phoenicochroite
Sign in to saveAlso known as melanochroït
Phoenicochroite, also known as melanochroite, is a lead chromate mineral with formula Pb2OCrO4. It forms striking orange red crystals. It was first discovered in 1839 in Beryozovskoye deposit, Urals, Russia. It is named from the Greek word φοίυικος for "deep red" and χρόα for "color", in allusion to its color.
Key facts
- Mineral.name
- Phoenicochroite
- Mineral.image
- Phoenicochroite-212833.jpg
- Mineral.caption
- Deep red Phoenicochroite crystal, with orange-yellow schwartzembergite. San Francisco Mine, Tocopilla Province, Chile. Photo width 1.5 mm.
- Mineral.category
- Sulfate (chromate) mineral
- Mineral.formula
- Pb2O(CrO4)
- Mineral.IMAsymbol
- Phc
- Mineral.strunz
- 7.FB.05
- Mineral.dana
- 35.1.2.1 Anhydrous chromates
- Mineral.system
- Monoclinic
- Mineral.class
- Prismatic (2/m) (same H-M symbol)
- Mineral.symmetry
- C2/m
- Mineral.unit cell
- a = 14 Å, b = 5.67 Å, c = 7.13 Å; β = 115.22°; Z = 4
- Mineral.color
- Dark red, bright red
- Mineral.habit
- Tabular crystals; thin coatings, and massive
- Mineral.cleavage
- Perfect on {201}
- Mineral.tenacity
- Sectile
- Mineral.luster
- Adamantine, resinous
- Mineral.streak
- Brick-red
via Wikipedia infobox
Wikidata facts
- Image
- Phoenicochroite-212833.jpg
Show 6 more facts
- Strunz 8th edition (series ID, updated)
- VI/E.02
- IMA Mineral Symbol
- Phc
- chemical formula
- Pb₂O(CrO₄)
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 7.FB.05
- Commons category
- Phoenicochroite
- Nickel-Strunz 9th edition (updated 2009)
- 7.FB.05
Sources (1)
via Wikidata · CC0
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Article
1 sectionsContents
- References
{{Infobox mineral | name = Phoenicochroite | boxwidth = | boxbgcolor = | image = Phoenicochroite-212833.jpg | imagesize = | alt = | caption = Deep red Phoenicochroite crystal, with orange-yellow schwartzembergite. San Francisco Mine, Tocopilla Province, Chile. Photo width 1.5 mm. | category = Sulfate (chromate) mineral | formula = Pb2O(CrO4) | IMAsymbol = Phc | molweight = | strunz = 7.FB.05 | dana = 35.1.2.1 Anhydrous chromates | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = C2/m | unit cell = a = 14 Å, b = 5.67 Å, c = 7.13 Å; β = 115.22°; Z = 4 | color = Dark red, bright red | colour = | habit = Tabular crystals; thin coatings, and massive | twinning = | cleavage = Perfect on {201} | fracture = | tenacity = Sectile | mohs = | luster = Adamantine, resinous | streak = Brick-red | diaphaneity = Translucent | gravity = 5.75, 7.01 | density = | polish = | opticalprop = Biaxial (+) | refractive = nα = 2.380, nβ = 2.440, nγ = 2.650 | birefringence = 0.270 (δ) | pleochroism = | 2V = 58° (measured) | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = Health risks: contains carcinogenic and mutagenic chromate ion | prop1 = | prop1text = | references = }}
Phoenicochroite, also known as melanochroite, is a lead chromate mineral with formula Pb2OCrO4. It forms striking orange red crystals. It was first discovered in 1839 in Beryozovskoye deposit, Urals, Russia. It is named from the Greek word φοίυικος for "deep red" and χρόα for "color", in allusion to its color.