Schallerite (original) (raw)
A valid IMA mineral species - grandfathered
About SchalleriteHide
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Formula:
Mn2+16As3Si12O36(OH)17
Colour:
Light brown, reddish brown
Lustre:
Resinous, Waxy, Greasy
Name:
Named by Robert Burns Gage, Esper Signus Larsen (Senior), and Helen E. Vassar in 1925 after Waldemar Theodore Schaller [August 3, 1882 Oakland, California, USA - September 1, 1967 Washington, DC, USA] mineralogist and ore deposits specialist with the U. S. Geological Survey. USA.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:3557:2
bae7b1bd-875e-4eee-87b4-0857d134bf1e
IMA Classification of SchalleriteHide
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Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Mn2+16As3+3Si12O36(OH)17
Classification of SchalleriteHide
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9.EE.15
9 : SILICATES (Germanates)
E : Phyllosilicates
E : Single tetrahedral nets of 6-membered rings connected by octahedral nets or octahedral bands
72.4.1a.3
72 : PHYLLOSILICATES Two-Dimensional Infinite Sheets with Other Than Six-Membered Rings
4 : Two-Dimensional Infinite Sheets with Other Than Six-Membered Rings with 4-, 6-, and 12-membered rings
17.7.12
17 : Silicates Containing other Anions
7 : Silicates with vanadate, arsenate or antimonate
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.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Slr | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Slr | Warr (2020) | Warr, L.N. (2020) Recommended abbreviations for the names of clay minerals and associated phases. Clay Minerals, 55, 261–264 doi:10.1180/clm.2020.30 |
Physical Properties of SchalleriteHide
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Colour:
Light brown, reddish brown
Density:
3.37 g/cm3 (Measured) 3.45 g/cm3 (Calculated)
Optical Data of SchalleriteHide
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RI values:
_n_ω = 1.704 _n_ε = 1.679
δ = 0.025
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Chemistry of SchalleriteHide
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Mindat Formula:
Mn2+16As3Si12O36(OH)17
Common Impurities:
Ti,Al,Zn,Mg,Ca,Cl,H2O
Crystallography of SchalleriteHide
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Class (H-M):
3_m_ - Ditrigonal Pyramidal
Cell Parameters:
a = 13.43 Å, c = 14.31 Å
Unit Cell V:
2,235.23 ų (Calculated from Unit Cell)
Morphology:
Tapered pseudohexagonal horizontally striated crystals with pedion.
Comment:
Space group uncertain
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0015710 | Schallerite | Kato T, Watanabe I (1992) The crystal structures of schallerite and friedelite Yamaguchi University, College of Arts Bulletin 26 51-63 | 1992 | Franklin, New Jersey | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.55 Å | (40) |
2.83 Å | (30) |
2.67 Å | (60) |
2.47 Å | (50) |
2.02 Å | (50) |
1.975 Å | (40) |
1.688 Å | (100) |
1.511 Å | (60) |
Geological EnvironmentHide
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Type Occurrence of SchalleriteHide
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General Appearance of Type Material:
Massive, resembling bustamite or rhodochrosite.
Place of Conservation of Type Material:
Harvard University, Cambridge, Massachusetts, USA, number 87106.
National Museum of Natural History, Washington, D.C., USA, number R6610.
Geological Setting of Type Material:
Veinlets in willemite-franklinite ore, also with rhodonite.
Synonyms of SchalleriteHide
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Other Language Names for SchalleriteHide
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Relationship of Schallerite to other SpeciesHide
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Other Members of this group:
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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9.EE. | Cairncrossite | Sr2Ca7-xNa2x(Si4O10)4(OH)2(H2O)15-x | Tric. 1 : _P_1 |
