
mineral
Likely olivine (peridot)
Olivine-group silicate, approximately (Mg,Fe)₂SiO₄
AI-generated identification · may be incorrectSmall, rough yellow-green fragments with a vitreous-to-dull luster; olivine has Mohs hardness 6.5–7, orthorhombic crystals, and poor cleavage. The photo alone cannot confirm the identification or provide reliable specific gravity.
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Physical properties
Small, rough yellow-green fragments with a vitreous-to-dull luster; olivine has Mohs hardness 6.5–7, orthorhombic crystals, and poor cleavage. The photo alone cannot confirm the identification or provide reliable specific gravity.
Formation & geological history
Olivine crystallizes in magnesium-rich igneous rocks, especially basalt and peridotite, and may also occur in meteorites. Its age and exact formation environment cannot be determined from the image.
Uses & applications
Gem-quality olivine is cut as peridot; common material is collected and studied as a rock-forming mineral.
Geological facts
Olivine is a major mineral in Earth’s upper mantle and is commonly altered by weathering into greenish serpentine minerals.
Field identification & locations
Check for glassy luster, hardness near 7, and granular crystals; similar green minerals include epidote and serpentine. Occurs in basalt and peridotite worldwide, including Hawaii, Arizona, and Pakistan.
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