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

Vergasovaite

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

About VergasovaiteHide

Formula:
Cu3(SO4)(MoO4,SO4)O
Colour:
Olive-green
Lustre:
Vitreous
Hardness:
4 - 5½
Specific Gravity:
4.32 (Calculated)
Crystal System:
Orthorhombic
Name:
Named in honor of Lidiya Pavlovna Vergasova (Лидия Павловна Вергасова) (b. 1941, USSR), of the Institute of Volcanology, Russian Academy of Sciences, Petropavlovsk, Russia.
May topotactically transform into cupromolybdite (Nazarchuk et al., 2024).


Unique IdentifiersHide

Mindat ID:
7352
Long-form identifier:
mindat:1:1:7352:9

IMA Classification of VergasovaiteHide

Classification of VergasovaiteHide

7.BB.30

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
B : Sulfates (selenates, etc.) with additional anions, without H2O
B : With medium-sized 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
VgsIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of VergasovaiteHide

Vitreous
Transparency:
Transparent
Colour:
Olive-green
Streak:
Light yellow
Hardness:
4 - 5½ on Mohs scale
Hardness:
VHN25=302 - 413 kg/mm2 - Vickers
Tenacity:
Brittle
Fracture:
Irregular/Uneven
Density:
4.32 g/cm3 (Calculated)

Optical Data of VergasovaiteHide

Type:
Biaxial
RI values:
nα = 1.87 nγ = 1.98
Max. Birefringence:
δ = 0.110
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
Dispersion:
strong
Reflectivity:
WavelengthR1 (%)R2 (%)
400nm10.64% 13.03%
420nm10.39% 12.62%
440nm10.16% 12.17%
460nm9.95% 11.86%
470nm9.85% 11.69%
480nm9.8%11.61%
500nm9.66% 11.4%
520nm9.55% 11.22%
540nm9.42% 11.06%
546nm9.4% 11.01%
560nm9.35% 10.93%
580nm9.26% 10.78%
589nm9.22%10.76%
600nm9.11%10.63%
620nm9.07% 10.52%
640nm9% 10.48%
650nm9% 10.42%
660nm9.03% 10.45%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 13.03%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Gray
Internal Reflections:
Ubiquitous light green to white internal reflections
Pleochroism:
Visible
Comments:
Olive-green parallel to c; yellowish to brownish green ⊥ c.

Chemistry of VergasovaiteHide

Mindat Formula:
Cu3(SO4)(MoO4,SO4)O
Element Weights:
Element% weight
Cu41.205 %
O31.123 %
Mo20.741 %
S6.931 %

Calculated from ideal end-member formula.
Cu
O
Mo
S

Crystallography of VergasovaiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 7.421(2) Å, b = 6.754(3) Å, c = 13.624(5) Å
Ratio:
a:b:c = 1.099 : 1 : 2.017
Unit Cell V:
682.85 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Stout prismatic crystals, slightly elongate on [001]. Forms include {100}, {110}, {120}, {130}, {111}, {263}, and {315}. Also as radiating aggregates.
Twinning:
None observed.
Comment:
Space Group: P nma.

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)
0006764VergasovaiteBerlepsch P, Armbruster T, Brugger J, Bykova E Y, Kartashov P M (1999) The crystal structure of vergasovaite Cu3O[(Mo,S)O4SO4], and its relation to synthetic Cu3O[MoO4]2 European Journal of Mineralogy 11 101-11019990293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.077 Å(100)
3.391 Å(60)
3.342 Å(60)
2.542 Å(60)
2.500 Å(60)
2.275 Å(60)
3.71 Å(30)
Comments:
Treschina fumarole, Tolbachik volcano, Kamchatka Krai, Russia. The data are from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45a : [Sulfates, arsenates, selenates, antimonates]
45b : [Other oxidized fumarolic minerals]

Type Occurrence of VergasovaiteHide

General Appearance of Type Material:
Olive-green intergrowths of stout prismatic crystals, slightly elongate on [001] and up to 0.3 mm long. It also occurs as radiating aggregates, to 0.6 mm.
Place of Conservation of Type Material:
A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia;
Natural History Museum, Basel, Switzerland.
Geological Setting of Type Material:
Occurs on encrustations of sulfates in fumaroles.
Associated Minerals at Type Locality:

Synonyms of VergasovaiteHide

Other Language Names for VergasovaiteHide

Common AssociatesHide

Associations Based on Photo Data:
7 photos of Vergasovaite associated with EuchlorineKNaCu3(SO4)3O

Related Minerals - Strunz-mindat GroupingHide

7.BB.IskandaroviteSb6O7(SO4)2Orth. mm2 : Ccc2
7.BB.BrumadoiteCu3(Te6+O4)(OH)4 · 5H2OMon. 2/m : P21/m
7.BB.Novikovite(NH4)4Mo6+2Mo5+2O8(SO4)5Mon. 2/m
7.BB.10HauckiteFe3+3(Mg,Mn2+)24Zn18(SO4)4(CO3)2(OH)81Hex. 6/mmm(6/m2/m2/m) : P6/mmm
7.BB.15AntleriteCu3(SO4)(OH)4Orth. mmm(2/m2/m2/m)
7.BB.20DolerophaniteCu2(SO4)OMon. 2/m : B2/m
7.BB.25BrochantiteCu4(SO4)(OH)6Mon. 2/m : P21/b
7.BB.25RamaccioniiteCu4[SeO4](OH)6Mon. 2/m : P21/b
7.BB.30CupromolybditeCu3O(MoO4)2Orth. mmm(2/m2/m2/m) : Pnma
7.BB.35KlebelsbergiteSb4O4(SO4)(OH)2Orth. mm2
7.BB.35TavagnascoiteBi4O4(SO4)(OH)2Orth. mm2 : Pca21
7.BB.40SchuetteiteHg2+3O2(SO4)Trig. 32 : P3121
7.BB.45ParaotwayiteNi(OH)2-x(SO4,CO3)0.5xMon.
7.BB.50XocomecatliteCu3(TeO4)(OH)4Orth.
7.BB.55Pauflerite(V4+O)SO4Orth. mmm(2/m2/m2/m) : Pnma
7.BB.60GrandviewiteCu3Al2(SO4)(OH)10 · H2OTric. 1 : P1
7.BB.65TimroseitePb2Cu5(TeO6)2(OH)2Orth. mm2 : Pmn21
7.BB.70GlikiniteZn3O(SO4)2Mon. 2/m : P21/m
7.BB.80MojaveiteCu6[Te6+O4(OH)2](OH)7ClTrig. 3 : R3
7.BB.85ParatimroseitePb2Cu4(TeO6)2(H2O)2Orth. 222 : P212121

Fluorescence of VergasovaiteHide

Not fluorescent.

Other InformationHide

IR Spectrum:
The IR spectrum shows no indication of OH and H2O.
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 VergasovaiteHide

References for VergasovaiteHide

Localities for VergasovaiteHide

Showing 3 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.
Russia
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
        • Great Fissure eruption (Main Fracture)
          • Northern Breakthrough (North Breach)
Pekov et al. (2012)
Bykova et al. (1998)
Zelenski et al. (2012)
 
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 03:18:54 Page updated: August 23, 2026 18:01:35
Go to top of page