Parti Sapphire
Corundum (Al2O3)
Rock Type: mineral

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.
Identified on: 5/3/2026
Mode: Standard