Plattnerite
From Wikipedia, the free encyclopedia
| Plattnerite | |
|---|---|
 | |
| General | |
| Category | Oxide minerals |
| Formula | PbO2 |
| IMA symbol | Ptn[1] |
| Strunz classification | 4.DB.05 |
| Crystal system | Tetragonal |
| Crystal class | Ditetragonal dipyramidal (4/mmm) H–M Symbol: (4/m 2/m 2/m) |
| Space group | P42/mnm |
| Unit cell | a = 4.95 Å, c = 3.38 Å; Z = 2 |
| Identification | |
| Formula mass | 239.20 g/mol |
| Color | Dark brown, iron-black |
| Crystal 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 scale hardness | 5.5 |
| Luster | Bright metallic to adamantine |
| Streak | Chestnut brown |
| Diaphaneity | Subtranslucent to opaque |
| Specific gravity | 8.5–9.63, average = 9.06 |
| Optical properties | Uniaxial (-) |
| Refractive index | nω=2.35, nε=2.25 |
| Birefringence | δ = 0.1 |
| Alters to | tarnishes to dull on exposure |
| Other characteristics | Non-fluorescent, nonmagnetic |
| References | [2][3][4] |
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.
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,[5] including cerussite, smithsonite, hemimorphite, leadhillite, hydrozincite, rosasite, aurichalcite, murdochite, limonite, pyromorphite, wulfenite, calcite and quartz.[3]
