Rock Identifier
Likely olivine (peridot) (Olivine-group silicate, approximately (Mg,Fe)₂SiO₄) — mineral
mineral

Likely olivine (peridot)

Olivine-group silicate, approximately (Mg,Fe)₂SiO₄

AI-generated identification · may be incorrect

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.

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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.