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Dumortierite is related to several other nesosilicate boro-silicates such as grandidierite, harkerite, holtite, kornerupine, magnesiodumortierite, prismatine and werdingite. Dumortierite is far more common than all of these. In fact, it is the most common boro-silicate with the exception of the more common members of the Tourmaline Group. Dumortierite is commonly found in aluminum rich metamorphic rocks in contact metamorphic regions and in some pegmatites. It can alter to the mineral pyrophyllite. Dumortierite is named for the French paleontologist, Eugene Dumortier.
PHYSICAL CHARACTERISTICS:
Color is typically blue to violet, but also pink and brown.
Luster is vitreous to dull.
Transparency: Crystals are translucent to transparent, massive specimens are nearly opaque.
Crystal System is orthorhombic; 2/m 2/m 2/m.
Crystal Habits include prismatic crystals but more commonly massive, columnar and fibrous.
Cleavage good in one direction and poor in four others, but rarely seen.
Fracture is uneven to hackly.
Hardness is 7 - 8.5
Specific Gravity is 3.3 - 3.4
Streak is bluish white.
Other Characteristics: Crystals are pleochroic from red to blue to violet. Some specimens fluoresce a blue color under longwave UV light with a fluorescent yellow matrix and a few specimens from Oreana, Nevada have fluoresced white under shortwave UV light. Associated Minerals are numerous and include quartz, kyanite, sillimanite, staurolite, andalusite, muscovite, lazulite and pyrophyllite
Notable Occurrences include the type locality of Beaunan, France as well as Quartzite, La Paz County, Arizona; Colorado; Oreana, Nevada; New York, New York and Alpine, San Diego County and Los Angeles County, California, USA; Magadanskaya, Siberia, Russia and Sahatany, Madagascar.
Best Field Indicators include hardness, color, density, fluorescence, fibrous crystal habit and environment.
