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  1. Galena - Wikipedia

    Galena is one of the most abundant and widely distributed sulfide minerals. It crystallizes in the cubic crystal system often showing octahedral forms. It is often associated with the minerals sphalerite, …

  2. Galena Mineral | Uses and Properties - Geology.com

    What is Galena? Galena is a lead sulfide mineral with a chemical composition of PbS. It is the world's primary ore of lead and is mined from a large number of deposits in many countries. It is found in …

  3. Visit Galena, IL: Things to Do, Events & Hotels | Galena Country

    Discover the charm of Galena Country in Illinois! Plan your getaway to Galena today to experience local flavor, rich history, rolling vineyards and more.

  4. Galena (Lead Ore) : Properties, Occurrence, Formation and Uses

    Apr 28, 2018 · Galena, a mineral of both historical and geological significance, is a lead sulfide mineral with the chemical formula PbS. It stands out with its distinctive metallic luster and cubic crystal …

  5. Galena | Lead sulfide, Lead ore, Silver ore | Britannica

    galena, a gray lead sulfide (PbS), the chief ore mineral of lead.

  6. Galena: Mineral information, data and localities. - mindat.org

    Galena is the primary ore mineral of lead.

  7. Galena: The mineral galena information and pictures

    Detailed description, properties and locality information guide about the lead ore mineral galena.

  8. How Is Galena Formed? From Hydrothermal to Sedimentary

    4 days ago · Galena is the natural mineral form of lead (II) sulfide, chemically represented as PbS. It serves as the most important ore for lead and is often mined for its silver content, which can …

  9. Galena – Mineral Properties, Photos and Occurrence

    Apr 1, 2019 · Galena, historically also named lead glance, is among the most abundant sulfides. Besides forming aesthetic mineral specimens, galena is the primary lead ore. And galena itself was a …

  10. Galena | Common Minerals

    Galena is the most abundant lead mineral, has been mined for millennia, and remains our major source of that metal. It is a metallic, lead-gray mineral with cubic cleavage and a distinctly high density that …