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

Calciolangbeinite

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

About CalciolangbeiniteHide

Formula:
K2Ca2(SO4)3
Colour:
Colorless
Lustre:
Vitreous
Hardness:
3 - 3½
Specific Gravity:
2.68
Crystal System:
Isometric
Name:
Name as being the Ca-analogue of langbeinite.
Chemically similar to 'Unnamed (Potassium Calcium Sulfate)'. The Ca analogue of langbeinite.

Forms a solid solution with the latter. The content of 20 mol%, or more, of the langbeinite end-member induces breakdown into cubic lower-magnesian calciolangbeinite and langbeinite, upon slow cooling.

The calciolangbeinite-O (low-temperature) polymorph, although topologically similar to calciolangbeinite-C (probably stabilized by Mg admixture), is "the first natural orthorhombic langbeinite-like sulfate".

Note: the original (first-described) material was the cubic polymorph.


Unique IdentifiersHide

Mindat ID:
42383
Long-form identifier:
mindat:1:1:42383:6

IMA Classification of CalciolangbeiniteHide

Classification of CalciolangbeiniteHide

7.AD.

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
A : Sulfates (selenates, etc.) without additional anions, without H2O
D : With only large cations

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

Physical Properties of CalciolangbeiniteHide

Vitreous
Transparency:
Transparent
Colour:
Colorless
Streak:
White
Hardness:
3 - 3½ on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
Not observed
Fracture:
Conchoidal
Density:
2.68(2) g/cm3 (Measured)    2.74 g/cm3 (Calculated)

Optical Data of CalciolangbeiniteHide

Type:
Isotropic
RI values:
n = 1.527(2)
Surface Relief:
Low (negative)
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

Chemistry of CalciolangbeiniteHide

Mindat Formula:
K2Ca2(SO4)3
Element Weights:
Element% weight
O42.996 %
S21.542 %
Ca17.950 %
K17.512 %

Calculated from ideal end-member formula.

Crystallography of CalciolangbeiniteHide

Polytype:
Formula:
Crystal System:
Class (H-M)
Space Group:
Space Group Setting:
Cell Parameters:
Ratio:
Unit Cell Volume (calc):
Z:
Comment:
Calciolangbeinite-CCalciolangbeinite-O
K2Ca2(SO4)3 K2Ca2(SO4)3
Isometric Orthorhombic 
23 - Tetartoidal222 - Disphenoidal
P213P212121
  
a = 10.1887(4) Å
a = 10.3330(2) Å, b = 10.5027(2) Å, c = 10.1763(2) Å
a:b:c = 0.984 : 1 : 0.969
V 1057.68 ųV 1104.37 ų
44
  

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45a : [Sulfates, arsenates, selenates, antimonates]
46 : Near-surface hydrothermal alteration of minerals (see also #22)
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
51 : Pyrometamorphic minerals (see also #54 and #56)<0.36

Type Occurrence of CalciolangbeiniteHide

Synonyms of CalciolangbeiniteHide

Other Language Names for CalciolangbeiniteHide

Relationship of Calciolangbeinite to other SpeciesHide

Other Members of Langbeinite Group:
Efremovite(NH4)2Mg2(SO4)3Iso. 23 : P213
Ferroefremovite(NH4)2Fe2+2(SO4)3Iso. 23 : P213
LangbeiniteK2Mg2(SO4)3Iso. 23 : P213
ManganolangbeiniteK2Mn2(SO4)3Iso. 23 : P213

Related Minerals - Strunz-mindat GroupingHide

7.AD.BubnovaiteK2Na8Ca(SO4)6Trig. 3m : P31c
7.AD.DobrovolskyiteNa4Ca(SO4)3Trig. 3 : R3
7.AD.MurphyitePb(Te6+O4)Mon. 2/m : P21/b
7.AD.CuprodobrovolskyiteNa4Cu(SO4)3Trig. 3 : R3
7.AD.KristjániteKNa2H(SO4)2Mon. 2/m
7.AD.05Mascagnite(NH4)2SO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.05ArcaniteK2SO4Orth. mmm(2/m2/m2/m)
7.AD.10MercalliteKHSO4Orth. mmm(2/m2/m2/m) : Pbca
7.AD.15MiseniteK8H6(SO4)7Mon.
7.AD.20Letovicite(NH4)3H(SO4)2Tric.
7.AD.25ThénarditeNa2SO4Orth. mmm(2/m2/m2/m) : Fddd
7.AD.25GlauberiteNa2Ca(SO4)2Mon. 2/m : B2/b
7.AD.30MetathénarditeNa2SO4Hex. 6/mmm(6/m2/m2/m) : P63/mmc
7.AD.30AnhydriteCaSO4Orth. mmm(2/m2/m2/m)
7.AD.35BaryteBaSO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.35CelestineSrSO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.35OlsacheritePb2(Se6+O4)(SO4)Orth.
7.AD.35AnglesitePbSO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.40KalistrontiteK2Sr(SO4)2Trig. 3m(32/m) : R3m
7.AD.40PalmieriteK2Pb(SO4)2Trig. 3m(32/m) : R3m
7.AD.45IvsiteNa3H(SO4)2Mon. 2/m : P21/b
7.AD.55MarkhininiteTlBi(SO4)2Tric. 1 : P1

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 17.5117% 5,429 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity:

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

Fluorescence of CalciolangbeiniteHide

Not fluorescent

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 CalciolangbeiniteHide

References for CalciolangbeiniteHide

Localities for CalciolangbeiniteHide

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.
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.
Israel
 
  • Southern District
    • Beersheba Subdistrict
      • Tamar Regional Council
        • Hatrurim Basin
Galuskin et al. (2016)
Palestine
 
  • West Bank
    • Bethlehem Governorate
Galuskina et al. (2019)
    • Quds Governorate
Galuskina et al. (2014)
Russia (TL)
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
        • Great Fissure eruption (Main Fracture)
          • Northern Breakthrough (North Breach)
            • Second scoria cone
Williams et al. (2011) +2 other references
 
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 02:31:41 Page updated: August 21, 2026 15:16:59
Go to top of page