Vote for your favorite mineral in #MinCup26! - Azurite vs. Smithsonite
It's carbonate-vs-carbonate to kick off Mineral Cup 2026 with copper-rich Azurite against zinc-rich Smithsonite.
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic TimeExplore Fossils
Minerals by PropertiesMinerals by ChemistryMineral Visual ExplorerAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral QuizTime Machine
Photo SearchPhoto GalleriesSearch by ColorPhoto Colour ExplorerNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Ferro-holmquistite

A valid IMA mineral species
This page is currently not sponsored. Click here to sponsor this page.
Formula:
◻Li2(Fe2+3Al2)(Si8O22)(OH)2
The holmquistite group comprises orthorhombic amphiboles in the lithium amphibole subgroup.

Holmquistite is defined with Fe2+>Mg and Al>Fe3+ in the C position.
The type material is Mg-rich.
Colour:
Black, dark-violet, light sky-blue.
Lustre:
Vitreous
Hardness:
5 - 6
Specific Gravity:
3.145 (Calculated)
Crystal System:
Orthorhombic
Name:
For its relationship to holmquistite.
Ferro-holmquistite forms a series with holmquistite. Like holmquistite, ferro-holmquistite is almost exclusively formed in the reaction zone between Li-pegmatites and their host rock, predominantly as a metasomatic alteration product of pre-existing amphiboles. Quéméneur and Lagache(1994) show a significant variation of Fe content in holmquistite from different localities and they suggest that the holmquistite minerals retain their Fe/Mg ratio from the original amphibole.

Ferro-holmquistite is under-reported in the literature, as both ferro-holmquistite and holmquistite are often referred to as holmquistite.


Hide all sections | Show all sections

Unique IdentifiersHide

Mindat ID:
8957
Long-form identifier:
mindat:1:1:8957:5

Similar NamesHide

Ferri-holmquistite◻{Li2}{Mg3Fe23+}(Si8O22)(OH)2

IMA Classification of Ferro-holmquistiteHide

Approved
IMA status notes:
Redefined by the IMA
IMA Formula:
◻Li2(Fe2+3Al2)Si8O22(OH)2
Approval year:
2004
First published:
2005
Approval history:
Redefined IMA 2012 s.p.

Classification of Ferro-holmquistiteHide

9.DD.05

9 : SILICATES (Germanates)
D : Inosilicates
D : Inosilicates with 2-periodic double chains, Si4O11; Orthoamphiboles

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

Physical Properties of Ferro-holmquistiteHide

Vitreous
Transparency:
Translucent
Colour:
Black, dark-violet, light sky-blue.
Streak:
Light bluish-violet. White with a sky-blue tinge (?)
Hardness:
5 - 6 on Mohs scale
Density:
3.145 g/cm3 (Calculated)

Optical Data of Ferro-holmquistiteHide

Type:
Biaxial (-)
RI values:
nα = 1.628 nβ = 1.646 nγ = 1.651
2V:
Calculated: 55.1°
Max. Birefringence:
δ = 0.023
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
Optical Extinction:
c = X, with the optic axial plane coinciding with (010).
Pleochroism:
Weak
Comments:
α = colorless, β = pale violet-blue, γ = blue to deep violet.

Chemistry of Ferro-holmquistiteHide

Mindat Formula:
◻Li2(Fe2+3Al2)(Si8O22)(OH)2

The holmquistite group comprises orthorhombic amphiboles in the lithium amphibole subgroup.

Holmquistite is defined with Fe2+>Mg and Al>Fe3+ in the C position.
The type material is Mg-rich.
Element Weights:
Element% weight
O45.385 %
Si26.556 %
Fe19.802 %
Al6.378 %
Li1.641 %
H0.238 %

Calculated from ideal end-member formula.

Crystallography of Ferro-holmquistiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pnma
Setting:
Pnma
Cell Parameters:
a = 18.287 Å, b = 17.68 Å, c = 5.278 Å
Ratio:
a:b:c = 1.034 : 1 : 0.299
Unit Cell V:
1706.45 ų
Z:
4
Morphology:
Prismatic crystals.

Crystal StructureHide

Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File    Best | x | y | z | a | b | c
Rotation
Stop | Start
Labels
Console Off | On | Grey | Yellow
IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0003812Ferro-holmquistiteCamara F, Oberti R (2005) The crystal-chemistry of holmquistites: Ferroholmquistite from Greenbushes (Western Australia) and hints for compositional constraints in B-Li amphiboles American Mineralogist 90 1167-117620050293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.1128 Å(100)
3.0047 Å(10)
1.5818 Å(7)
2.7095 Å(5)
Comments:
Greenbushes Mine, Western Australia, Australia. The data are from Camara and Oberti (2005).

