
mineral
Black Spinel
Magnesium Aluminum Oxide (MgAl2O4)
AI-generated identification · may be incorrectHardness: 8 (Mohs scale); Color: Black, opaque; Luster: Vitreous (glassy) to submetallic; Crystal system: Isometric (octahedral crystals); Cleavage: None/Indistinct; Specific Gravity: 3.54-3.63
- Hardness
- 8 (Mohs scale)
- Color
- Black, opaque
- Luster
- Vitreous (glassy) to submetallic
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Physical properties
Hardness: 8 (Mohs scale); Color: Black, opaque; Luster: Vitreous (glassy) to submetallic; Crystal system: Isometric (octahedral crystals); Cleavage: None/Indistinct; Specific Gravity: 3.54-3.63
Formation & geological history
Spinel forms as a metamorphic mineral in limestone/dolomite through contact metamorphism. It is also found as a primary mineral in mafic igneous rocks and as water-worn pebbles in alluvial deposits. They can be hundreds of millions of years old.
Uses & applications
Primarily used in jewelry as a more affordable, durable alternative to black diamonds or black sapphires. It is also highly valued by gemstone collectors.
Geological facts
Black Spinel is known for its intense black color and lack of secondary hues. Historically, spinels were often confused with rubies or sapphires (such as the famous 'Black Prince's Ruby' in the British Crown Jewels, which is actually a red spinel).
Field identification & locations
Identify in the field by its high hardness (it will scratch glass), octahedral crystal shape, and lack of cleavage. Common sources include Thailand, Myanmar, Sri Lanka, and Vietnam.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary