Smithsonite - Wikipedia Smithsonite, also known as zinc spar, is the mineral form of zinc carbonate (Zn CO 3) Historically, smithsonite was identified with hemimorphite before it was realized that they were two different minerals
Smithsonite: properties, color, crystals, uses, gemstone What is Smithsonite? Smithsonite is a zinc carbonate mineral with a chemical composition of ZnCO 3 Today it is a minor ore of zinc, but in the early days of metallurgy it was one of the most important ores Typical smithsonite colors are brown, gray, white, green, and yellow
Smithsonite Meanings and Crystal Properties Smithsonite, also known as Zinc Spar, is a zinc carbonate mineral that is most commonly found in botryoidal, masses (sometimes with a druzy surface), and stalactites
Smithsonite | Properties, Formation, Occurrence» Geology Science Smithsonite is a mineral that belongs to the carbonate group It is named after James Smithson, an English scientist and mineralogist who was the founder of the Smithsonian Institution in the United States
Smithsonite: Mineral information, data and localities. Calcite Group Siderite-Smithsonite Series Smithsonite is often found as a secondary mineral in the oxidation zone of zinc ore deposits It can also be observed in sedimentary deposits and as a direct oxidation product of sphalerite Visit gemdat org for gemological information about Smithsonite
Smithsonite Gemstone: Properties, Meanings, Value More Smithsonite is a joy-inducing, colorful gem! Learn all about what smithsonite stone is, including its uses, history, and how to get your own in our Smithsonite Gemstone Guide
Smithsonite: The Colorful Zinc Carbonate Mineral with a Rich History . . . Smithsonite, also known as zinc spar, is a captivating mineral treasured for its soft colors and smooth, grape-like formations Though often overlooked in the world of gemstones, this zinc carbonate mineral holds a unique place in history, science, and collector circles
Smithsonite: Meanings, Properties, Facts and More What Is Smithsonite? Smithsonite is a mineral that is typically white but it occurs in many different colors, including, pink, blue, green, yellow, and brown It is typically found as botryoidal, globular, or stalactitic masses in the cavities and fissures of hydrothermal or sedimentary rocks