---|---|---|---|
9.EE.05 | Bementite | Mn7Si6O15(OH)8 | Mon. |
9.EE.07 | Innsbruckite | Mn33(Si2O5)14(OH)38 | Mon. m : B m |
9.EE.10 | Brokenhillite | Mn8Si6O15(OH)10 | Hex. 6_m_ m : P_63_m c |
9.EE.10 | Pyrosmalite-(Fe) | Fe2+8Si6O15(OH,Cl)10 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
9.EE.10 | Friedelite | Mn2+8Si6O15(OH,Cl)10 | Mon. 2/m : _B_2/m |
9.EE.10 | Pyrosmalite-(Mn) | Mn2+8Si6O15(OH,Cl)10 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
9.EE.10 | Mcgillite | (Mn,Fe)8Si6O15(OH)8Cl2 | Mon. 2/m : _B_2/m |
9.EE.15 | Nelenite | (Mn,Fe)16(Si12O30)(OH)14[As3+3O6(OH)3] | Trig. 3_m_ _(_32/m ) : R_3_m |
9.EE.20 | Palygorskite | ◻Al2Mg2◻2Si8O20(OH)2(H2O)4 · 4H2O | Mon. 2/m : _B_2/m |
9.EE.20 | Tuperssuatsiaite | Fe3+Fe3+2(Na◻)◻2Si8O20(OH)2(H2O)4 · 2H2O | Mon. 2/m : _B_2/m |
9.EE.20 | Yofortierite | Mn2+Mn2+2Mn2+2◻2Si8O20(OH)2(H2O)4 · 4H2O | Mon. 2/m : _B_2/m |
9.EE.20 | Windhoekite | Fe3+(Fe3+1.67◻0.33)Ca2◻2Si8O20(OH)2(H2O)4(OH)2 · 6H2O | Mon. 2/m : _B_2/m |
9.EE.20 | Unnamed (Na-Ca-Fe-Silicate-Hydrate) | NaCa(Fe2+,Al,Mn)5[Si8O19(OH)](OH)7 · 5H2O | Tric. 1 : _P_1 |
9.EE.20 | Windmountainite | ◻Fe3+2Mg2◻2Si8O20(OH)2(H2O)4 · 4H2O | Mon. 2/m : _B_2/m |
9.EE.20 | Ikorskyite | KMn3+(Si4O10) · 3H2O | Mon. 2/m : _P_21/b |
9.EE.25 | Falcondoite | (Ni,Mg)4Si6O15(OH)2 · 6H2O | Orth. |
9.EE.25 | Loughlinite | Na2Mg3Si6O16 · 8H2O | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.EE.25 | Sepiolite | Mg4(Si6O15)(OH)2 · 6H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n a |
9.EE.25 | Kalifersite | (K,Na)5Fe3+7Si20O50(OH)6 · 12H2O | Tric. 1 : _P_1 |
9.EE.30 | Gyrolite | NaCa16Si23AlO60(OH)8 · 14H2O | Tric. 1 : _P_1 |
9.EE.30 | Orlymanite | Ca4Mn3Si8O20(OH)6 · 2H2O | Hex. |
9.EE.30 | Tungusite | Ca4Fe2Si6O15(OH)6 | Tric. 1 : _P_1 |
9.EE.35 | Reyerite | (Na,K)2Ca14(Si,Al)24O58(OH)8 · 6H2O | Trig. 3 : _P_3 |
9.EE.35 | Truscottite | (Ca,Mn)14Si24O58(OH)8 · 2H2O | Trig. |
9.EE.35 | Kodamaite | Na3(Ca5Na)Si16O36(OH)4F2 · (14-x)H2O | Tric. 1 : _P_1 |
9.EE.40 | Natrosilite | Na2Si2O5 | Mon. 2/m : _P_21/b |
9.EE.45 | Makatite | Na2Si4O8(OH)2 · 4H2O | Mon. 2/m : _P_21/b |
9.EE.50 | Varennesite | Na8Mn2Si10O25(OH,Cl)2 · 12H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m |
9.EE.55 | Raite | Mn2+Mn2+2Na2(◻1.75Ti0.25)Si8O20(OH)2(H2O)4 · Na(H2O)6 | Orth. 222 : _C_222 |
9.EE.60 | Intersilite | Na6Mn2+Ti[Si10O24(OH)](OH)3 · 4H2O | Mon. |
9.EE.65 | Shafranovskite | Na3K2(Mn,Fe,Na)4[Si9(O,OH)27](OH)2 · nH2O | Trig. 3_m_ : P_31_c |
9.EE.65 | Zakharovite | Na4Mn5Si10O24(OH)6 · 6H2O | Trig. 3_m_ |
9.EE.70 | Zeophyllite | Ca13Si10O28(OH)2F8 · 6H2O | Trig. 3 : _R_3 |
9.EE.75 | Minehillite | (K,Na)2-3Ca28Zn4Al4Si40O112(OH)16 | Hex. |
9.EE.80 | Fedorite | (Na,K)2-3(Ca4Na3)Si16O38(OH,F)2 · 3.5H2O | Tric. 1 : _P_1 |
9.EE.80 | Martinite | (Na,◻,Ca)12Ca4(Si,S,B)14B2O38(OH,Cl)2F2 · 4H2O | Tric. 1 : _P_1 |
9.EE.80 | Ellingsenite | Na5Ca6Si18O38(OH)13 · 6H2O | Tric. 1 : _P_1 |
9.EE.85 | Lalondeite | (Na,Ca)6(Ca,Na)3Si16O38(F,OH)2 · 3H2O | Tric. 1 : _P_1 |
Other InformationHide
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Notes:
In a closed tube, gives off water at a fairly low heat. Upon increasing the heat it produces an arsenic coating in the neck of the closed tube. This is very characteristic, and together with its appearance is sufficient distinguish it from willemite, bustamite, rhodonite, rhodochrosite, or friedelite.
Slowly decomposed by hot hydrochloric acid leaving a residue of granular silica.
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 SchalleriteHide
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References for SchalleriteHide
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Localities for SchalleriteHide
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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.