Vulcanite (original) (raw)
A valid IMA mineral species
About VulcaniteHide
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Specific Gravity:
7.1 (Calculated)
Crystal System:
Orthorhombic
Name:
According to the type description, vulcanite is named for "the locality of the mine", but it is unclear whether this refers to the town of Vulcan, located near the mine, or the Vulcan mining district.
This page provides mineralogical data about Vulcanite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:4213:6
2237b8ff-7aa5-4230-8b66-ae3ea338166c
IMA Classification of VulcaniteHide
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Type description reference:
Classification of VulcaniteHide
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2.CB.75
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
C : Metal Sulfides, M: S = 1: 1 (and similar)
B : With Zn, Fe, Cu, Ag, etc.
2.8.13.1
2 : SULFIDES
8 : AmXp, with m:p = 1:1
3.1.18
3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)
1 : Sulphides etc. of Cu
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Vul | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Pronunciation of VulcaniteHide
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Pronunciation:
Play | Recorded by | Country |
---|---|---|
Sorry, your browser doesn't support HTML5 audio. | Jolyon Ralph | United Kingdom |
Physical Properties of VulcaniteHide
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Hardness:
VHN50=34 - 40 kg/mm2 - Vickers
Cleavage:
Distinct/Good
One direction parallel to the length of the lath-shaped grains; another direction, less prominent, perpendicular to the first.
Density:
7.1 g/cm3 (Calculated)
Optical Data of VulcaniteHide
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Anisotropism:
very strong: brilliant yellow-white, grayish yellow-white, yellow-orange to gray
Bireflectance:
very strong
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 25.6% | 30.7% |
420nm | 24.4% | 30.0% |
440nm | 23.0% | 30.5% |
460nm | 21.3% | 37.0% |
480nm | 19.7% | 47.9% |
500nm | 18.1% | 56.8% |
520nm | 16.6% | 63.4% |
540nm | 15.2% | 67.8% |
560nm | 13.8% | 70.8% |
580nm | 12.7% | 73.1% |
600nm | 11.8% | 74.9% |
620nm | 11.3% | 76.4% |
640nm | 11.2% | 77.4% |
660nm | 11.6% | 78.2% |
680nm | 12.9% | 78.9% |
700nm | 15.0% | 79.3% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 79.3%.
R1 shown in black, R2 shown in red
Colour in reflected light:
bright yellow or yellow-white to medium blue-gray
Comments:
bright yellow to blue-gray
Chemistry of VulcaniteHide
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Crystallography of VulcaniteHide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 4.09 Å, b = 6.95 Å, c = 3.15 Å
Ratio:
a:b:c = 0.588 : 1 : 0.453
Unit Cell V:
89.54 ų (Calculated from Unit Cell)
Twinning:
Very thin twin lamellae at approximately 45◦ to the prominent cleavage in some grains.
Comment:
Space Group: Pmnm.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0015547 | Vulcanite | Baranova R V, Pinsker Z G (1964) Study of the copper-tellurium system in thin films Soviet Physics Crystallography 9 83-85 | 1964 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.03 Å | (100) |
2.86 Å | (70) |
3.52 Å | (60) |
6.94 Å | (40) |
3.47 Å | (30) |
2.65 Å | (30) |
2.32 Å | (30) |
Geological EnvironmentHide
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Type Occurrence of VulcaniteHide
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Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, R933, 85136
Associated Minerals at Type Locality:
Reference:
Cameron, E.N., Threadgold, I.M. (1961) Vulcanite, a new copper telluride from Colorado, with notes on certain associated minerals. American Mineralogist: 46: 258-268.
