Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Tr
→ Tremolite
Ca-Mg amphibole
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈtrɛməlaɪt/
↔ TREM-uh-lite
from Tremola Valley
⚠ Safety & Handling
⚠asbestiformhigh (some)
Some habits asbestiform.
Handling: Avoid fibrous specimens. Solid bladed crystals are safe.
Information provided in good faith. Consult local hazmat regulations for transport and disposal. Severely hazardous specimens may require special storage cabinets.
Type Locality
Tremola, Val Leventina— Switzerland
Described 1789 by Saussure
› Browse all type localities
Cleavage & Fracture
Cleavage:
perfect2 directions ~56°/124°
Fracture:
splintery
Asbestiform varieties can split fibrously.
🔬
Collector tier: Micromount / Niche
Best appreciated at thumbnail or smaller scale — often dull-colored, sub-millimeter, or radioactive. Specialist appeal.
Tremolite sits at 5–6 on the Mohs scale —
just hard enough to scratch glass.
Colors:
Streak White
Crystal system Monoclinic
SilicatesSilicates (Inosilicates — Amphiboles)
TL;DR · 1 min read
Tremolite (Ca₂Mg₅Si₈O₂₂(OH)₂) is the magnesium end-member of the calcic amphibole group and the principal mineral of nephrite jade. It forms in metamorphosed dolomitic carbonates as long fibrous to bladed crystals — the same Tremolite that constitutes the nephrite of Hetian (Xinjiang) and the historic European jade trade.
Tremolite (Ca₂Mg₅Si₈O₂₂(OH)₂) is the magnesium end-member of the calcic amphibole group and the principal mineral of nephrite jade. It forms in metamorphosed dolomitic carbonates as long fibrous to bladed crystals — the same Tremolite that constitutes the nephrite of Hetian (Xinjiang) and the historic European jade trade. Pure Tremolite is white to pale gray; iron substitution darkens it toward Actinolite.