
mineral
Black Spinel
Magnesium Aluminum Oxide (MgAl2O4)
AI-generated identification · may be incorrectHardness: 8.0 on Mohs scale; Color: Jet black, opaque; Luster: Vitreous to sub-adamantine; Crystal Structure: Isometric/Cubic (often octahedrons); Cleavage: Indistinct; Specific Gravity: 3.54-3.63.
- Hardness
- 8
- Color
- Jet black, opaque
- Luster
- Vitreous to sub-adamantine
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Physical properties
Hardness: 8.0 on Mohs scale; Color: Jet black, opaque; Luster: Vitreous to sub-adamantine; Crystal Structure: Isometric/Cubic (often octahedrons); Cleavage: Indistinct; Specific Gravity: 3.54-3.63.
Formation & geological history
Formed through contact metamorphism where magmatic intrusions interact with limestone or dolomite. Also found in igneous rocks like basalt. These are often primary deposits or found as water-worn pebbles in alluvial deposits.
Uses & applications
Primarily used in jewelry as a more affordable, durable alternative to black diamonds or black sapphires. Used in faceted stones, beads, and cabochons.
Geological facts
Black spinel is often called the 'Master of Re-energization'. It was historically confused with black tourmaline or onyx, but its superior hardness and brilliance distinguish it as a high-quality gemstone.
Field identification & locations
Identify in the field by its high hardness (it will scratch glass and quartz) and its lack of perfect cleavage. Commonly found in Thailand, Sri Lanka, Myanmar, and Australia.
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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