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

Steigerite

A valid IMA mineral species - grandfathered
This page is currently not sponsored. Click here to sponsor this page.
Hide all sections | Show all sections

About SteigeriteHide

09690480017271926935914.jpg
George Steiger
Formula:
Al(VO4) · 3H2O
Colour:
Canary-yellow, greenish yellow, olive-green
Lustre:
Waxy
Hardness:
2½ - 3
Specific Gravity:
2.52 - 2.58
Crystal System:
Monoclinic
Name:
Named in honor of George Steiger (27 May 1869, Columbia, Pennsylvania, USA - 18 April 1944, Washington, D.C., USA), Chief Chemist, United States Geological Survey, Washington, D.C., USA.
A secondary mineral occurring either as impregnations in sandstones or as a weathering product from vanadium-rich schists.


Unique IdentifiersHide

Mindat ID:
3759
Long-form identifier:
mindat:1:1:3759:0

IMA Classification of SteigeriteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
AlV5+O4·3H2O

Classification of SteigeriteHide

8.CE.65

8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
E : With only medium-sized cations, RO4:H2O about 1:2.5
40.4.5.1

40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
4 : (AB)5(XO4)2·xH2O
21.3.1

21 : Vanadates (and vanadates with arsenate or phosphate)
3 : Vanadates of Al, rare earths, Pb, V or Bi

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

Physical Properties of SteigeriteHide

Transparency:
Translucent
Comment:
Lustre waxy in compact aggregates
Colour:
Canary-yellow, greenish yellow, olive-green
Hardness:
2½ - 3 on Mohs scale
Tenacity:
Fragile
Cleavage:
Perfect
On {010}, perfect; on {100}, fair.
Density:
2.52 - 2.58 g/cm3 (Measured)    2.58 g/cm3 (Calculated)

Optical Data of SteigeriteHide

Type:
Biaxial (+)
RI values:
nα = 1.72 - 1.73 nβ = 1.73 - 1.734 nγ = 1.748 - 1.752
Max. Birefringence:
δ = 0.022 - 0.028
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.

No measured or calculated 2V is on file for this mineral, so the value used here (64°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Dispersion:
relatively strong

Chemistry of SteigeriteHide

Mindat Formula:
Al(VO4) · 3H2O
Element Weights:
Element% weight
O57.151 %
V25.995 %
Al13.768 %
H3.086 %

Calculated from ideal end-member formula.
O
V
Al
H

Crystallography of SteigeriteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Cell Parameters:
a = 11.84 Å, b = 25 Å, c = 11.04 Å
β = 111.17°
Ratio:
a:b:c = 0.474 : 1 : 0.442
Unit Cell V:
3,047.30 ų (Calculated from Unit Cell)
Z:
24
Morphology:
Cryptocrystalline fibrous, may be flat platy {010} Gumlike to compact massive, commonly as powdery coatings.
Comment:
Class is either 2/ or 2; space group is either P21/m or P21.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.93 Å(100)
12.52 Å(50)
2.18 Å(50)
1.897 Å(50)
1.758 Å(50)
3.09 Å(40)
2.21 Å(40)
Comments:
Kara-Tau Mountains, Kazakhstan.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47e : [Vanadates, chromates, manganates]

Type Occurrence of SteigeriteHide

General Appearance of Type Material:
Fracture cotings
Place of Conservation of Type Material:
U.S. National Museum of Natural History, Washington, D.C., USA: #C5108.
Geological Setting of Type Material:
Nodular concretions of Corvusite in sandstone.
Associated Minerals at Type Locality:

Other Language Names for SteigeriteHide

German:Steigerit
Spanish:Steigerita

Varieties of SteigeriteHide

ChromsteigeriteA Cr-bearing variety of steigerite.

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Steigerite associated with Barnesite(Na,Ca)V6O16 · 3H2O
2 photos of Steigerite associated with GypsumCaSO4 · 2H2O
2 photos of Steigerite associated with VanoxiteV4+4V5+2O13 · 8H2O
1 photo of Steigerite associated with Bokite(Al,Fe)1.3(V5+,V4+,Fe3+)8O20 · 7.5H2O
1 photo of Steigerite associated with FervaniteFe3+4V5+4O16 · 5H2O
1 photo of Steigerite associated with Corvusite(Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O
1 photo of Steigerite associated with 'Petrified Wood'

