Cryptomelane
About Cryptomelane
Many manganese oxides are better identified using infra-red spectroscopy than by X-ray diffraction because of issues of crystal size, disorder, etc. (Potter and Rossman, 1979).
Unique Identifiers
IMA Classification of Cryptomelane
Classification of Cryptomelane
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
K : With large (+- medium-sized) cations; tunnel structures
7 : MULTIPLE OXIDES
9 : AB8X16
7 : Oxides and Hydroxides
2 : Oxides of the alkali metals
Mineral Symbols
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Cml | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| Cpt | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
| Cml | Warr (2020) | Warr, L.N. (2020) Recommended abbreviations for the names of clay minerals and associated phases. Clay Minerals, 55, 261–264 doi:10.1180/clm.2020.30 |
Physical Properties of Cryptomelane
Chemistry of Cryptomelane
Chemical Analysis
| 1 | |
|---|---|
| Mn2O3 | 81.0 % |
| Fe2O3 | 0.8 % |
| Al2O3 | 0.5 % |
| K2O | 3.3 % |
| Na2O | 0.8 % |
| H2O | 12.2 % |
| Total: | 98.6 % |
| ID | Locality | Reference | Notes |
|---|---|---|---|
| 1 | Lierneux, Liège, Wallonia, Belgium | Analysis by Pisani |
Crystallography of Cryptomelane
β = 90.95°
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) |
|---|---|---|---|---|---|---|---|
| 0016237 | Cryptomelane | Vicat J, Fanchon E, Strobel P, Tran Qui D (1986) The structure of K1.33Mn8O16 and cation ordering in hollandite-type structures _cod_database_code 1008322 Acta Crystallographica B42 162-167 | ![]() | 1986 | synthetic | 0 | 293 |
| 0009758 | Cryptomelane | Post J E, Von Dreele R B, Buseck P R (1982) Symmetry and cation displacements in hollandites: structure refinements of hollandite, cryptomelane and priderite Acta Crystallographica B38 1056-1065 | ![]() | 1982 | Chindwara, India | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 6.90 Å | (90) |
| 4.90 Å | (80) |
| 3.45 Å | (10) |
| 3.10 Å | (80) |
| 2.46 Å | (10) |
| 2.39 Å | (100) |
| 2.19 Å | (20) |
| 2.15 Å | (60) |
| 1.92 Å | (10) |
| 1.83 Å | (60) |
| 1.64 Å | (30) |
| 1.54 Å | (60) |
| 1.42 Å | (40) |
| 1.35 Å | (50) |
| 1.29 Å | (20) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| High-? alteration and/or metamorphism | |
| 32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits | |
| Stage 7: Great Oxidation Event | <2.4 |
| 47e : [Vanadates, chromates, manganates] | |
| 47h : [Near-surface oxidized, dehydrated minerals] |
Type Occurrence of Cryptomelane
Synonyms of Cryptomelane
Other Language Names for Cryptomelane
Varieties of Cryptomelane
| Thallium-bearing Cryptomelane | A thallium-bearing cryptomelane (0.23 at% Tl). Compare thalliomelane. Originally reported from Peach Springs District, Coconino Co., Arizona, USA. |
Relationship of Cryptomelane to other Species
| Coronadite | Pb(Mn4+6Mn3+2)O16 | Mon. 2/m |
| Ferricoronadite | Pb(Mn4+6Fe3+2)O16 | Tet. 4/m : I4/m |
| Ferrihollandite | Ba(Mn4+6Fe3+2)O16 | Mon. 2/m |
| Hollandite | Ba(Mn4+6Mn3+2)O16 | Mon. 2/m |
| Manjiroite | Na(Mn4+7Mn3+)O16 | Tet. 4/m : I4/m |
| Strontiomelane | Sr(Mn4+6Mn3+2)O16 | Mon. 2/m : P21/b |
| Thalliomelane | Tl(Mn4+7.5Cu2+0.5)O16 | Tet. 4/m : I4/m |
Common Associates
| 91 photos of Cryptomelane associated with Goethite | Fe3+O(OH) |
| 48 photos of Cryptomelane associated with Lepidocrocite | Fe3+O(OH) |
| 34 photos of Cryptomelane associated with Pyrolusite | Mn4+O2 |
| 31 photos of Cryptomelane associated with Hollandite | Ba(Mn4+6Mn3+2)O16 |
| 27 photos of Cryptomelane associated with Scholzite | CaZn2(PO4)2 · 2H2O |
| 25 photos of Cryptomelane associated with Malachite | Cu2(CO3)(OH)2 |
| 24 photos of Cryptomelane associated with Azurite | Cu3(CO3)2(OH)2 |
| 17 photos of Cryptomelane associated with 'Wad' | |
| 17 photos of Cryptomelane associated with Quartz | SiO2 |
| 13 photos of Cryptomelane associated with Aurorite | Mn2+Mn4+3O7 · 3H2O |
Related Minerals - Strunz-mindat Grouping
| 4.DK.K | Thalliomelane | Tl(Mn4+7.5Cu2+0.5)O16 |
| 4.DK. | Ferrihollandite | Ba(Mn4+6Fe3+2)O16 |
| 4.DK. | Kopernikite | K(Ti7Cr3+)O16 |
| 4.DK.4.DK. | Ferricoronadite | Pb(Mn4+6Fe3+2)O16 |
| 4.DK.05a | Manjiroite | Na(Mn4+7Mn3+)O16 |
| 4.DK.05b | Mannardite | Ba(Ti4+6V3+2)O16 |
| 4.DK.05b | Redledgeite | Ba(Ti4+6Cr3+2)O16 |
| 4.DK.05 | Akaganeite | (Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2O |
| 4.DK.05a | Coronadite | Pb(Mn4+6Mn3+2)O16 |
| 4.DK.05a | Hollandite | Ba(Mn4+6Mn3+2)O16 |
| 4.DK.05a | Strontiomelane | Sr(Mn4+6Mn3+2)O16 |
| 4.DK.05b | Henrymeyerite | Ba(Ti4+7Fe2+)O16 |
| 4.DK.05b | Priderite | K(Ti4+7Fe3+)O16 |
| 4.DK.10 | Romanèchite | (Ba,H2O)2(Mn4+,Mn3+)5O10 |
| 4.DK.10 | Todorokite | (Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O |
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) | 5.3224% | 1,650 | 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 Cryptomelane
Other Information
Internet Links for Cryptomelane
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References for Cryptomelane
Localities for Cryptomelane
Showing 758 localities.
Locality List
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- This locality has estimated coordinates.
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? - 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.






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The
Salisbury Mine, Salisbury, Litchfield County, Connecticut, USA