
mineral
Corundum (Ruby Variety)
Corundum (Al2O3)
AI-generated identification · may be incorrectHardness: 9 on Mohs scale; Color: Pinkish-red (Ruby); Luster: Adamantine to vitreous; Crystal structure: Trigonal/Hexagonal; Cleavage: None (has parting); Specific Gravity: 3.95–4.10
- Hardness
- 9 on Mohs scale
- Color
- Pinkish-red (Ruby)
- Luster
- Adamantine to vitreous
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Physical properties
Hardness: 9 on Mohs scale; Color: Pinkish-red (Ruby); Luster: Adamantine to vitreous; Crystal structure: Trigonal/Hexagonal; Cleavage: None (has parting); Specific Gravity: 3.95–4.10
Formation & geological history
Formed in aluminum-rich metamorphic rocks such as mica schists or gneisses, and certain igneous rocks like syenites. They often concentrate in alluvial deposits due to high density and hardness.
Uses & applications
Abrasives (industrial grade), watch bearings, lasers, and high-end jewelry (gem grade). Rough specimens are highly sought by mineral collectors.
Geological facts
Corundum is the second hardest natural mineral after diamond. Red corundum is called Ruby; all other colors are known as Sapphires.
Field identification & locations
Identify in the field by its distinct hexagonal barrel shape (crystal habit), extreme hardness (it will scratch glass and almost all other minerals), and high density. Commonly found in Myanmar, Sri Lanka, and parts of Madagascar.
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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