Olive-green olivine grains in a dark igneous rock specimen with vitreous to oily sparkle
Also known as: Forsterite-fayalite series, Chrysolite, Peridot parent mineral
CommonMineralOlivine group silicate; commonly a forsterite-rich member of the forsterite-fayalite solid-solution series
Hardness6.5-7
Crystal SystemOrthorhombic
Density3.2-4.4 g/cm³, increasing with iron content
LusterVitreous to oily
Formula(Mg,Fe)2SiO4; forsterite Mg2SiO4 to fayalite Fe2SiO4
ColorsOlive green, Yellow-green, Bottle green, Brownish green, Yellow, Brown, Nearly black

What Is Olivine?

Olivine is a common olive-green to yellow-green magnesium-iron nesosilicate and a major rock-forming mineral in Earth’s mantle. In most hand specimens it appears as glassy, sugary green grains in basalt, gabbro, peridotite, or dunite rather than as showy isolated crystals.

Collectors often meet olivine in two very different forms: ordinary granular rock material and transparent gem-quality peridot. Fresh surfaces can look vitreous to slightly oily, with colors from bottle green and yellow-green to brownish green; darker iron-rich material may approach brown or nearly black.

Origin & History

The name olivine directly refers to the mineral’s typical olive-green color. It was introduced in the late 18th century and is commonly credited to Abraham Gottlob Werner, giving a modern mineral name to a material whose gem variety had already been prized for a very long time.

Peridot, the transparent gem form of olivine, has been used since antiquity, especially from the historic Red Sea locality on Zabargad Island, Egypt. For checking locality names and mineral records, mindat.org is a useful plain-text reference alongside specimen labels and museum catalog information.

Where Is Olivine Found?

Olivine is found worldwide in mafic and ultramafic igneous rocks, especially basalt, gabbro, peridotite, and dunite. It is also known from some volcanic sands and from certain meteorites, including pallasites and chondrites, making it important to both field collectors and planetary-material collectors.

San Carlos Apache Reservation, Arizona, USA Zabargad Island, Red Sea, Egypt Sapat Gali, Kohistan District, Pakistan Mogok, Mandalay Region, Myanmar Eifel volcanic field, Germany Lanzarote, Canary Islands, Spain Åheim and Almklovdalen, Norway Hawaii, USA

Formation

Olivine forms at high temperatures from magnesium- and iron-rich magmas. It is especially abundant in mantle-derived rocks such as peridotite and dunite, and it also crystallizes in basalt and gabbro, where it may stand out as green granular crystals against darker rock.

At Earth’s surface, olivine weathers relatively easily over geologic time. Moist, acidic, or hydrothermal conditions can alter it to serpentine, iddingsite, iron oxides, and clay minerals, so fresh green grains are usually more desirable to collectors than crumbly brown altered patches.

How to Identify Olivine

Identify olivine by looking for olive-green to yellow-green glassy grains, commonly in basalt, peridotite, or dunite. It has a Mohs hardness of about 6.5-7, a white to colorless streak, no obvious cleavage, and a conchoidal to uneven brittle fracture.

In the hand, olivine usually looks granular and sparkly rather than long and prismatic. It can be separated from epidote by its lack of strong cleavage, and from pyroxene by its greener color and more sugary granular habit; iron-rich pieces may be darker and only very weakly magnetic.

Properties of Olivine

Physical Properties

Crystal SystemOrthorhombic
Hardness (Mohs)6.5-7 (Hard)
Density3.2-4.4 g/cm³, increasing with iron content
LusterVitreous to oily
DiaphaneityTransparent to translucent; commonly translucent in rock-forming grains
FractureConchoidal to uneven; brittle
StreakWhite to colorless
MagnetismUsually nonmagnetic; iron-rich varieties may show very weak magnetic response
ColorsOlive green, Yellow-green, Bottle green, Brownish green, Yellow, Brown, Nearly black

Chemical Properties

ClassificationNesosilicate
Formula(Mg,Fe)2SiO4; forsterite Mg2SiO4 to fayalite Fe2SiO4
ElementsMagnesium, Iron, Silicon, Oxygen
Common ImpuritiesNickel, Manganese, Calcium, Chromium, Aluminum

Optical Properties

Refractive IndexApproximately 1.63-1.88, depending on Mg-Fe composition
BirefringenceAbout 0.035-0.052
PleochroismNone to weak; iron-rich material may show weak yellow-green to greenish-brown pleochroism
Optical CharacterBiaxial positive or biaxial negative depending on composition

Olivine Health & Safety

Olivine is not considered toxic for normal handling. The main risk is inhaling mineral dust when cutting, grinding, or polishing, especially from mixed rock specimens that may contain other silicates.

Safe to HandleYes
Safe in WaterYes
ToxicNo
Dust HazardYes

Olivine Value & Price

Collection Score
4
Popularity
4
Aesthetic
4
Rarity
2
Sci-Cultural Value
5

Price Range

Rough/Tumbled: Common olivine-bearing rock specimens are often inexpensive, roughly $2-$30. Attractive peridot crystals or mantle xenolith specimens may range from about $20-$300+, with fine gem crystals or historic-locality specimens higher.

