Iowaite (original) (raw)
A valid IMA mineral species
About IowaiteHide
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Formula:
Mg6Fe3+2(OH)16Cl2 · 4H2O
Name:
For the state of the type locality.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:2038:7
eed77052-7ca7-4f15-9638-4e1d295fe87b
IMA Classification of IowaiteHide
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Type description reference:
Classification of IowaiteHide
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4.FL.05
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
F : Hydroxides (without V or U)
L : Hydroxides with H2O +- (OH); sheets of edge-sharing octahedra
6.4.5.1
6 : HYDROXIDES AND OXIDES CONTAINING HYDROXYL
4 : Miscellaneous
8.11.8
8 : Halides - Fluorides, Chlorides, Bromides and Iodides; also Fluoborates and Fluosilicates
11 : Halides of Fe and Ni
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Iow | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Iow | 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 IowaiteHide
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Cleavage:
Perfect
Perfect basal cleavage
Density:
2.11(2) g/cm3 (Measured)
Optical Data of IowaiteHide
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RI values:
_n_ω = 1.543 - 1.561 _n_ε = 1.533 - 1.543
δ = 0.010 - 0.018
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Chemistry of IowaiteHide
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Mindat Formula:
Mg6Fe3+2(OH)16Cl2 · 4H2O
Crystallography of IowaiteHide
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Class (H-M):
3_m_ _(_32/m ) - Hexagonal Scalenohedral
Cell Parameters:
a = 3.1077(9) Å, c = 23.885(13) Å
Comment:
updated cell parameters from Zhitova et al. (2023); formerly here: a=3.119(5), c=24.25(2) (also from a powder diffraction data)
Crystal StructureHide
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X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
8.109 Å | (100) |
4.047 Å | (40) |
2.363 Å | (27) |
2.019 Å | (23) |
2.639 Å | (17) |
1.530 Å | (13) |
1.560 Å | (8) |
Comments:
Sioux Co., Iowa, USA. Data from the type description. The type specimen was remeasured about 27 years later (Braithwaite 1994) and a shift in the data was measured, likely due to dehydration.
Geological EnvironmentHide
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Type Occurrence of IowaiteHide
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General Appearance of Type Material:
Platy crystals 2-3mm in size
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, 121706.
Geological Setting of Type Material:
Altered serpentinite in precambrian basement
Reference:
Kohls, D.W., Rodda,, J.L. (1967) Iowaite, a new hydrous magnesium hydroxide-ferric oxychloride from the Precambrian of Iowa. American Mineralogist: 52: 1261-1271.
Synonyms of IowaiteHide
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Other Language Names for IowaiteHide
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Varieties of IowaiteHide
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Relationship of Iowaite to other SpeciesHide
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Other Members of this group:
Desautelsite | Mg6Mn3+2(OH)16[CO3] · 4H2O | Trig. 3_m_ _(_32/m ) |
---|---|---|
Droninoite | Ni6Fe3+2(OH)16Cl2 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Hydrotalcite | Mg6Al2(CO3)(OH)16 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Hydrotalcite-3R | Mg6Al2(CO3)(OH)16 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Kaznakhtite | Ni6Co3+2(CO3)(OH)16 · 4H2O | Trig. 3 : _R_3 |
Meixnerite | Mg6Al2(OH)16(OH)2 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Pyroaurite | Mg6Fe3+2(OH)16[CO3] · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Reevesite | Ni6Fe3+2(OH)16(CO3) · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Stichtite | Mg6Cr3+2(OH)16[CO3] · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Takovite | Ni6Al2(OH)16[CO3] · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
UM2002-02-COH:FeNi | (Fe2+,Ni)6Fe3+2(CO3)(OH)16 · 4H2O | |
