Zoisite is a calcium aluminum silicate typically found in metamorphic environments like eclogites and amphibolites. While common in its opaque, green-and-black ruby-in-zoisite form, it is most famous for its transparent blue variety, Tanzanite, which is prized by gem collectors for its strong pleochroism.
Is this zoisite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch zoisite with a known reference. Zoisite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, pearly on cleavage.
- 4Match the color rangeCompare against the expected color range: gray, green, pink, brown, blue, yellow, apple green, rose red.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: columnar, prismatic, striated.
Often confused with
Zoisite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zoisite
Minerals reported to co-occur with zoisite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Al₃(SiO₄)₃(OH)
- Mohs hardness
- 6-7
- Density
- 3.15-3.36 g/cm³
- Streak
- White
- Luster
- Vitreous, pearly on cleavage
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Columnar, prismatic, striated
- Cleavage
- {010}, perfect; {100}, imperfect
- Rarity
- Common
- Uses
- Gemstone, Lapidary, Collector
- Host rock
- Typically in medium-grade regionally metamorphosed crystalline schists formed from igneous, sedimentary, or metamorphic rocks relatively high in calcium; in eclogites and blueschist facies metamorphic rocks
Where rockhounds find zoisite
5 mapped spotsClassic worldwide localities
- Goshen and Williamsburg, Hampshire Co., Massachusetts, USA
- Keystone quarry, near Cornog, Chester Co., Pennsylvania, USA
- Milford Heights, Baltimore Co., Maryland, USA
- Spruce Pine, Mitchell Co., North Carolina, USA
- Saualpe, Carinthia, and in the Zillertal, Tirol, Austria
- Trondheim, Norway
Field-hunting tip
Where it forms: Typically in medium-grade regionally metamorphosed crystalline schists formed from igneous, sedimentary, or metamorphic rocks relatively high in calcium; in eclogites and blueschist facies metamorphic rocks. If you start seeing garnet, albite, biotite in float, you are in the right ground. Typical habit: columnar, prismatic, striated. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Idaho, Maryland, Utah. Start trip planning there.









