
mineral
Black Spinel
Magnesium Aluminum Oxide (MgAl2O4)
AI-generated identification · may be incorrectHardness: 8.0 on Mohs scale; Color: Opaque black; Luster: Vitreous (glassy); Crystal Structure: Isometric/Cubic; Cleavage: Indistinct; Specific Gravity: 3.54-3.63
- Hardness
- 8
- Color
- Opaque black
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 8.0 on Mohs scale; Color: Opaque black; Luster: Vitreous (glassy); Crystal Structure: Isometric/Cubic; Cleavage: Indistinct; Specific Gravity: 3.54-3.63
Formation & geological history
Formed through contact metamorphism where magmas intrude into aluminous schists or limestones. The finest specimens are often found in metamorphic marbles or as water-worn pebbles in alluvial deposits.
Uses & applications
Primarily used in jewelry as a faceted gemstone. Due to its high hardness and brilliance, it is a popular, natural alternative to black diamond or black tourmaline.
Geological facts
Black Spinel was historically often mistaken for black diamond or magnetite. It is considered one of the rarest colors of spinel, despite being more affordable than the red or blue varieties.
Field identification & locations
Identified in the field by its high hardness (it cannot be scratched by steel) and lack of magnetism compared to magnetite. Found commonly in Thailand, Sri Lanka, Myanmar, and Tanzania. Collectors look for sharp facet edges and a high polish.
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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