Cut/Polished:

Value depends on whether the specimen is ordinary rock-forming olivine, gem-quality peridot, or a scientifically interesting mantle xenolith or meteorite occurrence. Color, transparency, crystal form, locality, size, and freshness are important; weathered brown olivine is less desirable.

Durability

Good for specimens; moderate for jewelry when gem-quality — Scratch resistance: Hard enough to resist many everyday scratches, but not as hard as corundum or topaz., Toughness: Fair to good; brittle and can chip along fractures.

Stable under normal indoor conditions, but olivine can alter or weather over geologic time, especially in moist, acidic, or hydrothermal environments. Avoid harsh acids and prolonged soaking of fractured specimens.

How to Care for Olivine

Use & Storage

Store olivine and peridot specimens separately from softer minerals and protect transparent crystals from knocks and abrasion.

Cleaning

Clean with lukewarm water, mild soap, and a soft brush. Dry thoroughly after rinsing.

Cleanse & Charge

For metaphysical use, cleanse with gentle smoke, sound, or brief running water, and charge in indirect sunlight or on a dry quartz cluster.

Placement

Display away from high-humidity environments if the specimen is altered or crumbly. Transparent peridot crystals look best under soft, bright lighting.

Caution

Avoid ultrasonic cleaners, steam cleaning, strong acids, and hard impacts. Do not soak fragile matrix specimens for long periods.

Works Well With

Olivine Meaning & Healing Properties

In modern crystal healing traditions, olivine and peridot are associated with renewal, growth, confidence, warmth, prosperity, and emotional release. These meanings are cultural and spiritual beliefs, not scientifically proven effects, but many collectors choose olivine for its bright green, forward-moving feel.

Metaphysical users commonly connect olivine with the Heart and Solar Plexus chakras, and with Leo, Virgo, and Libra. For ritual care, use gentle smoke, sound, brief running water, indirect sunlight, or a dry quartz cluster; avoid harsh acids, steam, ultrasonic cleaners, and long soaking of fragile matrix pieces.

Qualities
RenewalGrowthConfidenceWarmthProsperity
Zodiac Signs
Planets
Elements

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Olivine FAQ

What is Olivine?
Olivine is a magnesium-iron nesosilicate mineral with the formula (Mg,Fe)2SiO4. It is a major rock-forming mineral in Earth’s mantle and commonly occurs as olive-green grains in basalt, gabbro, peridotite, and dunite.
Is Olivine rare?
Olivine as a mineral is common, especially in mafic and ultramafic rocks. Gem-quality transparent olivine, known as peridot, is more selective in value and appeal, especially when color, clarity, crystal form, and locality are strong.
What chakra is Olivine associated with?
In modern crystal healing traditions, olivine and peridot are associated with the Heart and Solar Plexus chakras. These associations are spiritual beliefs rather than scientifically proven effects.
Is Olivine safe in water?
Fresh olivine is generally safe to rinse briefly in water, and it can be cleaned with lukewarm water, mild soap, and a soft brush. Avoid prolonged soaking of fractured, altered, or matrix specimens because moisture may loosen grains or encourage deterioration.
How do you cleanse and charge Olivine?
For metaphysical use, cleanse olivine with gentle smoke, sound, or brief running water. Charge it in indirect sunlight or on a dry quartz cluster, and avoid steam, ultrasonic cleaners, strong acids, and long soaking.
What zodiac signs are linked with Olivine?
Olivine and peridot are commonly linked with Leo, Virgo, and Libra in modern crystal traditions. The listed planetary associations are the Sun and Mercury, with Earth and Fire as related elements.
How much is Olivine worth?
Common olivine-bearing rock specimens are often inexpensive, roughly $2-$30. Attractive peridot crystals or mantle xenolith specimens may range from about $20-$300+, while fine gem crystals or historic-locality pieces can be higher.
What is Olivine’s structure and how is it identified?
Olivine is an orthorhombic nesosilicate in the forsterite-fayalite solid-solution series. Identify it by olive-green to yellow-green granular crystals, vitreous to oily luster, white streak, no obvious cleavage, and Mohs hardness of about 6.5-7.
What crystals pair well with Olivine?
For display or metaphysical layouts, olivine is commonly paired with quartz, black tourmaline, amethyst, and carnelian. Store it separately from softer minerals and protect transparent peridot crystals from knocks and abrasion.
Where is Olivine found?
Olivine is widespread in mantle-derived and mafic igneous rocks worldwide. Notable sources include Arizona in the United States, Zabargad Island in Egypt, Pakistan, Myanmar, China, Tanzania, Norway, Germany, South Africa, Australia, Brazil, and Hawaii.

Related Crystals

The metaphysical properties described are based on tradition and personal experience. Crystals are not a substitute for professional medical advice or treatment.