Honessite (original) (raw)
A valid IMA mineral species - grandfathered
About HonessiteHide
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Formula:
(Ni1-xFe3+x)(OH)2[SO4]x/2 · nH2O
Name:
Named in 1956 by Allen V. Heyl, Charles Milton, and Joseph M. Axelrod in honor of Arthur Pharaoh Honess (10 August 1887, Berea, Ohio - 17 December 1942, Pennsylvania), Professor of Mineralogy in the School of Mineral Industries at Pennsylvania State College.
Often occurs as pseudomorphs after acicular millerite.
May convert readily into hydrohonessite, depending on humidity and temperature.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:1927:5
078dc343-64fb-4965-a0dc-3298bd68dc6c
IMA Classification of HonessiteHide
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Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
(Ni1-xFe3+x)(SO4)x/2(OH)2 · nH2O (x < 0.5, n < 3x/2)
Type description reference:
Classification of HonessiteHide
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7.DD.35
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
D : Sulfates (selenates, etc.) with additional anions, with H2O
D : With only medium-sized cations; sheets of edge-sharing octahedra
31.10.6.1
31 : HYDRATED SULFATES CONTAINING HYDROXYL OR HALOGEN
10 : Miscellaneous
25.12.11
25 : Sulphates
12 : Sulphates of Co and Ni
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 |
---|---|---|
Hon | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Hon | 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 HonessiteHide
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Optical Data of HonessiteHide
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RI values:
_n_α = 1.615 _n_β = 1.635
δ = 1.615
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Chemistry of HonessiteHide
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Mindat Formula:
(Ni1-xFe3+x)(OH)2[SO4]x/2 · nH2O
(x < 0.5, n > 3x/2)
Crystallography of HonessiteHide
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Cell Parameters:
a = 3.083(4) Å, c = 26.71(9) Å
Unit Cell V:
219.86 ų (Calculated from Unit Cell)
Comment:
Point Group: n.d.; : Space Group: n.d; Z = n.d.
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
8.84 Å | (100) |
4.43 Å | (40) |
2.62 Å | (20) |
1.54 Å | (15) |
1.52 Å | (15) |
2.65 Å | (10) |
2.39 Å | (10) |
Geological EnvironmentHide
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Type Occurrence of HonessiteHide
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General Appearance of Type Material:
Green or brown powdery alteration of millerite.
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, 117698.
Geological Setting of Type Material:
Mississippi Valley-type lead-zinc district.
Associated Minerals at Type Locality:
Reference:
Heyl, A.V., Milton, C., Axelrod, J.M. (1956) Nickel minerals from near Linden, Iowa County, Wisconsin. Bulletin of the Geological Society of America: 67: 1706.
Other Language Names for HonessiteHide
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Relationship of Honessite 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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7.DD. | Asagiite | NiCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/b |
---|---|---|---|
7.DD.05 | Felsőbányaite | Al4(SO4)(OH)10 · 4H2O | Mon. 2 : _P_21 |
7.DD.07 | Llantenesite | Cu6Al[SeO4](OH)12Cl · 3H2O | Trig. 3_m_ : P_31_c |
7.DD.10 | Langite | Cu4(SO4)(OH)6 · 2H2O | Mon. m |
7.DD.10 | Posnjakite | Cu4(SO4)(OH)6 · H2O | Mon. m : P m |
7.DD.10 | Wroewolfeite | Cu4(SO4)(OH)6 · 2H2O | Mon. m : P m |
7.DD.10 | Gobelinite | CoCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/m |
7.DD.10 | Fehrite | MgCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/b |
7.DD.15 | Spangolite | Cu6Al(SO4)(OH)12Cl · 3H2O | Trig. 3_m_ : P_31_c |
7.DD.15 | Kobyashevite | Cu5(SO4)2(OH)6 · 4H2O | Tric. 1 : _P_1 |
