
mineral
Black Spinel
Magnesium Aluminum Oxide (MgAl2O4)
AI-generated identification · may be incorrectHardness: 8 on Mohs scale; Color: Jet black; Luster: Vitreous (glassy); Crystal Structure: Isometric (cubic/octahedral); Cleavage: Indistinct; Specific Gravity: 3.54-3.63
- Hardness
- 8 on Mohs scale
- Color
- Jet black
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 8 on Mohs scale; Color: Jet black; Luster: Vitreous (glassy); Crystal Structure: Isometric (cubic/octahedral); Cleavage: Indistinct; Specific Gravity: 3.54-3.63
Formation & geological history
Formed primarily as a metamorphic mineral in limestone or as a primary mineral in mafic igneous rocks. It is also common in alluvial deposits after weathering out of harder matrix rocks.
Uses & applications
Used almost exclusively in the jewelry industry as a durable and affordable alternative to black diamonds or black sapphires. It is highly valued for its high refractive index and deep black color.
Geological facts
Black Spinel was often mistaken for black diamond or tourmaline in antiquity. It is one of the hardest minerals and is remarkably stable under high heat and chemical exposure. Famous red 'rubies' in royal crowns are often actually Spinels.
Field identification & locations
Identified in the field by its distinct octahedral crystal habit when found in matrix, and its extreme hardness which prevents scratching by steel. Common locations include Thailand, Sri Lanka, and Myanmar.
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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