Gehlenite is a member of the melilite group that typically forms in contact metamorphosed limestones. Collectors should look for short, prismatic, or tabular tetragonal crystals embedded within skarn mineral assemblages.
Is this gehlenite?
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 gehlenite with a known reference. Gehlenite 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. Streak: white to grayish white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: gray, brown, colorless, greenish, yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: massive, prismatic, tabular.
Often confused with
Gehlenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gehlenite
Minerals reported to co-occur with gehlenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Al(AlSiO₇)
- Mohs hardness
- 5-6
- Density
- 3.038 g/cm³
- Streak
- White to grayish white
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent and opaque
- Crystal system
- Tetragonal
- Crystal habit
- Massive, prismatic, tabular
- Cleavage
- Distinct on {001}, poor on {110}
- Rarity
- Uncommon
- Uses
- Collector, Scientific research
- Host rock
- In contact metamorphosed impure limestones; in calcium-rich ultramafic volcanic rocks
Where rockhounds find gehlenite
Classic worldwide localities
- Crestmore, Riverside Co., California, USA
- Tres Hermanas district, Luna Co., New Mexico, USA
- Iron Hill, Gunnison Co., Colorado, USA
- Scawt Hill, near Larne, and at Carneal, Co. Antrim, Ireland
- Bellerberg volcano, two km north of Mayen, Eifel district, Germany
- Terneras mine, Velardeña, Durango, Mexico
Field-hunting tip
Where it forms: In contact metamorphosed impure limestones; in calcium-rich ultramafic volcanic rocks. If you start seeing dolomite, calcite, augite in float, you are in the right ground. Typical habit: massive, prismatic, tabular. Train your eye for that shape before scanning the outcrop.







