Beudantite
| Beudantite | |
|---|---|
|
Large brown crystals of Beudantite. | |
| General | |
| Category | Arsenate minerals |
| Formula (repeating unit) | PbFe3(OH)6SO4AsO4 |
| Strunz classification | 08.BL.10 |
| Dana classification | 43.4.1.1 |
| Crystal symmetry | Trigonal 3 2/m |
| Unit cell |
a = 7.32 Å, c = 17.02 Å; Z = 3 |
| Identification | |
| Color | black, dark green, brown, yellowish, red, greenish yellow, brown |
| Crystal habit | tabular, acute rhombohedral, pseudo-cubic, pseudo-cuboctahedral |
| Crystal system | Trigonal Hexagonal Scalenohedral |
| Cleavage | distinct; good on {0001} |
| Mohs scale hardness | 3.5-4.5 |
| Luster | vitreous, resinous |
| Streak | grayish yellow to green |
| Diaphaneity | transparent, translucent |
| Specific gravity | 4.48 |
| Optical properties | Uniaxial (-) |
| Refractive index | nω = 1.957 nε = 1.943 |
| Birefringence | δ = 0.014 |
| Pleochroism | visible |
| Other characteristics | Soluble in HCl |
| References | [1][2][3] |
Beudandite is a secondary mineral occurring in the oxidized zones of polymetallic deposits.[3] It is a lead, iron, arsenate, sulfate with endmember formula: PbFe3(OH)6SO4AsO4.
Beudantite is in a subgroup of the alunite group. It is the arsenate analogue of the phosphate corkite. Beudantite also forms a solid-solution with segnitite and plumbojarosite.[1]
It crystallizes in the trigonal crystal system and shows a variety of crystal habits including tabular, acute rhombohedral, pseudo-cubic and pseudo-cuboctahedral.
It occurs in association with carminite, scorodite, mimetite, dussertite, arseniosiderite, pharmacosiderite, olivenite, bayldonite, duftite, anglesite, cerussite and azurite.[3]
Discovery
Beudantite was first described in 1826 for an occurrence in the Louise Mine, Wied Iron Spar District, Westerwald, Rhineland-Palatinate, Germany. It was named by Armand Lévy after his fellow Frenchman and mineralogist François Sulpice Beudant (1787–1850).[1]
References
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