
mineral
Ruby (Raw Corundum)
Corundum (Al2O3 with Chromium impurities)
Hardness: 9 on Mohs scale; Color: Pinkish-red to deep red; Luster: Adamantine to vitreous; Crystal Structure: Hexagonal/Trigonal (often found as flat hexagonal plates); Cleavage: None (has parting); Specific Gravity: 3.97-4.05.
- Hardness
- 9 on Mohs scale
- Color
- Pinkish-red to deep red
- Luster
- Adamantine to vitreous
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Physical properties
Hardness: 9 on Mohs scale; Color: Pinkish-red to deep red; Luster: Adamantine to vitreous; Crystal Structure: Hexagonal/Trigonal (often found as flat hexagonal plates); Cleavage: None (has parting); Specific Gravity: 3.97-4.05.
Formation & geological history
Formed in aluminum-rich metamorphic rocks such as marble or schist, and in igneous environments like syenites. They are found in deposits ranging from Precambrian to more recent alluvial gravels.
Uses & applications
Used primarily as a gemstone in jewelry. Industrial uses include lasers, watches (bearings), and high-durability optical windows.
Geological facts
Ruby is the red variety of Corundum; any other color is called Sapphire. It is the second hardest natural material after diamond. Its red color is caused specifically by the presence of chromium.
Field identification & locations
Identify in the field by its distinct hexagonal crystal habit and its extreme hardness (will scratch almost any other mineral). Common locations include Myanmar, Sri Lanka, Thailand, and Madagascar.
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