Pronunciation: [ba͡ɪsmˈɒkla͡ɪt] (IPA) 
Bismoclite is a mineral with the chemical formula (BiO)2CO3. The word is pronounced /ˈbɪzməklaɪt/. The first syllable is stressed, and the "i" in "bi" is pronounced as a short "i" sound, similar to the "i" in "bin". The "s" is pronounced as a voiceless "s" sound, and the "m" is pronounced as a nasal "m" sound. The "o" in "oclite" is pronounced as a long "o" sound, like the "o" in "bone," and the "e" is silent.
Bismoclite is a mineral that is classified as a rare secondary mineral. Chemically, it is composed of lead, bismuth, and chlorine, with the chemical formula PbBiOCl. It usually forms in hydrothermal deposits, resulting from the alteration of primary lead ores containing bismuth minerals.
Bismoclite crystallizes in the orthorhombic crystal system, which means it exhibits a three-dimensional lattice structure with three unequal crystal axes at right angles to each other. It typically forms as small, thin, tabular or prismatic crystals, which are often transparent or translucent. The mineral is also observed in compact or granular aggregates.
In terms of physical properties, bismoclite is characterized by its pearl-like to resinous luster, and it shares a similar color with many other lead-bearing minerals—it ranges from yellowish to greenish-gray. It has a relatively low hardness, typically ranging from 3.5 to 4 on the Mohs scale.
Bismoclite is an interesting mineral for collectors due to its relative scarcity and the unique combination of its chemical composition. As a mineral consisting of lead and bismuth, it showcases the properties and characteristics of both elements. However, due to the scarcity and limited distribution of bismoclite, it does not have any significant commercial applications or uses beyond scientific research and mineralogy.
The word "bismoclite" is derived from the chemical element "bismuth" and the Greek word "klitos", which means inclined or leaning. Bismuth is a chemical element with the symbol Bi and atomic number 83. The term "bismoclite" specifically refers to a bismuth oxychloride mineral. The word's etymology combines the name of the element and the Greek term, reflecting the characteristic inclination or leaning structure of this mineral.
