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hematite |
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hematite (hĕm`ətīt), mineral, an oxide of iron, Fe2O3, containing about 70% metal, occurring in nature in red to reddish-brown earthy masses and in steel-gray to black crystalline forms. Hematite that has a metallic luster is called specular hematite, or specular iron. The red powdered hematite is used as a pigment (ocher ocher (ō`kər), mixture of varying proportions of iron oxide and clay, used as a pigment . ..... Click the link for more information. ) and as rouge in polishing. Hematite is the most important ore of iron. Extensive and richly productive deposits occur in the Lake Superior region (Michigan, Minnesota, and Wisconsin) and the Birmingham district (Alabama). The mineral is widely distributed throughout the world and is responsible for the red coloration of many sedimentary rocks. See limonite limonite (līm`ənīt) or brown hematite ..... Click the link for more information. . hematiteor haematiteHeavy and relatively hard oxide mineral, ferric oxide (Fe2O3), that constitutes the most important iron ore because of its high iron content and its abundance. Much hematite (from the Greek word meaning “blood,” for its red colour) occurs in a soft, fine-grained, earthy form called red ocher or ruddle. Red ocher is used as a paint pigment; a purified form, rouge, is used to polish plate glass. The world's largest production comes from the Hamersley Range in western Australia. hematite [′hē·mə‚tīt] (mineralogy) Fe2O3An iron mineral crystallizing in the rhombohedral system; the most important ore of iron, it is dimorphous with maghemite, occurs in black metallic-looking crystals, in reniform masses or fibrous aggregates, or in reddish earthy forms. Also known as bloodstone; red hematite; red iron ore; red ocher; rhombohedral iron ore. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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| 005 Bleached hematitic siltstone ------------------------------------------------------- HC05-1 300 305 5 1. Strong argillic and hematitic alteration was observed at approximately 845 feet when the hole passed from upper-plate chert into carbonate rocks presumed to be part of the lower plate assemblage. Veins cut in the trenching and drilling comprise vein breccias with strong silicification, hematitic gossans, and oxide copper minerals. |
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