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Gladiusite

A valid IMA mineral species
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About GladiusiteHide

Formula:
Fe2(Fe,Mg)4(PO4)(OH)11(H2O)
Colour:
Dark green, almost black; red-brown, brownish
Lustre:
Vitreous
Hardness:
4 - 4½
Specific Gravity:
3.11
Crystal System:
Monoclinic
Name:
For the crystal morphology (resembling a double-edged sword (gladius, Latin for sword)).
Note: Gladiusite contains both Fe3+ and Fe2+ in the (ideal) ratio of 2:1. The colour of the type material is described as "dark green, almost black". The red-brown, brownish colour of most of the material shown in the photos here suggests that some or all of the Fe2+ might be oxidised, which might correspond to a new species (comment by Uwe Kolitsch, May 2021).


Unique IdentifiersHide

Mindat ID:
11032
Long-form identifier:
mindat:1:1:11032:1

Similar NamesHide

IMA Classification of GladiusiteHide

Classification of GladiusiteHide

8.DF.40

8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
F : With only medium-sized cations, (OH,etc.):RO4 > 3:1

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

Physical Properties of GladiusiteHide

Vitreous
Transparency:
Translucent
Colour:
Dark green, almost black; red-brown, brownish
Streak:
Olive-green (in 10-12 hours, changes to brownish red)
Hardness:
4 - 4½ on Mohs scale
Hardness:
VHN20=300(20) kg/mm2 - Vickers
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
None observed
Fracture:
Irregular/Uneven
Density:
3.11(2) g/cm3 (Measured)    3.08 g/cm3 (Calculated)

Optical Data of GladiusiteHide

Type:
Biaxial (-)
RI values:
nα = 1.722 nβ = 1.73 nγ = 1.737
Max. Birefringence:
δ = 0.015
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:
Moderate
Dispersion:
r > v
Pleochroism:
Strong
Comments:
X = olive-green, Y = grayish blue, Z = dark green with a blue tint
Comments:
Absorption: X > Y > Z.

Chemistry of GladiusiteHide

Mindat Formula:
Fe2(Fe,Mg)4(PO4)(OH)11(H2O)
Element Weights:
Element% weight
Fe52.756 %
O40.305 %
P4.877 %
H2.063 %

Calculated from ideal end-member formula.

Crystallography of GladiusiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Cell Parameters:
a = 16.950(2) Å, b = 11.650(1) Å, c = 6.2660(6) Å
β = 90.000(4)°
Ratio:
a:b:c = 1.455 : 1 : 0.538
Unit Cell V:
1,237.33 ų (Calculated from Unit Cell)
Z:
4
Twinning:
Extensive, pseudo-orthorhombic revealed by structure analysis.
Comment:
Space group P21/n, pseudo-orthorhombic.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0005729GladiusiteSokolova E V, Hawthorne F C, McCammon C A, Liferovich R P (2001) The crystal structure of gladiusite, (Fe,Mg)4Fe2(PO4)(OH)11(H2O) The Canadian Mineralogist 39 1121-113020010293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
4.805 Å(100)
5.83 Å(89)
3.533 Å(84)
6.87 Å(77)
2.868 Å(66)
3.787 Å(62)
9.61 Å(53)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
22 : Hydration and low-? subsurface aqueous alteration (see also #23)

Type Occurrence of GladiusiteHide

General Appearance of Type Material:
Acicular masses and as freestanding radiating clusters of arrow-head crystals; clusters do not exceed 2 mm in diameter. The crystals show subtly curved faces and a habit similar to a double-edged sword. Acicular crystals vary from 0.5-7 um thick and from
Place of Conservation of Type Material:
A.E. Fersman Mineralogical Museum, Moscow, Russia (2310/1), and in the Geological Museum, Institute of Geosciences, University of Oulu, Finland (12182).
Geological Setting of Type Material:
Low-temperature hydrothermal mineral in vugs in veins of dolomitic carbonatite.
Associated Minerals at Type Locality:

Synonyms of GladiusiteHide

Other Language Names for GladiusiteHide

Related Minerals - Strunz-mindat GroupingHide

8.DF.WiperamingaiteNaCaFe3+Al(PO4)F5(OH) · H2OOrth. 222 : P212121
8.DF.KernowiteCu2Fe(AsO4)(OH)4 · 4H2OMon.
8.DF.05HotsoniteAl11(SO4)3(PO4)2(OH)21 · 16H2OTric.
8.DF.10Liskeardite[(Al,Fe)32(AsO4)18(OH)42(H2O)22] · 52H2OMon.
8.DF.10Rosièresite(Pb, Cu, Al, P, O, H)Amor.
8.DF.10EvansiteAl3(PO4)(OH)6 · 6H2OAmor.
8.DF.10BolivariteAl2(PO4)(OH)3 · 4-5H2OAmor.
8.DF.15Rusakovite(Fe3+,Al)5(VO4,PO4)2(OH)9 · 3H2O
8.DF.20LiroconiteCu2Al(AsO4)(OH)4 · 4H2OMon. 2/m
8.DF.25SieleckiiteCu3Al4(PO4)2(OH)12 · 2H2OMon. 2/m : B2/m
8.DF.30ChalcophylliteCu18Al2(AsO4)4(SO4)3(OH)24 · 36H2OTrig. 3 : R3
8.DF.35ParnauiteCu9(AsO4)2(SO4)(OH)10 · 7H2OOrth. mm2 : Pmn21
8.DF.50ForêtiteCu2Al2(AsO4)(OH,O,H2O)6 Tric. 1 : P1

Fluorescence of GladiusiteHide

Other InformationHide

Notes:
Soluble in HCl, after several hours at room temperature.
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 GladiusiteHide

References for GladiusiteHide

Localities for GladiusiteHide

Showing 2 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.
Russia (TL)
 
  • Murmansk Oblast
    • Kovdorsky District
Can. Mineral. 38:1477-1485. +1 other reference
Mikhailova et al. (2015)
 
and/or  
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