3(AsO4)2(OH)6 |
| 8.BL. | Cloudite | BaFe3+3(PO4)(SO4)(OH)6 |
| 8.BL. | Oberwolfachite | SrFe3+3(AsO4)(SO4)(OH)6 |
| 8.BL. | Arsenobenauite | SrFe3+3(AsO4)(AsO3OH)(OH)6 |
| 8.BL.05 | Gallobeudantite | PbGa3(AsO4)(SO4)(OH)6 |
| 8.BL.05 | Slottaite | SrFe3+3(PO4)(SO4)(OH)6 |
| 8.BL.05 | Corkite | PbFe3+3(PO4)(SO4)(OH)6 |
| 8.BL.05 | Hidalgoite | PbAl3(AsO4)(SO4)(OH)6 |
| 8.BL.05 | Hinsdalite | PbAl3(PO4)(SO4)(OH)6 |
| 8.BL.05 | 'UM2011-07-POSO:AlBaH' | BaAl3(PO4)(SO4)(OH)6 |
| 8.BL.05 | Kemmlitzite | SrAl3(AsO4)(SO4)(OH)6 |
| 8.BL.05 | Beudantite | PbFe3+3(AsO4)(SO4)(OH)6 |
| 8.BL.05 | Weilerite | BaAl3(AsO4)(SO4)(OH)6 |
| 8.BL.05 | Woodhouseite | CaAl3(PO4)(SO4)(OH)6 |
| 8.BL.05 | Svanbergite | SrAl3(PO4)(SO4)(OH)6 |
| 8.BL.10 | Segnitite | PbFe3+3AsO4(AsO3OH)(OH)6 |
| 8.BL.10 | Arsenogoyazite | SrAl3(AsO4)(AsO3OH)(OH)6 |
| 8.BL.10 | Arsenogorceixite | BaAl3(AsO4)(AsO3OH)(OH)6 |
| 8.BL.10 | Dussertite | BaFe3+3(AsO4)(AsO3OH)(OH)6 |
| 8.BL.10 | Galloplumbogummite | Pb(Ga,Al,Ge)3(PO4)2(OH)6 |
| 8.BL.10 | Stibiosegnitite | Pb(Fe3+2.5Sb5+0.5)(AsO4)2(OH)6 |
| 8.BL.10 va | 'Viséite' | |
| 8.BL.10 | Arsenocrandallite | CaAl3(AsO4)(AsO3OH)(OH)6 |
| 8.BL.10 | Benauite | SrFe3+3(PO4)(PO3OH)(OH)6 |
| 8.BL.10 | Philipsbornite | PbAl3(AsO4)(AsO3OH)(OH)6 |
| 8.BL.10 | Crandallite | CaAl3(PO4)(PO3OH)(OH)6 |
| 8.BL.10 | Springcreekite | BaV3+3(PO4)2(OH,H2O)6 |
| 8.BL.10 | Kintoreite | PbFe3(PO4)(PO3OH)(OH)6 |
| 8.BL.10 | Plumbogummite | PbAl3(PO4)(PO3OH)(OH)6 |
| 8.BL.10 | Gorceixite | BaAl3(PO4)(PO3OH)(OH)6 |
| 8.BL.10 | Goyazite | SrAl3(PO4)(PO3OH)(OH)6 |
| 8.BL.13 | Florencite-(Ce) | CeAl3(PO4)2(OH)6 |
| 8.BL.13 | Florencite-(La) | LaAl3(PO4)2(OH)6 |
| 8.BL.13 | Florencite-(Nd) | NdAl3(PO4)2(OH)6 |
| 8.BL.13 | Zaïrite | BiFe3+3(PO4)2(OH)6 |
| 8.BL.13 | Arsenoflorencite-(La) | LaAl3(AsO4)2(OH)6 |
| 8.BL.13 | 'Arsenoflorencite-(Nd)' | NdAl3(AsO4)2(OH)6 |
| 8.BL.13 | 'Unnamed (As-analogue of Zaïrite)' | (Bi,Pb)Fe3+3(AsO4)2(OH)6 |
| 8.BL.13 | Arsenoflorencite-(Ce) | CeAl3(AsO4)2(OH)6 |
| 8.BL.13 | Graulichite-(Ce) | CeFe3+3(AsO4)2(OH)6 |
| 8.BL.13 | 'Arsenowaylandite' | BiAl3(AsO4)2(OH)6 |
| 8.BL.13 | Waylandite | BiAl3(PO4)2(OH)6 |
| 8.BL.13 | Florencite-(Sm) | SmAl3(PO4)2(OH)6 |
| 8.BL.15 | Viitaniemiite | Na(Ca,Mn2+)Al(PO4)(F,OH)3 |
| 8.BL.25 | Pattersonite | PbFe3+3(PO4)2(OH)5 · H2O |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 0.0000% | 0 | α, β, γ |
| Thorium (Th) | 31.8174% | 1,272,696 | 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 Eylettersite
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References for Eylettersite
Localities for Eylettersite
Showing 3 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.
Brazil | |
| Neumann et al. (2015) |
DR Congo (TL) | |
| Van Wambeke (1972) +1 other reference |
Namibia | |
| Schnaitmann et al. (2009) |




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The
Kobokobo pegmatite, Mwenga Territory, South Kivu, DR Congo