Tsavorite

Crystal system · Isometric

Tsavorite is a silicate mineral recognized among collectors for its crystal form and distribution.

About Tsavorite

Tsavorite is classified as a silicate mineral in the garnet group (grossular variety) and has the chemical formula Ca3Al2(SiO4)3. It crystallizes in the isometric system and holds a steady position among silicate species. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.

Identification & care

Crystals commonly develop as dodecahedral and trapezohedral crystals. Its color is typically vivid green and emerald-green. The luster is vitreous to adamantine, the streak is white, and specimens are typically transparent. The fracture is conchoidal, which is one of its key identifying features.

Collector context

How it forms

The geological setting for Tsavorite is typically metamorphic — cr- and v-bearing calc-silicate rocks and granulites. It is commonly found in association with grossular, diopside, tremolite, graphite, pyrrhotite.

Why collectors care

Tsavorite is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.

What affects value

Value in Tsavorite is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.

Naming history

The name Tsavorite has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.