
mineral
Dumortierite Quartz
Al7BO3(SiO4)3O3 (Aluminum borate silicate)
AI-generated identification · may be incorrectHardness: 7.0 to 8.5 (aggregate); Color: Deep blue, violet-blue, or grayish-blue; Luster: Vitreous to dull; Crystal structure: Orthorhombic; Cleavage: Good; Specific gravity: 3.26 to 3.50
- Hardness
- 7
- Color
- Deep blue, violet-blue, or grayish-blue
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7.0 to 8.5 (aggregate); Color: Deep blue, violet-blue, or grayish-blue; Luster: Vitreous to dull; Crystal structure: Orthorhombic; Cleavage: Good; Specific gravity: 3.26 to 3.50
Formation & geological history
Formed in high-temperature aluminum-rich regional metamorphic rocks, specifically pegmatites and metamorphic schists. Most specimens date from the Late Proterozoic to Phanerozoic eras.
Uses & applications
Used primarily in lapidary work for cabochons and beads, as well as in the production of high-grade spark plug porcelain and electrical insulators due to its high aluminum content.
Geological facts
Often mistaken for Sodalite or Lapis Lazuli, but it is significantly harder and lacks the brassy pyrite inclusions common in Lapis. It was named after the French paleontologist Eugène Dumortier.
Field identification & locations
Identify in the field by its distinct waxy to vitreous luster and its resistance to scratching by a steel file. Commonly found in Brazil, Namibia, Madagascar, and the United States (California/Nevada). Collectors look for deep even color saturation.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary