Rock Identifier
Ruby (Raw Corundum) (Corundum (Al2O3 with Chromium impurities)) — mineral
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
Identified More mineral

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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.