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Brookite

General Information

Brookite is a polymorph with two other minerals. Rutile, anatase and brookite all have the same chemistry, TiO2, but they have different structures. At higher temperatures, about 1023.15 Kelvin, brookite will revert to the rutile structure. Rutile is the more common and the more well known mineral of the three. Brookite shares many properties with rutile (i.e., color and luster). However, due to structural differences, brookite and rutile differ in crystal habit and cleavage.
Chemistry: TiO2, Titanium Oxide Class: Oxides and Hydroxides Subclass: Color: Dark Brown to Greenish Black, Dark Blue Streak: Light Brown Luster: Submetallic
Transparency: Opaque Crystal System: Orthorhombic Hardness: 5.5-6 Cleavage: Poor prismatically and in the basal direction Fracture: Subconchoidal and Uneven Specific Gravity: 3.9-4.1
Crystal Habits: Tabular to platy crystals with a pseudohexagonal outline. Magnet Cove specimens tend to be more equant with complex facets Uses: Minor ore of titanium and as mineral specimens Associated Minerals: Anatase, Rutile, Quartz, Feldspars, Chalcopyrite, Hematite, Sphene Other Characteristics: Sometimes intergrown with staurolite Notable Occurrences: Magnet Cove, Arkansas; Butte, Montana; Somerville, Massachusetts; Ellenville, New York, USA; Eicham, Austria; Tremadoc, Wales, England; Ural Mountains, Russia; St. Gotthard, Switzerland Best Field Indicators: Crystal habit, Luster, Density, Streak, Associations and Locality


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