Woodallite | Mg6Cr2(OH)16Cl2 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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4.FL. | Trébeurdenite | Fe2+2Fe3+4O2(OH)10CO3 · 3H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
---|---|---|---|
4.FL. | Mariakrite | [Ca4Al2(OH)12(H2O)4][Fe2S4] | Tric. 1 : _P_1 |
4.FL.05 | Muskoxite | Mg7Fe4O13 · 10H2O | Trig. 3_m_ _(_32/m ) |
4.FL.05 | Jamborite | Ni2+1-xCo3+x(OH)2-x(SO4)x · nH2O | Trig. 3_m_ _(_32/m ) : R_3_m |
4.FL.05 | Mössbauerite | Fe3+6O4(OH)8[CO3] · 3H2O | Trig. 3 |
4.FL.05 | Meixnerite | Mg6Al2(OH)16(OH)2 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
4.FL.05 | Woodallite | Mg6Cr2(OH)16Cl2 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
4.FL.05 | Fougèrite | Fe2+4Fe3+2(OH)12[CO3] · 3H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
4.FL.05 | Dritsite | Li2Al4(OH)12Cl2 · 3H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m c m |
4.FL.05 | Rotemite | Ca4Cr2(OH)12Cl2 · 4H2O | Trig. 3_m_ _(_32/m ) : R_3_c |
4.FL.10 | Hydrocalumite | Ca4Al2(OH)12(Cl,CO3,OH)2 · 4H2O | Mon. 2 : _P_21 |
4.FL.15 | Kuzelite | Ca4Al2(OH)12[SO4] · 6H2O | Trig. |
4.FL.20 | Jianshuiite | (Mg,Mn,Ca)Mn3O7 · 3H2O | Trig. 3 : _R_3 |
4.FL.20 | Ernienickelite | NiMn3O7 · 3H2O | Trig. 3 : _R_3 |
4.FL.20 | Aurorite | Mn2+Mn4+3O7 · 3H2O | Trig. 3 : _R_3 |
4.FL.20 | Chalcophanite | ZnMn4+3O7 · 3H2O | Trig. 3 : _R_3 |
4.FL.25 | Woodruffite | Zn2+x/2(Mn4+1-xMn3+x)O2 · yH2O | Mon. 2/m : _B_2/m |
4.FL.30 | Asbolane | (Ni,Co)2-xMn4+(O,OH)4 · nH2O | Hex. |
4.FL.30 va | Lampadite | Cu, Mn, O, H | |
4.FL.35 | Buserite | Na4Mn14O27 · 21H2O | |
4.FL.40 | Takanelite | (Mn,Ca)Mn4O9 · H2O | Hex. |
4.FL.40 | Ranciéite | (Ca,Mn2+)0.2(Mn4+,Mn3+)O2 · 0.6H2O | Trig. 3 : _P_3 |
4.FL.45 | Birnessite | (Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O | Mon. 2/m : _B_2/m |
4.FL.55 | Cianciulliite | Mn(Mg,Mn)2Zn2(OH)10 · 2-4H2O | Mon. 2/m : _B_2/m |
4.FL.60 | Jensenite | Cu3[TeO6] · 2H2O | Mon. 2/m : _P_21/m |
4.FL.65 | Leisingite | Cu2MgTe6+O6 · 6H2O | Trig. 3 : _P_3 |
4.FL.70 | Akdalaite | Al10O14(OH)2 | Hex. |
4.FL.75 | Cafetite | CaTi2O5 · H2O | Mon. 2/m : _P_21/b |
4.FL.80 | Mourite | UMo5O12(OH)10 | Mon. |
4.FL.85 | Deloryite | Cu4(UO2)(MoO4)2(OH)6 | Mon. 2/m : _B_2/m |
4.FL.90 | Lagalyite | Ca2xMn1-xO2 · 1.5-2H2O | Mon. |
4.FL.95 | Tunnerite (of Cornu) | ||
4.FL.100 | Carbocalumite | Ca4Al2(OH)12(CO3) · 6H2O | Trig. 3_m_ _(_32/m ) : R_3_c |
4.FL.100 | Mampsisite | Ca4Al2(CO3)(OH)12 · 5H2O | Tric. |
Other InformationHide
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Thermal Behaviour:
In DTA measurements, a large endothermic reaction occurs between 315°C and 350°C, representing a collapse of the iowaite structure. The material changes in color from light tan to dark brown, water is evolved, and periclase is formed.
Notes:
Insoluble in water and readily soluble in mineral acids.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for IowaiteHide
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References for IowaiteHide
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Reference List:
Mills, S. J., Christy, A. G., Génin, J.-M. R., Kameda, T., Colombo, F. (2012) Nomenclature of the hydrotalcite supergroup: natural layered double hydroxides. Mineralogical Magazine, 76 (5) 1289-1336 doi:10.1180/minmag.2012.076.5.10
Zhitova, Elena S., Chukanov, Nikita V., Pekov, Igor V., Zolotarev, Andrey A., Shilovskikh, Vladimir V., Bocharov, Vladimir N. (2023) Crystal chemistry of iowaite, Mg6FeIII2(OH)16Cl2 × 4H2O, a natural layered double hydroxide. Applied Clay Science, 243. 107070 doi:10.1016/j.clay.2023.107070
Localities for IowaiteHide
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This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The
symbol next to localities in the list can be used to jump to that position on the map.
Locality ListHide
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- 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).
Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.