
mineral
Olivine (Peridot)
Olivine Group (Mg,Fe)2SiO4
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Olive-green, yellow-green; Luster: Vitreous; Crystal Structure: Orthorhombic; Cleavage: Poor; Specific Gravity: 3.27-4.37.
- Hardness
- 6
- Color
- Olive-green, yellow-green
- Luster
- Vitreous
Identified More mineral →
Explore Olivine (Peridot) in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 6.5-7 Mohs; Color: Olive-green, yellow-green; Luster: Vitreous; Crystal Structure: Orthorhombic; Cleavage: Poor; Specific Gravity: 3.27-4.37.
Formation & geological history
Formed in the Earth's upper mantle and brought to the surface through volcanic activity; commonly found in mafic and ultramafic igneous rocks like basalt and peridotite.
Uses & applications
Used primarily as a gemstone (Peridot) in jewelry. Also used as a refractory material in steel making, as a casting sand, and as an abrasive.
Geological facts
Olivine is one of the most common minerals in Earth's mantle and has also been discovered in lunar rocks and many meteorites (pallasites). Its gem-quality name is Peridot.
Field identification & locations
Identify by its distinctive olive-green color and lack of perfect cleavage. Often found as small, glassy grains in basalt lava or dark volcanic rocks in regions like Arizona or Hawaii.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Mineral Sand (Heavy Mineral Sand Concentrate)
Placer deposit concentrate containing minerals such as ilmenite, rutile, zircon, and magnetite
mineral
Calcite–fluorite mineral specimen with iron-oxide staining
Calcite (CaCO₃), likely fluorite (CaF₂), with possible quartz and iron/manganese oxides
mineral
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Soil with Mineral Detritus and Quartz Fragments
Regolith / Silicate Mineral Aggregate
sedimentary
Schist
Schist
Metamorphic