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plattnerite
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plattnerite

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Plattnerite is an oxide mineral and is the beta crystalline form of lead dioxide (β-PbO2), scrutinyite being the other, alpha form. It was first reported in 1845 and named after German mineralogist Karl Friedrich Plattner. Plattnerite forms bundles of dark needle-like crystals on various minerals; the crystals are hard and brittle and have tetragonal symmetry.

Key facts

Mineral.name
Plattnerite
Mineral.category
Oxide minerals
Mineral.image
Galena-Quartz-136082.jpg
Mineral.caption
Quartz and galena sample, plattnerite over the large galena cube.
Mineral.formula
PbO2
Mineral.IMAsymbol
Ptn
Mineral.molweight
239.20 g/mol
Mineral.strunz
4.DB.05
Mineral.system
Tetragonal
Mineral.class
Ditetragonal dipyramidal (4/mmm) H–M Symbol: (4/m 2/m 2/m)
Mineral.symmetry
P42/mnm
Mineral.unit cell
a = 4.95 Å, c = 3.38 Å; Z = 2
Mineral.color
Dark brown, iron-black
Mineral.habit
Prismatic crystals, may be nodular or botryoidal, fibrous and concentrically zoned, massive
Mineral.twinning
Contact and penetration twinning on {011}, rarely polysynthetic
Mineral.cleavage
None
Mineral.fracture
Sub-conchoidal, fibrous
Mineral.tenacity
Brittle

via Wikipedia infobox

Wikidata facts

Image
Plattnerite16346-5.jpg
Show 6 more facts
IMA Mineral Symbol
Ptn
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
4.DB.05
Commons category
Plattnerite
chemical formula
PbO₂
Nickel-Strunz 9th edition (updated 2009)
4.DB.05
Strunz 8th edition (series ID, updated)
IV/D.02
Sources (1)

via Wikidata · CC0

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Article

4 sections
Contents
  • Occurrence
  • Properties and applications
  • References
  • External links

{{Infobox mineral | name = Plattnerite | category = Oxide minerals | boxwidth = | boxbgcolor = | image = Galena-Quartz-136082.jpg | imagesize = | caption = Quartz and galena sample, plattnerite over the large galena cube. | formula = PbO2 | IMAsymbol = Ptn | molweight = 239.20 g/mol | strunz = 4.DB.05 | system = Tetragonal | class = Ditetragonal dipyramidal (4/mmm) H–M Symbol: (4/m 2/m 2/m) | symmetry = P42/mnm | unit cell = a = 4.95 Å, c = 3.38 Å; Z = 2 | color = Dark brown, iron-black | habit = Prismatic crystals, may be nodular or botryoidal, fibrous and concentrically zoned, massive | twinning = Contact and penetration twinning on {011}, rarely polysynthetic | cleavage = None | fracture = Sub-conchoidal, fibrous | tenacity = Brittle | mohs = 5.5 | luster = Bright metallic to adamantine | refractive = nω=2.35, nε=2.25 | opticalprop = Uniaxial (-) | birefringence = δ = 0.1 | pleochroism = | streak = Chestnut brown | gravity = 8.5–9.63, average = 9.06 | melt = | fusibility = | diagnostic = | solubility = | alteration = tarnishes to dull on exposure | diaphaneity = Subtranslucent to opaque | other = Non-fluorescent, nonmagnetic | references = }} Plattnerite is an oxide mineral and is the beta crystalline form of lead dioxide (β-PbO2), scrutinyite being the other, alpha form. It was first reported in 1845 and named after German mineralogist Karl Friedrich Plattner. Plattnerite forms bundles of dark needle-like crystals on various minerals; the crystals are hard and brittle and have tetragonal symmetry.

==Occurrence== Plattnerite is found in numerous arid locations in North America (US and Mexico), most of Europe, Asia (Iran and Russia), Africa (Namibia) and Southern and Western Australia. It occurs in weathered hydrothermal base-metal deposits as hay-like bundles of dark prismatic crystals with a length of a few millimeters; the bundles grow on, or sometimes within various minerals, including cerussite, smithsonite, hemimorphite, leadhillite, hydrozincite, rosasite, aurichalcite, murdochite, limonite, pyromorphite, wulfenite, calcite and quartz.

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