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Blossite

A valid IMA mineral species
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08819620014946272122650.jpg
Dr. F. Donald Bloss
Formula:
α-Cu2(V2O7)
Colour:
Black
Lustre:
Metallic
Specific Gravity:
3.95 - 3.97
Crystal System:
Orthorhombic
Name:
Named in honor of Dr. Fred Donald Bloss (30 May 1920, Chicago, Illinois - 22 April, 2020, Blacksburg, Virginia), mineralogist at the Virginia Polytechnic Institute, Blacksburg, Virginia, USA. He was president of the Mineralogical Society of America, editor of the American Mineralogist and was an expert in optical mineralogy. He wrote several books including 'The Spindle Stage: Principles and Practice'.
Dimorphous with Ziesite


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Unique IdentifiersHide

Mindat ID:
697
Long-form identifier:
mindat:1:1:697:6
GUID
(UUID V4):
897be2a6-4a7d-4483-a19f-390b357f90d6

IMA Classification of BlossiteHide

Classification of BlossiteHide

8.FA.05

8 : PHOSPHATES, ARSENATES, VANADATES
F : Polyphosphates, Polyarsenates, [4]-Polyvanadates
A : Polyphosphates, etc., without OH and H2O; dimers of corner-sharing RO4 tetrahedra.
38.5.6.1

38 : ANHYDROUS NORMAL PHOSPHATES, ARSENATES, AND VANADATES
5 : Miscellaneous
21.1.7

21 : Vanadates (and vanadates with arsenate or phosphate)
1 : Vanadates of the alkalis and Cu

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

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

Physical Properties of BlossiteHide

Metallic
Transparency:
Opaque
Colour:
Black
Streak:
Red-brown
Density:
3.95 - 3.97 g/cm3 (Measured)    4.051 g/cm3 (Calculated)
Comment:
On synthetic material

Optical Data of BlossiteHide

Type:
Biaxial
RI values:
n = 2.05
Max Birefringence:
δ = 0.000
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Very High
Anisotropism:
Moderate; grey to creamy grey-brown
Bireflectance:
Weak to moderate; in shades of cream-white
Reflectivity:
WavelengthR1R2
481 nm14.6% 15.3%
547 nm15.4% 16.6%
591 nm14.8% 16.7%
644 nm14.5% 15.7%

Reflectance graph
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 16.7%.
R1 shown in black, R2 shown in red
Colour in reflected light:
White
Internal Reflections:
Red-brown

Chemistry of BlossiteHide

Mindat Formula:
α-Cu2(V2O7)

Crystallography of BlossiteHide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Space Group:
Fdd2
Cell Parameters:
a = 20.676(6) Å, b = 8.392(3) Å, c = 6.446(2) Å
Ratio:
a:b:c = 2.464 : 1 : 0.768
Unit Cell V:
1,118.46 ų (Calculated from Unit Cell)
Z:
8
Morphology:
Equant crysyals

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0001075BlossiteRobinson P D, Hughes J M, Malinconico M L (1987) Blossite, alpha-Cu2V2O7, a new fumarolic sublimate from Izalco volcano, El Salvador - data obtained by personal communication, May 2003. American Mineralogist 72 397-40019870293
0009498BlossiteMercurio-Lavaud D, Frit B (1973) Structure cristalline de la variete basse temperature du pyrovanadate de cuivre: Cu2V2O7 alpha Acta Crystallographica B29 2737-27411973synthetic0293
0009530BlossiteCalvo C, Faggiani R (1975) Alpha cupric divanadate Acta Crystallographica B31 603-6051975synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.260 Å(100)
3.080 Å(100)
3.220 Å(80)
2.483 Å(80)
2.102 Å(70)
2.096 Å(70)
1.712 Å(70)
Comments:
Recorded on synthetic α-Cu^2[V^2O^7]; ICDD 26-566

Geological EnvironmentHide

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

Type Occurrence of BlossiteHide

General Appearance of Type Material:
Equant anhedral crystals, to 150 µm, typically intergrown with other fumarolic copper vanadates
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA (No. 164270)
Geological Setting of Type Material:
Sublimates from the outer zone of a fumarole in the crater of a basaltic composite volcano, probably formed between 100 °C and 200 °C
Associated Minerals at Type Locality:
Reference:
Robinson, P.D., Hughes, J.M., Malinconico, M.L. (1987) Blossite, α-Cu2+2V5+2O7, a new fumarolic sublimate from Izalco volcano, El Salvador. American Mineralogist: 72: 397-400.

Synonyms of BlossiteHide

Other Language Names for BlossiteHide

German:Blossit
Spanish:Blossita

Related Minerals - Strunz-mindat GroupingHide

8.FA.AnastasenkoiteCaFe2+(P2O7)Tric. 1 : P1
8.FA.Phosphocyclite-(Fe)Fe2+2(P4O12)Mon. 2/m : B2/b
8.FA.Phosphocyclite-(Ni)Ni2(P4O12)Mon. 2/m : B2/b
8.FA.LisaniteCaNiP2O7Tric. 1 : P1
8.FA.ShasuiteCaNi3(P2O7)2Mon. 2/m : P21/b
8.FA.NabateaiteFe2P2O7Tric. 1 : P1
8.FA.SamraiteNi2P2O7Mon. 2/m : P21/b
8.FA.BakakiniteCa2V2O7Tric. 1 : P1
8.FA.10Ziesiteβ-Cu2(V2O7)Mon. 2/m : B2/b
8.FA.15ChervetitePb2(V2O7)Mon. 2/m : P21/b
8.FA.15UM1999-17:O:PbVPb4V2O9 or Pb4(VO4)2O
8.FA.20Pyrocoproite(K,Na)2Mg(P2O7)Mon.
8.FA.20PyrophosphiteK2Ca(P2O7)Mon.
8.FA.25Petewilliamsite(Ni,Co)30(As2O7)15Mon. 2 : B2

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 BlossiteHide

References for BlossiteHide

Localities for BlossiteHide

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.

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.
El Salvador (TL)
 
  • Sonsonate Department
Robinson et al. (1987) +1 other reference
Russia
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
Pekov et al. (2013)
 
and/or  
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