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Holdawayite

A valid IMA mineral species
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About HoldawayiteHide

Formula:
Mn6(CO3)2(OH)7(Cl,OH)
Colour:
Light to bright pink
Lustre:
Vitreous
Hardness:
3
Specific Gravity:
3.19
Crystal System:
Monoclinic
Name:
Named in honor of Michael Jon Holdaway (b. 1936, d. March 21, 2025), professor of petrology and Southern Methodist University, Dallas, Texas, USA, for his contributions to mineralogy ind petrology and for his efforts as editor of the American Mineralogist.
This page provides mineralogical data about Holdawayite.


Unique IdentifiersHide

Mindat ID:
1919
Long-form identifier:
mindat:1:1:1919:0

IMA Classification of HoldawayiteHide

Classification of HoldawayiteHide

5.BA.20

5 : CARBONATES (NITRATES)
B : Carbonates with additional anions, without H2O
A : With Cu, Co, Ni, Zn, Mg, Mn
16b.4.2.2

16b : HYDRATED CARBONATES CONTAINING HYDROXYL OR HALOGEN
4 : AmBn(XO3)pZqxH2O & with (m+n):p = 3:1
11.12.2

11 : Carbonates
12 : Carbonates of Mn

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
HdwIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of HoldawayiteHide

Vitreous
Transparency:
Translucent
Colour:
Light to bright pink
Comment:
It gradually changes to a brown color on exposure and in some cases has developed a thin black sooty coating that masks the true color
Streak:
Light pink
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
{100}
Density:
3.19(4) g/cm3 (Measured)    3.24 g/cm3 (Calculated)

Optical Data of HoldawayiteHide

Type:
Biaxial (-)
RI values:
nα = 1.644(1) nβ = 1.719(1) nγ = 1.721(1)
2V:
Measured: 12° to 18°, Calculated: 16°
Max. Birefringence:
δ = 0.077
Based on recorded range of RI values above.

Interference Colours:
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. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
relatively strong
Optical Extinction:
X = b; Z ∧ c = 45(3)° in the obtuse angle of beta.
Pleochroism:
Non-pleochroic

Chemistry of HoldawayiteHide

Mindat Formula:
Mn6(CO3)2(OH)7(Cl,OH)
Element Weights:
Element% weight
Mn54.561 %
O34.427 %
Cl5.868 %
C3.976 %
H1.168 %

Calculated from ideal end-member formula.
Mn
O
Cl
C
H

Crystallography of HoldawayiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 23.437(5) Å, b = 3.3137(3) Å, c = 16.618(6) Å
β = 111.15(2)°
Ratio:
a:b:c = 7.073 : 1 : 5.015
Unit Cell V:
1,203.67 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Granular aggregates or massive. Fibrous, elongated along [001].

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0001165HoldawayitePeacor D R, Rouse R C (1988) Holdawayite, Mn6(CO3)2(OH)7(Cl,OH), a structure containing anions in zeolite-like channels American Mineralogist 73 637-64219880293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.93 Å(100)
7.77 Å(40)
5.459 Å(80)
3.879 Å(70)
2.926 Å(40)
2.690 Å(60b)
2.589 Å(50b)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)
High-? alteration and/or metamorphism
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Type Occurrence of HoldawayiteHide

General Appearance of Type Material:
Subhedral crystals approximately 2 cm in diameter.
Place of Conservation of Type Material:
Canadian Museum of Nature, Ottawa, Ontario, Canada, numbers 51510, 51511.
National Museum of Natural History, Washington, D.C., USA, number 163209.
Geological Setting of Type Material:
Tectonically intercalated manganese and iron ores, which are locally dominated by carbonate- and silicate-facies rocks rather than by the more usual hausmannite ores.
Associated Minerals at Type Locality:

Synonyms of HoldawayiteHide

Other Language Names for HoldawayiteHide

Common AssociatesHide

Associations Based on Photo Data:
4 photos of Holdawayite associated with AllactiteMn2+7(AsO4)2(OH)8

Related Minerals - Strunz-mindat GroupingHide

5.BA.05AzuriteCu3(CO3)2(OH)2Mon. 2/m : P21/b
5.BA.10Mcguinnessite(Mg,Cu)2(CO3)(OH)2Mon. 2/m
5.BA.10Zincrosasite(Zn,Cu)2(CO3)(OH)2Mon.
5.BA.10ParádsasváriteZn2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.10Rosasite(Cu,Zn)2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.10NullaginiteNi2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.10Georgeite[Cu(OH)2-x(H2O)x][CO3]x/2Amor.
5.BA.10Glaukosphaerite(Cu,Ni)2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.10PokrovskiteMg2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.10KolweziteCuCo(CO3)(OH)2Tric.
5.BA.10ChukanoviteFe2+2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.10MalachiteCu2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.10PerchiazziiteCo2(CO3)(OH)2Mon. 2/m : P21/b
5.BA.15Aurichalcite(Zn,Cu)5(CO3)2(OH)6Mon. 2/m : P21/m
5.BA.15HydrozinciteZn5(CO3)2(OH)6Mon. 2/m : B2/m
5.BA.25'UM1977-03-COSiO:CaClH'Ca10-11(CO3)7(SiO4)Cl1-2(OH)1-2Mon.
5.BA.25DeferniteCa6(CO3)1.58(Si2O7)0.21(OH)7[Cl0.50(OH)0.08(H2O)0.42]Orth. mmm(2/m2/m2/m) : Pnma
5.BA.30SclariteZn7(CO3)2(OH)10Mon. 2/m : B2/b
5.BA.30Loseyite(Mn2+,Zn,Mg)4Zn3(CO3)2(OH)10Mon. 2/m

Fluorescence of HoldawayiteHide

Other InformationHide

Notes:
Effervesces weakly in dilute HCl. It is stained light pink with an alizain-red-dilute HCl mixture.
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 HoldawayiteHide

References for HoldawayiteHide

Localities for HoldawayiteHide

Showing 4 localities.

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.
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Locality ListHide

- 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.
Germany
 
  • Rhineland-Palatinate
    • Rhein-Lahn-Kreis
Wittern (2001)
      • Lahnstein
        • Friedrichssegen
Der Aufschluss Vol.55
Namibia (TL)
 
  • Otjozondjupa Region
    • Otavi Constituency
      • Kombat
Peacor et al. (1988)
Romania
 
  • Maramureș County
    • Târgu Lăpuș
Udubasa et al. (1996) +2 other references
 
and/or  
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