Related Minerals - Strunz-mindat GroupingHide

8.CE.MonteneroiteCu2+Mn2+2(AsO4)2 · 8H2OMon. 2/m : B2/m
8.CE.BelmonteiteCaMn2(AsO4)2 · 7H2OOrth. mm2
8.CE.XBabánekiteCu3(AsO4)2 · 8H2O Mon. 2/m : B2/m
8.CE.05ChudobaiteMg5(AsO4)2(AsO3OH)2 · 10H2OTric. 1 : P1
8.CE.05GeigeriteMn2+5(AsO4)2(HAsO4)2 · 10H2OTric. 1 : P1
8.CE.10NewberyiteMg(PO3OH) · 3H2OOrth. mmm(2/m2/m2/m) : Pbca
8.CE.10ManganonewberyiteMn(PO3OH)(H2O)3Orth. mmm(2/m2/m2/m) : Pbca
8.CE.15Fanguangite(MoO2)(PO3OH) · 4H2OTric. 1 : P1
8.CE.15BrassiteMg(HAsO4) · 4H2OOrth. mmm(2/m2/m2/m) : Pbca
8.CE.20PhosphorrössleriteMg(PO3OH) · 7H2OMon. 2/m : P2/b
8.CE.20RössleriteMg(HAsO4) · 7H2OMon. 2/m : B2/b
8.CE.25SwitzeriteMn2+3(PO4)2 · 7H2OMon. 2/m : P21/b
8.CE.25MetaswitzeriteMn2+3(PO4)2 · 4H2OMon. 2/m : P2/b
8.CE.30PradetiteCoCu4(AsO4)2(HAsO4)2 · 9H2OTric. 1 : P1
8.CE.30VeselovskýiteZnCu4(AsO4)2(HAsO4)2 · 9H2OTric. 1 : P1
8.CE.30LindackeriteCuCu4(AsO4)2(HAsO4)2 · 9H2OTric. 1 : P1
8.CE.30KlajiteMnCu4(AsO4)2(HAsO4)2 · 9-10H2OTric. 1 : P1
8.CE.30Hloušekite(Ni,Co)Cu4(AsO4)2(AsO3OH)2 · 9H2OTric. 1 : P1
8.CE.30OndrušiteCaCu4(AsO4)2(HAsO4)2 · 10H2OTric. 1 : P1
8.CE.35BobierriteMg3(PO4)2 · 8H2OMon. 2/m : B2/b
8.CE.40Barićite(Mg,Fe)3(PO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40ParasymplesiteFe2+3(AsO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40GritsenkoiteCoMg2(AsO4)2(H2O)8Mon. 2/m : B2/m
8.CE.40CabreriteNiMg2(AsO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40PakhomovskyiteCo3(PO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40VivianiteFe2+Fe2+2(PO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40ArupiteNi3(PO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40ErythriteCo3(AsO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40HörnesiteMg3(AsO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40ManganohörnesiteMn2+3(AsO4)2 · 8H2OMon. 2/m : P2/m
8.CE.40KöttigiteZn3(AsO4)2 · 8H2OMon. 2/m : B2/m
8.CE.40FerrisymplesiteFe3+3(AsO4)2(OH)3 · 5H2OMon.
8.CE.40AnnabergiteNi3(AsO4)2 · 8H2OMon. 2/m : B2/m
8.CE.45SymplesiteFe2+3(AsO4)2 · 8H2OTric. 1 : P1
8.CE.50CattiiteMg3(PO4)2 · 22H2OTric. 1 : P1
8.CE.55KoninckiteFe3+PO4 · 3H2OTet. 422 : P41212
8.CE.60KaňkiteFeAsO4 · 3.5H2OMon. 2 : P2
8.CE.60HilarioniteFe3+2(SO4)(AsO4)(OH) · 6H2OMon. 2/m : B2/m
8.CE.70MetaschoderiteAl2(PO4)(VO4) · 6H2OMon. 2/m : P2/m
8.CE.70SchoderiteAl2(PO4)(VO4) · 8H2OMon.
8.CE.75ZigrasiteMgZr(PO4)2 · 4H2OTric. 1 : P1
8.CE.75'UM2009-11-PO:CaHZr'CaZr[PO4]2 · 4H2OTric.
8.CE.75MalhmooditeFeZr(PO4)2 · 4H2OMon. 2/m : P21/b
8.CE.80SantabarbaraiteFe3+3(PO4)2(OH)3 · 5H2OAmor.
8.CE.85Metaköttigite(Zn,Fe,Fe)3(AsO4)2 · 8(H2O,OH)Tric. 1 : P1
8.CE.90SlavkoviteCu13(AsO4)6(AsO3OH)4 · 23H2OTric. 1 : P1

Other InformationHide

Notes:
Readily soluble in dilute mineral acids to a deep cherry-red solution. Insoluble in water.
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 SteigeriteHide

References for SteigeriteHide

Localities for SteigeriteHide

Showing 11 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.
Kazakhstan
 
  • Kyzylorda Region
    • Shieli District
Fleischer (1959) +1 other reference
  • Turkistan Region
    • Ran River valley
Amer.Mineral. (1961)
    • Sozak District
      • Aksumbe
Evseev (1995) +1 other reference
USA
 
  • Arizona
    • Apache County
      • Cane Valley Mining District
        • Yazzie Mesa
          • Monument No. 2 channel
Weeks et al. (1955) +3 other references
  • Colorado
    • Mesa County
      • Calamity Mesa
Eckel et al. (1997)
Eckel et al. (1997)
    • Montrose County
Eckel et al. (1997)
    • San Miguel County
      • Gypsum Valley Mining District
Eckel et al. (1997)
Henderson (1935) +1 other reference
  • Utah
    • Grand County
      • Thompsons Mining District
        • The Poison Strip
Bullock (1981)
    • San Juan County
      • La Sal Creek Mining District
Collected and analyzed by Joy Desor.
 
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 13:20:59 Page updated: August 22, 2026 20:37:05
Go to top of page