Other Language Names for VulcaniteHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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2.CB. | Agmantinite | Ag2MnSnS4 | Orth. |
---|---|---|---|
2.CB. | Richardsite | Zn2CuGaS4 | Tet. 42_m_ : I_42_m |
2.CB. | Gachingite | Au(Te1-xSex) | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CB. | Tolstykhite | Au3S4Te6 | Tric. 1 : _P_1 |
2.CB. | Hanswilkeite | KFeS2 | Mon. 2/m : _B_2/b |
2.CB. | Auroselenide | AuSe | Mon. 2/m : _B_2/m |
2.CB. | Ruizhongite | (Ag2◻)Pb3Ge2S8 | Iso. 43_m_ : I_43_d |
2.CB. | Okruginite | Cu2SnSe3 | Mon. m : B b |
2.CB.05a | Coloradoite | HgTe | Iso. 43_m_ : F_43_m |
2.CB.05a | Hawleyite | CdS | Iso. 43_m_ : F_43_m |
2.CB.05a | Metacinnabar | HgS | Iso. 43_m_ : F_43_m |
2.CB.05c | Polhemusite | (Zn,Hg)S | Tet. |
2.CB.05b | Sakuraiite | (Cu,Zn,Fe)3(In,Sn)S4 | Iso. |
2.CB.05a | Sphalerite | ZnS | Iso. 43_m_ : F_43_m |
2.CB.05a | Stilleite | ZnSe | Iso. 43_m_ : F_43_m |
2.CB.05a | Tiemannite | HgSe | Iso. 43_m_ : F_43_m |
2.CB.05 | UM1998-15-S:CuFeZn | Cu2Fe3Zn5S10 | |
2.CB.05a | Rudashevskyite | (Fe,Zn)S | Iso. 43_m_ : F_43_m |
2.CB.05a | Ishiharaite | (Cu,Ga,Fe,In,Zn)S | Iso. 43_m_ : F_43_m |
2.CB.07a | Shenzhuangite | NiFeS2 | Tet. 42_m_ : I_42_d |
2.CB.07a | Unnamed (Cu-Mn-Sn Sulphide) | Cu2MnSnS4 | |
2.CB.10a | Chalcopyrite | CuFeS2 | Tet. 42_m_ : I_42_d |
2.CB.10a | Eskebornite | CuFeSe2 | Tet. 42_m_ : P_42_c |
2.CB.10a | Gallite | CuGaS2 | Tet. 42_m_ : I_42_d |
2.CB.10b | Haycockite | Cu4Fe5S8 | Orth. 222 |
2.CB.10a | Lenaite | AgFeS2 | Tet. 42_m_ : I_42_d |
2.CB.10b | Mooihoekite | Cu9Fe9S16 | Tet. 42_m_ : P_42_m |
2.CB.10b | Putoranite | Cu1.1Fe1.2S2 | Iso. m_3_m _(_4/_m_32/m ) : P n_3_m |
2.CB.10a | Roquesite | CuInS2 | Tet. 42_m_ : I_42_d |
2.CB.10b | Talnakhite | Cu9(Fe,Ni)8S16 | Iso. 43_m_ : I_43_m |
2.CB.10a | Laforêtite | AgInS2 | Tet. 42_m_ : I_42_d |
2.CB.10a | Unnamed (Cu-Zn-In Sulphide) | CuZn2InS4 | |
2.CB.10a | UM1984-30-S:CuFeSn | Cu2Fe2Sn3S7 | |
2.CB.10c | Omariniite | Cu8Fe2ZnGe2S12 | Orth. 222 : _I_222 |
2.CB.15a | Černýite | Cu2(Cd,Zn,Fe)SnS4 | Tet. 42_m_ : I_42_m |
2.CB.15a | Ferrokësterite | Cu2FeSnS4 | Tet. 4 : _I_4 |
2.CB.15a | Hocartite | Ag2(Fe2+,Zn)SnS4 | Tet. 42_m_ : I_42_m |
2.CB.15a | Idaite | Cu5FeS6 | Hex. |
2.CB.15a | Kësterite | Cu2ZnSnS4 | Tet. 4 : _I_4 |
2.CB.15a | Kuramite | Cu3SnS4 | Tet. 42_m_ : I_42_m |
2.CB.15b | Mohite | Cu2SnS3 | Mon. |
2.CB.15a | Pirquitasite | Ag2ZnSnS4 | Tet. 4 : _I_4 |
2.CB.15a | Stannite | Cu2FeSnS4 | Tet. 42_m_ : I_42_m |
2.CB.15c | Stannoidite | Cu+6Cu2+2(Fe2+,Zn)3Sn2S12 | Orth. 222 : _I_222 |
2.CB.15a | Velikite | Cu2HgSnS4 | Tet. 4 : _I_4 |
2.CB.15c | UM2006-11-S:CuFeGeZn | Cu8(Fe,Zn)3Ge2S12 (?) | |
2.CB.17a v | Arsenic-bearing Renierite | Cu11GeAsFe4S16 | |
2.CB.20 | Chatkalite | Cu6FeSn2S8 | Tet. 42_m_ : _P_4_m_2 |
2.CB.20 | Mawsonite | Cu6Fe2SnS8 | Tet. 42_m_ : _P_4_m_2 |
2.CB.30 | Argyropyrite | near Ag2Fe7S11 | |
2.CB.30 | Colusite | Cu13VAs3S16 | Iso. 43_m_ : P_43_n |
