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CERUSSITE
, a See also:mineral consisting of See also:lead carbonate (PbCO3), and an important ore of lead
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The name (sometimes erroneously spelt cerusite) is from the See also:Lat. cerussa, " See also: Crystals are of frequent occurrence, and they usually have very See also:bright and smooth faces . The mineral also occurs in compact granular masses, and sometimes in fibrous forms . It is usually colourless or white, sometimes See also:grey or greenish in tint; it varies from transparent to translucent, and has an adamantine lustre . It is very brittle, and has a conchoidal fracture . Hardness 3-32; sp. gr . 6.5 . A variety containing 7% of See also:zinc carbonate, replacing lead carbonate, is known as iglesiasite, from See also:Iglesias in See also:Sardinia, where it is found . The mineral may be readily recognized by its characteristic twinning, in See also:conjunction with the adamantine lustre and high specific gravity . It dissolves with effervescence in dilute nitric See also:acid . Before the See also:blow- See also:pipe it fuses very readily, and gives reactions for lead . Cerussite occurs in metalliferous See also:veins in association with See also:galena, and has been formed by the See also:action of carbonated See also:waters on the galena: it is therefore found in the upper parts of the lodes FIG . 2 .
together with other secondary minerals, such as See also:limonite
.
Finely crystallized specimens have been obtained from the Friedrichssegen mine near See also:Ems in See also:Nassau, Johanngeorgenstadt in See also:Saxony, Mies in Bohemia, Phenixville in See also:Pennsylvania, Broken See also: |
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