
mineral
Parti Sapphire
Corundum (Al2O3)
AI-generated identification · may be incorrectHardness: 9.0 on Mohs scale; Color: Multi-colored (green, blue, yellow in one stone); Luster: Adamantine to vitreous; Crystal structure: Trigonal; Specific gravity: 3.98-4.06
- Hardness
- 9
- Color
- Multi-colored (green, blue, yellow in one stone)
- Luster
- Adamantine to vitreous
Identified More mineral →
Explore Parti Sapphire in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 9.0 on Mohs scale; Color: Multi-colored (green, blue, yellow in one stone); Luster: Adamantine to vitreous; Crystal structure: Trigonal; Specific gravity: 3.98-4.06
Formation & geological history
Formed in metamorphic or igneous rocks (such as basalt-related deposits) under high pressure and temperature. Colors are created by trace elements like iron and titanium in variable concentrations within a single crystal.
Uses & applications
Primary use is in high-end jewelry and as a gemstone for collectors; sapphire varieties are also used in industrial abrasive applications and watch crystals.
Geological facts
Parti sapphires are unique because they cannot be replicated by synthetic processes to look natural; each stone's color zoning is as unique as a fingerprint.
Field identification & locations
Identify by 'color zoning' (visible bands of different colors), extreme hardness, and lack of cleavage. Commonly found in Australia (Queensland and NSW), Nigeria, and Madagascar.
More like this
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