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, 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.







