Tremolite

A variety of Minerals

Tremolite specimen

What is Tremolite?

Tremolite is a member of the amphibole group of silicate minerals with composition: Ca2(Mg5.0-4.5Fe0.0-0.5)Si8O22(OH)2. Tremolite forms by metamorphism of sediments rich in dolomite and quartz. Tremolite forms a series with actinolite and ferro-actinolite. Pure magnesium tremolite is creamy white, but the color grades to dark green with increasing iron content. It has a hardness on Mohs scale of 5 to 6. Nephrite, one of the two minerals of the gemstone jade, is a green variety of tremolite. The fibrous form of tremolite is one of the six recognised types of asbestos. This material is toxic, and inhaling the fibers can lead to asbestosis, lung cancer and both pleural and peritoneal mesothelioma. Fibrous tremolite is sometimes found as a contaminant in vermiculite, chrysotile (itself a type of asbestos) and talc.

Optical Properties

Refractive Index
1.599-1.637
Birefringence
0.023-0.028
Pleochroism
None
Optical Character
Biaxial negative

Market Value Factors

Pricing varies for every rock and mineral, so use these universal factors to gauge Tremolite before comparing listings or appraisals.

Size & Weight

Larger, intact specimens usually command higher prices.

Rarity & Demand

Scarce material or popular varieties sell at a premium.

Condition & Finish

Chips, repairs, and heavy wear lower value; clean prep helps.

Treatment & Provenance

Untreated specimens with documented locality are prized.

Applies to all rocks & minerals.

Tremolite Localities Map

See where Tremolite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

Map preview
North ZoneCentral RidgeSouth Basin

Interactive map layers and collecting notes are available in the app.

The Meaning

Tremolite is considered a secondary birthstone for the signs of Scorpio, Pisces, Gemini and Libra.

Key Characteristics

Formation of Tremolite

Tremolite is an indicator of metamorphic grade since at high temperatures it converts to diopside. Tremolite occurs as a result of contact metamorphism of calcium and magnesium rich siliceous sedimentary rocks and in greenschist facies metamorphic rocks derived from ultramafic or magnesium carbonate bearing rocks. Associated minerals include calcite, dolomite, grossular, wollastonite, talc, diopside, forsterite, cummingtonite, riebeckite and winchite. Tremolite was first described in 1789 for an occurrence in Campolungo, Piumogna Valley, Leventina, Ticino (Tessin), Switzerland.

More Images

Tremolite specimen
Robert M. Lavinsky
Tremolite specimen
Didier Descouens

Quick Facts

Physical Properties

Color
White, brown, colourless, grey, light green, green, light yellow, pink-violet
Hardness (Mohs)
5 - 6
Density
2.964 g/cm³
Streak
White

Chemical Properties

Chemical Formula
☐{Ca2}{Mg5}(Si8O22)(OH)2
Elements
Ca, H, Mg, O, Si

Also Known As

TremoliteAbkhaziteGrammatiteRaphiliteSebesite
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Tremolite FAQs

How do I identify Tremolite?

Tremolite can be identified by its hardness of 5 - 6 on the Mohs scale, White color. Look for these key characteristics when examining specimens.

What color is Tremolite?

Tremolite typically appears in White, brown, colourless, grey, light green, green, light yellow, pink-violet. Color can vary depending on impurities and formation conditions.

How hard is Tremolite?

Tremolite has a hardness of 5 - 6 on the Mohs scale. This gives it moderate hardness.

What is the formation of tremolite of Tremolite?

Tremolite is an indicator of metamorphic grade since at high temperatures it converts to diopside. Tremolite occurs as a result of contact metamorphism of calcium and magnesium rich siliceous sedimentary rocks and in greenschist facies metamorphic rocks derived from ultramafic or magnesium carbonate bearing rocks. Associated minerals include calcite, dolomite, grossular, wollastonite, talc, diopside, forsterite, cummingtonite, riebeckite and winchite. Tremolite was first described in 1789 for an occurrence in Campolungo, Piumogna Valley, Leventina, Ticino (Tessin), Switzerland.

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