7.DD.15 | Unnamed (Dimorph of Devilline) | CaCu4(SO4)2(OH)6 · 3H2O | Mon. 2/m : _P_21/b |
7.DD.20 | Ktenasite | ZnCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/b |
7.DD.25 | Christelite | Cu2Zn3(SO4)2(OH)6 · 4H2O | Tric. 1 : _P_1 |
7.DD.30 | Campigliaite | Mn2+Cu4(SO4)2(OH)6 · 4H2O | Mon. 2 : _B_2 |
7.DD.30 | Devilline | CaCu4(SO4)2(OH)6 · 3H2O | Mon. 2/m : _P_21/b |
7.DD.30 | Orthoserpierite | Ca(Cu,Zn)4(SO4)2(OH)6 · 3H2O | Orth. m _m_2 : P c _a_21 |
7.DD.30 | Serpierite | Ca(Cu,Zn)4(SO4)2(OH)6 · 3H2O | Mon. 2/m : _B_2/b |
7.DD.30 | Niedermayrite | CdCu4(SO4)2(OH)6 · 4H2O | Mon. 2/m : _P_21/m |
7.DD.30 | Edwardsite | Cu3Cd2(SO4)2(OH)6 · 4H2O | Mon. 2/m : _P_21/b |
7.DD.35 | Carrboydite | (Ni1-xAlx)(SO4)x/2(OH)2 · nH2O | Hex. |
7.DD.35 | Glaucocerinite | (Zn1-xAlx)(OH)2(SO4)x/2 · nH2O | Hex. |
7.DD.35 | Hydrohonessite | (Ni1-xFe3+x)(OH)2(SO4)x/2 · nH2O | Hex. |
7.DD.35 | Motukoreaite | Mg6Al3(OH)18[Na(H2O)6][SO4]2 · 6H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
7.DD.35 | Mountkeithite | [(Mg1-xFe3+x)(OH)2][SO4]x/2 · nH2O | Hex. |
7.DD.35 | Shigaite | Mn6Al3(OH)18[Na(H2O)6](SO4)2 · 6H2O | Trig. 3 : _R_3 |
7.DD.35 | Wermlandite | Mg7Al2(OH)18[Ca(H2O)6][SO4]2 · 6H2O | Trig. 3_m_ _(_32/m ) : _P_3_c_1 |
7.DD.35 | Woodwardite | Cu1-xAlx(OH)2(SO4)x/2 · nH2O | Trig. 3_m_ _(_32/m ) : R_3_m |
7.DD.35 | Zincaluminite | Zn6Al6(SO4)2(OH)16 · 5H2O | |
7.DD.35 | Hydrowoodwardite | (Cu1-xAlx)(OH)2[SO4]x/2 · nH2O | Trig. 3_m_ _(_32/m ) : R_3_m |
7.DD.35 | Zincowoodwardite | Zn1-xAlx(OH)2[SO4]x/2 · nH2O | Trig. |
7.DD.35 | Natroglaucocerinite | Zn6Al3(OH)18[Na(H2O)6](SO4)2 · 6H2O | Hex. |
7.DD.35 | Nikischerite | Fe2+6Al3(OH)18[Na(H2O)6](SO4)2 · 6H2O | Trig. 3 : _R_3 |
7.DD.40 | Isselite | Cu6(SO4)(OH)10 · 5H2O | Orth. m _m_2 : P m _n_21 |
7.DD.40 | Lawsonbauerite | (Mn2+,Mg)9Zn4(SO4)2(OH)22 · 8H2O | Mon. 2/m : _P_21/b |
7.DD.40 | Torreyite | (Mg,Mn2+)7◻2Mn2+2Zn4(SO4)2(OH)22 · 8H2O | Mon. 2/m : _P_21/b |
7.DD.45 | Mooreite | Mg9◻2Mn2Zn4(SO4)2(OH)26 · 8H2O | Mon. 2/m : _P_2/b |
7.DD.45 | Hodgesmithite | (Cu,Zn)6Zn(SO4)2(OH)10 · 3H2O | Trig. 3 : _P_3 |
7.DD.47 | Lahnsteinite | Zn4(SO4)(OH)6 · 3H2O | Tric. 1 : _P_1 |
7.DD.50 | Namuwite | Zn4(SO4)(OH)6 · 4H2O | Trig. 3 : _P_3 |
7.DD.50 | Minohlite | (Cu,Zn)7(SO4)2(OH)10 · 8H2O | Hex. |
7.DD.52 | Lauraniite | Cu6Cd2(SO4)2(OH)12 · 5H2O | Mon. 2/m : _P_21/b |
7.DD.55 | Bechererite | Zn7Cu(OH)13[(SiO(OH)3(SO4)] | Trig. 3 : _P_3 |
7.DD.60 | Ramsbeckite | (Cu,Zn)15(SO4)4(OH)22 · 6H2O | Mon. 2/m |
7.DD.65 | Vonbezingite | Ca6Cu3(SO4)3(OH)12 · 2H2O | Mon. 2/m : _P_21/b |
7.DD.70 | Redgillite | Cu6(SO4)(OH)10 · H2O | Mon. 2/m : _P_21/b |
7.DD.75 | Chalcoalumite | CuAl4(SO4)(OH)12 · 3H2O | Mon. 2 : _P_21 |
7.DD.75 | Nickelalumite | NiAl4(SO4)(OH)12(H2O)3 | Mon. 2/m |
7.DD.75 | Kyrgyzstanite | ZnAl4(SO4)(OH)12 · 3H2O | Mon. 2/m |
7.DD.80 | Guarinoite | Zn6(SO4)(OH)10 · 5H2O | Hex. |
7.DD.80 | Schulenbergite | (Cu,Zn)7(SO4)2(OH)10 · 3H2O | Trig. 3 |
7.DD.80 | Thérèsemagnanite | NaCo4(SO4)(OH)6Cl · 6H2O | Trig. 3 : _P_3 |
7.DD.80 | UM1992-30-SO:CCuHZn | (Zn,Cu)7(SO4,CO3)2(OH)10 · 3H2O | Trig. 3 : _P_3 |
7.DD.85 | Montetrisaite | Cu6(SO4)(OH)10 · 2H2O | Orth. m _m_2 : C m _c_21 |
Other InformationHide
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Notes:
Insoluble in water. Soluble with slight effervescence in dilute acid solutions. Free oxygen is liberated.
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 HonessiteHide
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References for HonessiteHide
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Reference List:
Mills, S. J., Christy, A. G., Génin, J.-M. R., Kameda, T., Colombo, F. (2012) Nomenclature of the hydrotalcite supergroup: natural layered double hydroxides. Mineralogical Magazine, 76 (5) 1289-1336 doi:10.1180/minmag.2012.076.5.10
Localities for HonessiteHide
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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.