mottramite
Sign in to saveMottramite is an orthorhombic anhydrous vanadate hydroxide mineral, PbCu(VO4)(OH), at the copper end of the descloizite subgroup. It was formerly called cuprodescloizite or psittacinite (this mineral characterized in 1868 by Frederick Augustus Genth). Duhamelite is a calcium- and bismuth-bearing variety of mottramite, typically with acicular habit.
Key facts
- Mineral.name
- Mottramite
- Mineral.image
- Mottramite-174237.jpg
- Mineral.imagesize
- 260px
- Mineral.category
- Vanadate minerals
- Mineral.formula
- PbCu(VO4)(OH)
- Mineral.IMAsymbol
- Mott
- Mineral.molweight
- 402.69 g/mol
- Mineral.strunz
- 8.BH.40
- Mineral.dana
- 41.5.2.2
- Mineral.system
- Orthorhombic
- Mineral.class
- Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m)
- Mineral.symmetry
- Pnma
- Mineral.unit cell
- a = 7.68 Å, b = 9.27 Å, c = 6.03 Å; Z = 4
- Mineral.colour
- Grass-green, olive-green, yellow-green, siskin-green, blackish brown, nearly black
- Mineral.habit
- Encrustations, aggregates of plume-like forms and radial crystals
- Mineral.cleavage
- None observed
- Mineral.fracture
- Irregular/uneven, sub-conchoidal
- Mineral.tenacity
- Brittle
via Wikipedia infobox
Wikidata facts
- Image
- Mottramit - Mineralogisches Museum Bonn (7284).jpg
Show 6 more facts
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 8.BH.40
- Commons category
- Mottramite
- Nickel-Strunz 9th edition (updated 2009)
- 8.BH.40
- IMA Mineral Symbol
- Mott
- chemical formula
- PbCuVO₄(OH)
- Strunz 8th edition (series ID, updated)
- VII/B.11b
Sources (1)
via Wikidata · CC0
~12 min read
Article
7 sectionsContents
- Crystallography
- Appearance
- Physical properties
- Optical properties
- Occurrence
- Localities
- References
Mottramite is an orthorhombic anhydrous vanadate hydroxide mineral, PbCu(VO4)(OH), at the copper end of the descloizite subgroup. It was formerly called cuprodescloizite or psittacinite (this mineral characterized in 1868 by Frederick Augustus Genth). Duhamelite is a calcium- and bismuth-bearing variety of mottramite, typically with acicular habit.
Mottramite is a member of the adelite-descloizite group. Mottramite, which is a copper rich member, forms a series with descloizite, which is a zinc rich member. These two minerals usually contain significant percentages of both copper and zinc and are seldom pure. Mottramite also forms a series with duftite.