Cerussite

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Cerussite
Sample of cerussite-bearing quartzite
General
Category	Carbonate mineral
Chemical formula	Lead carbonate: PbCO₃
Identification
Color	Colorless, white, gray, blue, or green
Crystal habit	Massive granular, reticulate, tabular to equant crystals
Crystal system	Orthorhombic - Dipyramidal (2/m 2/m 2/m)
Twinning	Simple or cyclic contact twins
Cleavage	Good [110] and [021]
Fracture	Brittle conchoidal
Mohs Scale hardness	3 to 3.5
Luster	Adamantine, vitreous, resinous
Refractive index	nα = 1.803 nβ = 2.074 nγ = 2.076
Optical Properties	Biaxial (-)
Birefringence	δ = 0.273
Streak	White
Specific gravity	6.53 - 6.57
Diaphaneity	Transparent to translucent
Other Characteristics	May fluoresce yellow under LW UV
References	^[1]^[2]

Cerussite (also known as lead carbonate or white lead ore) is a mineral consisting of lead carbonate (PbCO₃), and an important ore of lead. The name is from the Latin cerussa, white lead. Cerussa nativa was mentioned by K Gesner in 1565, and in 1832 F. S. Beudant applied the name cruse to the mineral, whilst the present form, cerussite, is due to W. Haidinger (1845). Miners' names in early use were lead-spar and white-lead-ore.

Cerussite crystallizes in the orthorhombic system and is isomorphous with aragonite. Like aragonite it is very frequently twinned, the compound crystals being pseudo-hexagonal in form. Three crystals are usually twinned together on two faces of the prism, producing six-rayed stellate groups with the individual crystals intercrossing at angles of nearly 60°. Crystals are of frequent occurrence and they usually have very bright and smooth faces. The mineral also occurs in compact granular masses, and sometimes in fibrous forms. The mineral is usually colorless or white, sometimes grey or greenish in tint and varies from transparent to translucent with an adamantine lustre. It is very brittle, and has a conchoidal fracture. It has a Mohs hardness of 3 to 3.75 and a specific gravity of 6.5. A variety containing 7 % of zinc carbonate, replacing lead carbonate, is known as iglesiasite, from Iglesias in Sardinia, where it is found.

The mineral may be readily recognized by its characteristic twinning, in conjunction with the adamantine lustre and high specific gravity. It dissolves with effervescence in dilute nitric acid. A blowpipe test will cause it to fuse very readily, and gives indications for lead.

As crystaline ore

Finely crystallized specimens have been obtained from the Friedrichssegen mine near Ems in Nassau, Johanngeorgenstadt in Saxony, Mies in Bohemia, Phenixville in Pennsylvania, Broken Hill, New South Wales; and several other localities. Delicate acicular crystals of considerable length were found long ago in the Pentire Glaze mine near St Minver in Cornwall. It is often found in considerable quantities, and contains as much as 77.5% of lead.

Lead(II) carbonate is practically insoluble in neutral water (solubility product [Pb²⁺][CO₃^2-] ≈ 1.5x10^-13 at 25 °C), but will dissolve in dilute acids.

"White lead" is the key ingredient in the (now discontinued) lead paints. Ingestion of lead-based paint chips is the most common cause of lead poisoning in children.^[3]

Both "white lead" and lead acetate have been used in cosmetics throughout history, though this practice has ceased in Western Countries.^[4]