THE MINERAL MASSICOT
- Chemical Formula: PbO, Lead Oxide
- Class: Oxides and Hydroxides
- Uses: As a minor ore of lead, a pigment and as mineral specimens.
- Specimens
Massicot, which has been known by the chemically descriptive term of "lead monoxide", is an oxidation product of other lead minerals. It forms under oxidizing conditions of lead ore bodies and its presence is very indicative of the degree of oxidation. Something of interest to petrologists (rock scientists). It is probably more common than is known as it exists as a slight yellowish coating on many lead specimens, often to the detriment of the aesthetic appeal of the underlying mineral.
Massicot is the
orthorhombic variety of
PbO.
The tetragonal variety is the mineral
THE PHYSICAL CHARACTERISTICS OF MASSICOT:
- Color is yellow to reddish yellow due to minium inclusions.
- Luster is greasy, earthy to dull.
- Transparency: Crystals are generally opaque, but thin scales can be transparent.
- Crystal System is orthorhombic; 2 2 2.
- Crystal Habits include massive, earthy and scaly coatings on other lead minerals.
- Cleavage is distinct in two perpendicular directions, but is rarely seen.
- Fracture is uneven.
- Hardness is 2.
- Specific Gravity is 9.6 - 9.7 (Well above average for any mineral)
- Streak is light yellow.
- Associated Minerals include minium, galena, barite, wulfenite, pyromorphite, mimetite, bindheimite, cerussite, lead and sphalerite.
- Notable Occurrences include Freiberg,
Saxony , Germany as well as in Inyo County, California; at the Dogwater Mine, Graham County; Tonopah-Belmont Mine, Maricopa County and Cababi District, Arizona; Potosi, Missouri and at Leadville, Colorado, USA; Sardinia, Italy; Mexico; Hungary; and atLavrion , Greece.
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