
mineral
Celestite (Celestine)
Strontium Sulfate (SrSO4)
AI-generated identification · may be incorrectHardness: 3-3.5 (Mohs); Color: Pale blue to colorless, sometimes white; Luster: Vitreous to pearly; Crystal structure: Orthorhombic; Cleavage: Perfect; Specific gravity: 3.9-4.0
- Hardness
- 3-3
- Color
- Pale blue to colorless, sometimes white
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 3-3.5 (Mohs); Color: Pale blue to colorless, sometimes white; Luster: Vitreous to pearly; Crystal structure: Orthorhombic; Cleavage: Perfect; Specific gravity: 3.9-4.0
Formation & geological history
Formed most commonly in sedimentary rocks (limestones and dolomites) as a result of chemical precipitation from strontium-rich groundwater. It often occurs as geodes or cavity linings within evaporite deposits.
Uses & applications
Primary source of the element strontium, used in the manufacturing of glass for TV screens, fireworks (red flames), and metal alloys. Also popular in the gem and mineral trade for healing and aesthetic display.
Geological facts
The world's largest known geode is a celestite geode located in Put-in-Bay, Ohio, measuring 35 feet at its widest point. The name is derived from the Latin 'caelestis', meaning 'heavenly' or 'celestial', referring to its sky-blue color.
Field identification & locations
Identify in the field by its high density (feels heavy for its size), distinct pale blue color, and rectangular crystal habits. Commonly found in Madagascar, Sicily, and the Lake Erie region of the USA.
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