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Litharge (from Greek , 'stone' + 'silver' ) is one of the natural mineral forms of lead(II) oxide, PbO. Litharge is a secondary mineral which forms from the oxidation of galena ores. It forms as coatings and encrustations with internal tetragonal crystal structure. It is dimorphous with the yellow orthorhombic form massicot. It forms soft (Mohs hardness of 2), red, greasy-appearing crusts with a very high specific gravity of 9.14–9.35. PbO may be prepared by heating lead metal in air at approximately 600 °C (lead melts at only 300 °C). At this temperature it is also the end product o

Key facts

Mineral.name
Litharge
Mineral.image
Litharge.jpg
Mineral.category
Oxide minerals
Mineral.formula
PbO
Mineral.IMAsymbol
Lit
Mineral.strunz
4.AC.20
Mineral.system
Tetragonal
Mineral.class
Ditetragonal dipyramidal (4/mmm) H-M symbol: (4/m 2/m 2/m)
Mineral.symmetry
P4/nmm
Mineral.color
red
Mineral.cleavage
Distinct/Good. On {110}
Mineral.mohs
2
Mineral.luster
greasy, dull
Mineral.diaphaneity
transparent

via Wikipedia infobox

Wikidata facts

Image
Litharge.jpg
Show 6 more facts
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
4.AC.20
chemical formula
PbO
Nickel-Strunz 9th edition (updated 2009)
4.AC.20
Commons category
Litharge
IMA Mineral Symbol
Lit
Strunz 8th edition (series ID, updated)
IV/A.07
Sources (1)

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~3 min read

Article

5 sections
Contents
  • Historical terminology
  • Litharge smelting
  • References
  • Further reading
  • External links

{{Infobox mineral | name = Litharge | boxwidth = | boxbgcolor = | image = Litharge.jpg | imagesize = | alt = | caption = | category = Oxide minerals | formula = PbO | IMAsymbol = Lit | molweight = | strunz = 4.AC.20 | system = Tetragonal | class = Ditetragonal dipyramidal (4/mmm) H-M symbol: (4/m 2/m 2/m) | symmetry = P4/nmm | unit cell = | color = red | colour = | habit = | twinning = | cleavage = Distinct/Good. On {110} | fracture = | tenacity = | mohs = 2 | luster = greasy, dull | streak = | diaphaneity = transparent | gravity = | density = | polish = | opticalprop = | refractive = | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = }} Litharge (from Greek , 'stone' + 'silver' ) is one of the natural mineral forms of lead(II) oxide, PbO. Litharge is a secondary mineral which forms from the oxidation of galena ores. It forms as coatings and encrustations with internal tetragonal crystal structure. It is dimorphous with the yellow orthorhombic form massicot. It forms soft (Mohs hardness of 2), red, greasy-appearing crusts with a very high specific gravity of 9.14–9.35. PbO may be prepared by heating lead metal in air at approximately 600 °C (lead melts at only 300 °C). At this temperature it is also the end product of heating of other lead oxides in air. This is often done with a set of bellows pumping air over molten lead and causing the oxidized product to slip or fall off the top into a receptacle, where it quickly solidifies in minute scales. PbO2 –(293 °C)→ Pb12O19 –(351 °C)→ Pb12O17 –(375 °C)→ Pb3O4 –(605 °C)→ PbO

==Historical terminology== Historically, the term litharge has been combined to refer to other similar substances. For example, litharge of gold is litharge mixed with red lead, giving it a red color; litharge of bismuth is a similar result of the oxidation of bismuth; and litharge of silver is litharge that comes as a by-product of separating silver from lead. In fact, litharge originally meant the mineral residue from silver refining. The term has also been used as a synonym for white lead or red lead.

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