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
34 : Complex granite pegmatites

Type Occurrence of Ferro-holmquistiteHide

General Appearance of Type Material:
Elongated black to bluish-violet prismatic crystals, typically in the range 0.2–0.5 mm.
Place of Conservation of Type Material:
Museum of the Dipartimento di Scienze della Terra, Universita di Pavia #2004-01
Empirical Formula of Type Material:
A(K0.01Na0.01)B(Li1.88Mg0.08Na0.03Fe2+ 0.01) C(Al1.89Fe2+ 1.70Mg1.39Mn2+ 0.02) TSi8.00O22(OH1.97F0.03)
Chemical Analysis of Type Material:
SiO259.37 %
TiO20.03 %
Al2O311.86 %
Cr2O30 %
MgO7.32 %
CaO0.03 %
MnO0.18 %
Fe2O30 %
FeO15.14 %
ZnO0.02 %
Na2O0.17 %
K2O0.03 %
F0.07 %
Cl0.01 %
Li2O3.46 %
H2O2.19 %
Total:99.88 %
Geological Setting of Type Material:
Lithium-rich granite pegmatite.
Associated Minerals at Type Locality:

Synonyms of Ferro-holmquistiteHide

Other Language Names for Ferro-holmquistiteHide

Relationship of Ferro-holmquistite to other SpeciesHide

Other Members of Holmquistite Root Name Group:
Ferro-ferri-holmquistite◻Li2(Fe2+3Fe3+2)(Si8O22)(OH)2Orth. mmm(2/m2/m2/m) : Pmma
Holmquistite◻Li2(Mg3Al2)(Si8O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnma

Related Minerals - Strunz-mindat GroupingHide

9.DD.05Suenoite◻Mn2+2Mg5Si8O22(OH)2Orth. mmm(2/m2/m2/m) : Pnma
9.DD.05Proto-ferro-anthophyllite◻Fe2+2Fe2+5(Si8O22)(OH)2Orth. mmm(2/m2/m2/m)
9.DD.05Proto-ferro-suenoite◻Mn2+2(Fe2+5)(Si8O22)(OH)2Orth. mmm(2/m2/m2/m)
9.DD.05PapikeiteNaMg2(Mg3Al2}(Al3Si5O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnma
9.DD.05Gedrite◻Mg2(Mg3Al2)(Al2Si6O22)(OH)2Orth. mmm(2/m2/m2/m)
9.DD.05Holmquistite◻Li2(Mg3Al2)(Si8O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnma
9.DD.05'Sodic-anthophyllite'{Na}{Mg2}{Mg5}(AlSi7O22)(OH)2Orth.
9.DD.05'Sodic-ferro-anthophyllite'NaFe2+2Fe2+5(AlSi7O22)(OH)2Orth.
9.DD.05Ferro-papikeiteNaFe2+2(Fe2+3Al2)(Si5Al3O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnma
9.DD.05Ferro-anthophyllite◻Fe2+2Fe2+5(Si8O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnma
9.DD.05Proto-anthophyllite◻Mg2Mg5(Si8O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnnm
9.DD.05Ferro-gedrite◻Fe2+2(Fe2+3Al2)(Al2Si6O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnma
9.DD.05'Ferri-holmquistite'◻{Li2}{Mg3Fe3+2}(Si8O22)(OH)2
9.DD.05Ferro-ferri-holmquistite◻Li2(Fe2+3Fe3+2)(Si8O22)(OH)2Orth. mmm(2/m2/m2/m) : Pmma
9.DD.05Anthophyllite◻Mg2Mg5(Si8O22)(OH)2Orth. mmm(2/m2/m2/m) : Pnma

Other InformationHide

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 Ferro-holmquistiteHide

References for Ferro-holmquistiteHide

Localities for Ferro-holmquistiteHide

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.
Hide all sections | Show all sections

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.
Australia (TL)
 
  • Western Australia
    • Bridgetown-Greenbushes Shire
      • Greenbushes tinfield
Camara et al. (2005)
Brazil
 
  • Minas Gerais
    • Nazareno
Quéméneur et al. (1994)
 
and/or  
Mindat.org® is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization. Mindat® and mindat.org® are registered trademarks of the Hudson Institute of Mineralogy.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2026, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph and Ida Chau.
Content on this site may not be used to train, fine-tune, or otherwise develop artificial intelligence or machine learning models without prior written permission - see our Terms & Conditions.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 1, 2026 14:25:11 Page updated: August 19, 2026 01:47:36
Go to top of page