Mineral species: Olivine (gem peridot)
Mineral group: Olivine group
Chemical formula: Magnesium iron silicate [(Mg,Fe)2SiO4]
Mohs hardness: 6.75
Crystal system: Orthorhombic
Lustre: vitreous
Transparency: transparent
Streak: White
Cleavage: Poor
Fracture: Conchoidal to uneven
Specific gravity: 3.27-3.37
Refractive index: 1.65-1.69
Optical phenomena: None commonly reported
Colour range: Green, Brown
Common inclusions: Lily-pad stress inclusions, crystals, and fracture features
Geological environment: Peridot occurs in Mantle-derived igneous rocks and basaltic volcanic environments. Its Orthorhombic structure reflects the pressure-temperature conditions of those host rocks, with notable occurrences in Pakistan (Kohistan), China, Myanmar, Vietnam, Arizona (USA).
Principal mining regions: Pakistan (Kohistan), China, Myanmar, Vietnam, Arizona (USA)
Important commercial sources: Current commercial production includes Pakistan, China, Myanmar, and Arizona (USA)
Historical significance: Peridot has been used as a gem since antiquity and remains a major green jewelry stone.
Common treatments: Generally untreated in trade.
Synthetic or imitation forms: Glass and synthetic substitutes can imitate peridot color.
Common look-alikes: topaz, moonstone, tanzanite
Jewellery uses: Peridot is used chiefly for A good fit for collectors and jewellers looking for visible character without needing the highest hardness category.. In the trade it is commonly fashioned as faceted stones, calibrated cuts, and higher-clarity collector pieces, with Mohs hardness 6.75 guiding suitable jewellery applications.
Care recommendations: Peridot should be cleaned with lukewarm water, mild soap, and a soft brush. At Mohs 6.75 in the Orthorhombic system, avoid steam cleaners, harsh chemicals, and high-impact wear. Protect cleavage directions from sharp knocks during wear and setting.