Chlormanganokalite
About Chlormanganokalite
Unique Identifiers
IMA Classification of Chlormanganokalite
Classification of Chlormanganokalite
3 : HALIDES
C : Complex halides
J : With MX6 complexes; M = Fe, Mn, Cu
11 : HALIDE COMPLEXES
5 : AmBX6
8 : Halides - Fluorides, Chlorides, Bromides and Iodides; also Fluoborates and Fluosilicates
10 : Halides of Mn
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Cmk | 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 Chlormanganokalite
Optical Data of Chlormanganokalite
Relative to Canada balsam mounting medium (n ≈ 1.537).
For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Chemistry of Chlormanganokalite
Crystallography of Chlormanganokalite
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
CIF File Best | x | y | z | a | b | c
Stop | Start
Console Off | On | Grey | Yellow
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0019234 | Chlormanganokalite | Bellanca A (1947) La struttura della cloromanganocalite Periodico di Mineralogia 16 73-88 | 1947 | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 2.55 Å | (100) |
| 2.69 Å | (80) |
| 5.90 Å | (50) |
| 3.55 Å | (50) |
| 2.82 Å | (28) |
| 3.45 Å | (24) |
| 2.50 Å | (24) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 45b : [Other oxidized fumarolic minerals] | |
| Stage 10b: Anthropogenic minerals | <10 Ka |
| 54 : Coal and other mine fire minerals (see also #51 and #56) |
Type Occurrence of Chlormanganokalite
Synonyms of Chlormanganokalite
Other Language Names for Chlormanganokalite
Relationship of Chlormanganokalite to other Species
| Rinneite | K3Na[FeCl6] | Trig. 3m(32/m) : R3c |
| Saltonseaite | K3NaMnCl6 | Trig. 3m(32/m) : R3c |
Related Minerals - Strunz-mindat Grouping
| 3.CJ.05 | Rinneite | K3Na[FeCl6] |
| 3.CJ.05 | Saltonseaite | K3NaMnCl6 |
| 3.CJ.10 | Erythrosiderite | K2[Fe3+Cl5(H2O)] |
| 3.CJ.10 | Kremersite | (NH4,K)2[Fe3+Cl5(H2O)] |
| 3.CJ.15 | Mitscherlichite | K2CuCl4 · 2H2O |
| 3.CJ.20 | Douglasite | K2[Fe2+Cl4(OH2)2] |
| 3.CJ.25 | 'Redikortsevite' | (NH4)MgCl3 · 6H2O |
| 3.CJ.30 | Zirklerite | (Fe,Mg,Ca)9Al4Cl18(OH)12 · 14H2O (?) |
| 3.CJ.30 | Kalithallite | K3Tl3+Cl6 · 2H2O |
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) | 36.8809% | 11,433 | 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
Fluorescence of Chlormanganokalite
Other Information
Internet Links for Chlormanganokalite
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References for Chlormanganokalite
Localities for Chlormanganokalite
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.
Italy (TL) | |
| Nature (1906) +2 other references |
| Pelloux (1927) +2 other references | |
Poland | |
| Ł. Kruszewski (PXRD data) |

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The
Vesuvius fumaroles, Metropolitan City of Naples, Campania, Italy