Clinozoisite sits at 6.5 on the Mohs scale —
harder than glass; scratches steel.
Colors:
Streak White
Crystal system Monoclinic
SilicatesSilicates (Sorosilicates)
TL;DR · 1 min read
Clinozoisite (Ca₂Al₃(SiO₄)(Si₂O₇)O(OH)) is the monoclinic counterpart of orthorhombic zoisite — same chemistry, different crystal system. It is closely related to epidote but has lower iron content.
Clinozoisite (Ca₂Al₃(SiO₄)(Si₂O₇)O(OH)) is the monoclinic counterpart of orthorhombic zoisite — same chemistry, different crystal system. It is closely related to epidote but has lower iron content. Clinozoisite forms in low-grade metamorphic rocks and contact-aureole skarns. Italian Alps and Japan yield gem-quality material.
Clinozoisite belongs to the silicate class in the epidote group and has the chemical formula Ca2Al3(Si2O7)(SiO4)O(OH). It crystallizes in the monoclinic system and holds a steady position among silicate species.
Identification & care
Crystals commonly develop as prismatic, striated along length, tabular, massive. Its color range is broad, including colorless, pale yellow, pale green, and pale pink (thulite = mn-bearing — see id 432). The luster is vitreous, the streak is white, and specimens range from transparent to translucent. The cleavage is perfect {001}. The fracture is uneven to conchoidal, which aids identification.
Collector context
Collector notes
Clinozoisite holds a steady place in systematic mineral collections. Clinozoisite is widely represented across Chinese provinces, including Heilongjiang, Gansu, Anhui, Guizhou.
Frequently asked questions
What is Clinozoisite?
Clinozoisite is a silicate mineral recognized among collectors for its crystal form and distribution, with known Chinese sources.
What crystal system does Clinozoisite belong to?
Clinozoisite crystallises in the Monoclinic crystal system.
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