PAVONITE Meaning and
Definition
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Pavonite is a term used in mineralogy to refer to a rare sulfosalt mineral. It is named after its discovery location in Pavone Val Grande, Italy. Pavonite is composed of three elements: lead, antimony, and sulfur, with the chemical formula PbBi2S4. It is classified as a sulfosalt because of its distinct crystalline structure and its sulfur content.
The mineral is characterized by its metallic luster, typically appearing silver-gray to black in color. It occurs in compact masses or as elongated crystals, which are usually prismatic or acicular in shape. Pavonite is opaque and has a Mohs hardness of 2.5 to 3, making it a relatively soft mineral.
Pavonite is commonly found in hydrothermal veins associated with other minerals such as galena, sphalerite, and chalcopyrite. It forms at relatively low temperatures and high pressures, typically in association with ore deposits. While it is not widely distributed, notable occurrences of pavonite have been reported in various localities around the world, including Italy, Austria, Romania, and the United States.
Due to its scarcity and distinctive crystal structure, pavonite is of interest to mineral collectors and researchers studying mineralogy and geology. Its unique composition and physical properties make it valuable for investigations into the formation of ore deposits and the chemical processes occurring within the Earth's crust.
Etymology of PAVONITE
The word "pavonite" is derived from the Latin word "pavo", meaning "peacock" in English. It is named so due to its resemblance to the iridescent colors seen on a peacock's feathers. "Pavonite" is a reference to the mineral's characteristic bluish-green color, which is reminiscent of the vibrant hues found in peacock feathers.
