Redgillite (original) (raw)
A valid IMA mineral species
About RedgilliteHide
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Formula:
Cu6(SO4)(OH)10 · H2O
Colour:
Pale green, grass green, emerald green, nickel green
Crystal System:
Monoclinic
Name:
For its first noted occurrence at the Red Gill Mine (but not the type locality). The photo at right shows the mine that the mineral is named after, rather than the type locality.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:10349:1
1cf200d1-331c-4f70-ac8f-a7ed88671d66
IMA Classification of RedgilliteHide
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Classification of RedgilliteHide
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7.DD.70
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
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 |
---|---|---|
Rgl | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of RedgilliteHide
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Transparency:
Transparent, Translucent
Colour:
Pale green, grass green, emerald green, nickel green
Cleavage:
Perfect
On {001}, good on {100} and {010}.
Fracture:
Irregular/Uneven
Comment:
Brittle, slightly flexible, non-elastic.
Density:
3.45(5) g/cm3 (Measured) 3.450 g/cm3 (Calculated)
Optical Data of RedgilliteHide
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RI values:
_n_α = 1.693 _n_β = 1.721 _n_γ = 1.723
2V:
Measured: 30° (2), Calculated: 30°
δ = 0.030
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Optical Extinction:
X ≈ c, Y = b, Z ≈ a.
Comments:
X = Y = blue-green, Z = yellow-green.
Comments:
Absorption: Y > X > Z.
Chemistry of RedgilliteHide
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Mindat Formula:
Cu6(SO4)(OH)10 · H2O
Crystallography of RedgilliteHide
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Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Cell Parameters:
a = 3.155 Å, b = 10.441 Å, c = 19.436 Å
β = 90.089°
Ratio:
a:b:c = 0.302 : 1 : 1.862
Morphology:
Bladed crystals with squared-off or tapering terminations; usually in radiating groups.
Type material: Forms observed are {001} prominent, {010} as composite stepped faces, and {100} irregular.
Twinning:
Rarely on (001) (Schnorrer et al., 2006)
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
9.72 Å | (90) |
7.11 Å | (100) |
4.60 Å | (30) |
4.068 Å | (20) |
2.880 Å | (30) |
2.318 Å | (50) |
Geological EnvironmentHide
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Type Occurrence of RedgilliteHide
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General Appearance of Type Material:
Bladed crystals up to 0.15 mm long with squared-off or tapering terminations; usually in radiating groups.
Place of Conservation of Type Material:
Manchester Museum, The University of Manchester, England, MANCH:18024.
Geological Setting of Type Material:
In thin fractures in partly oxidized copper sulphides, probably dump-formed.
Associated Minerals at Type Locality:
Synonyms of RedgilliteHide
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Other Language Names for RedgilliteHide
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Simplified Chinese:瑞羟铜矾
Traditional Chinese:瑞羥銅礬
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 | Honessite | (Ni1-xFe3+x)(OH)2[SO4]x/2 · nH2O | Trig. |
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 | (Zn1-xAlx)(SO4)x/2(OH)2 · nH2O | |
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(H2O)4 · H2O | 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.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:
Dissolves slowly in dilute HCl.
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 RedgilliteHide
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References for RedgilliteHide
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Reference List:
Pluth, J. J., Steele, I. M., Kampf, A. R., Green, D. I. (2005) Redgillite, Cu6(OH)10(SO4)·H2O, a new mineral from Caldbeck Fells, Cumbria, England: description and crystal structure. Mineralogical Magazine, 69 (6) 973-980 doi:10.1180/0026461056960302
Localities for RedgilliteHide
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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.