Åkermanite is a member of the melilite group, typically found in high-temperature, low-pressure contact metamorphic zones or within alkaline igneous rocks. It is most often identified by its tabular tetragonal habit and its occurrence alongside other skarn minerals like diopside and wollastonite.
Is this åkermanite?
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 åkermanite with a known reference. Åkermanite 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. Åkermanite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Åkermanite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray, yellowish, brown.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Åkermanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside åkermanite
Minerals reported to co-occur with åkermanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂MgSi₂O₇
- Mohs hardness
- 5-6
- Density
- 2.94-2.96 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Distinct On {001}
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Contact Metamorphosed Limestone, Skarns, Alkali Igneous Rocks
- Typical price
- $20-150 depending on specimen size and clarity
Where rockhounds find åkermanite
Classic worldwide localities
- Monte Somma, Italy
- Jacupiranga, Brazil
- Ontario, Canada
- Kola Peninsula, Russia
Field-hunting tip
Look in contact metamorphosed limestone, skarns, alkali igneous rocks country — that is the host setting where åkermanite typically forms. If you start seeing calcite, forsterite, diopside in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