2.CB.30 | Germanite | Cu13Fe2Ge2S16 | Iso. 43_m_ : P_43_n |
2.CB.30 | Germanocolusite | Cu26V2(Ge,As)6S32 | Iso. 43_m_ : P_43_m |
2.CB.30 | Nekrasovite | Cu26V2(Sn,As,Sb)6S32 | Iso. 43_m_ : P_43_n |
2.CB.30 | Stibiocolusite | Cu13V(Sb,Sn,As)3S16 | Iso. 43_m_ : P_43_m |
2.CB.30 | Ovamboite | Cu20(Fe,Cu,Zn)6W2Ge6S32 | Iso. 43_m_ : P_43_n |
2.CB.30 | Maikainite | Cu20(Fe,Cu)6Mo2Ge6S32 | Iso. m_3_m _(_4/_m_32/m ) |
2.CB.30 | Frieseite | Ag2Fe5S8 (?) | |
2.CB.35a | Hemusite | Cu6SnMoS8 | Iso. |
2.CB.35a | Kiddcreekite | Cu6SnWS8 | Iso. 43_m_ : F_43_m |
2.CB.35a | Polkovicite | (Fe,Pb)3(Ge,Fe)1-xS4 | Iso. |
2.CB.35a | Renierite | (Cu1+,Zn)11Fe4(Ge4+,As5+)2S16 | Tet. 42_m_ : P_42_c |
2.CB.35a | Vinciennite | Cu+7Cu2+3Fe2+2Fe3+2Sn(As,Sb)S16 | Tet. |
2.CB.35a | Morozeviczite | (Pb,Fe)3Ge1-xS4 | Iso. |
2.CB.35b | Catamarcaite | Cu6GeWS8 | Hex. 6_m_ m : P_63_m c |
2.CB.40 | Lautite | CuAsS | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CB.42 | Lingbaoite | AgTe3 | Trig. 3_m_ : R_3_m |
2.CB.45 | Cadmoselite | CdSe | Hex. 6_m_ m : P_63_m c |
2.CB.45 | Greenockite | CdS | Hex. 6_m_ m : P_63_m c |
2.CB.45 | Wurtzite | (Zn,Fe)S | Hex. 6_m_ m : P_63_m c |
2.CB.45 | Rambergite | MnS | Hex. 6_m_ m : P_63_m c |
2.CB.45 | Buseckite | (Fe,Zn,Mn)S | Hex. 6_m_ m : P_63_m c |
2.CB.45 | Maletoyvayamite | Au3Se4Te6 | Tric. 1 : _P_1 |
2.CB.47 | Murchisite | Cr5S6 | Trig. 3_m_ _(_32/m ) : P_31_c |
2.CB.50 | Zincselenide | ZnSe | |
2.CB.50 | Wassonite | TiS | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CB.52 | Dzhezkazganite | ReMoCu2PbS6 ? | Trig. 3_m_ : R_3_m |
2.CB.55a | Cubanite | CuFe2S3 | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CB.55b | Isocubanite | CuFe2S3 | Iso. m_3_m _(_4/_m_32/m ) : F m_3_m |
2.CB.60 | Picotpaulite | TlFe2S3 | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m |
2.CB.60 | Raguinite | TlFeS2 | Orth. |
2.CB.65 | Argentopyrite | AgFe2S3 | Mon. 2/m |
2.CB.65 | Sternbergite | AgFe2S3 | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CB.70 | Sulvanite | Cu3VS4 | Iso. 43_m_ : P_43_m |
2.CB.80 | Empressite | AgTe | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CB.85 | Muthmannite | AuAgTe2 | Mon. 2/m : _P_2/m |
Other InformationHide
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Notes:
Tests for Cu and Te positive. Etch tests: 1:1 HNO3 effervesces, staining dark gray; 1:7 HNO3 effervesces after about 20 seconds, stains brownish-gray, and brings out cleavage; HCl bleaches grayish-white; FeCl instantly darkens, staining light brown; KCN bleaches and then stains light brownish-gray; HgCl2 and KOH negative.
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 VulcaniteHide
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References for VulcaniteHide
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Localities for VulcaniteHide
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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
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- 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.