Tschermakite is a complex calcium-magnesium-aluminum silicate belonging to the amphibole group, typically found in high-grade metamorphic rocks. Collectors often identify it by its prismatic, dark-colored crystalline habit and its occurrence within metamorphic terrains like skarns and amphibolites.
Is this tschermakite?
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 tschermakite with a known reference. Tschermakite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tschermakite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tschermakite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black, dark green, dark brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Tschermakite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tschermakite
Minerals reported to co-occur with tschermakite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂(Mg₃Al₂)(Si₆Al₂)O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.2-3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Massive, Granular
- Cleavage
- Perfect in Two Directions
- Rarity
- Uncommon
- Uses
- Collector, Petrological Studies
- Host rock
- Metamorphic Rocks Like Amphibolites and Skarns
- Typical price
- $10-50 per specimen
Where rockhounds find tschermakite
Classic worldwide localities
- Tschermak, Austria
- Adirondack Mountains, USA
- Grenville Province, Canada
- Kola Peninsula, Russia
Field-hunting tip
Look in metamorphic rocks like amphibolites and skarns country — that is the host setting where tschermakite typically forms. If you start seeing garnet, diopside, plagioclase in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







