Grossular is a calcium-aluminum garnet that ranges in color from the vibrant green of Tsavorite to the cinnamon-brown of Hessonite. It is most commonly found in contact metamorphic rocks, specifically skarns, where limestone has been altered by igneous intrusions. Collectors should look for distinct dodecahedral crystal forms and its characteristic vitreous luster.
Is this grossular?
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 grossular with a known reference. Grossular sits at Mohs 6.5-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Grossular leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Grossular typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, brown, yellow, orange, red, colorless.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral or trapezohedral crystals, massive, granular.
Often confused with
Grossular vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside grossular
Minerals reported to co-occur with grossular. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Al₂(SiO₄)₃
- Mohs hardness
- 6.5-7.5
- Density
- 3.5-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral or Trapezohedral Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Gemstone, Lapidary
- Host rock
- Metamorphosed Limestones and Skarns
- Typical price
- $10-50 per specimen, $50-500+ for high-quality faceted gems
Where rockhounds find grossular
Classic worldwide localities
- Quebec, Canada
- Tanzania
- Mexico
- Italy
- Kenya
- Russia
Field-hunting tip
Look in metamorphosed limestones and skarns country — that is the host setting where grossular typically forms. If you start seeing calcite, diopside, vesuvianite in float, you are in the right ground. Field specimens usually show a dodecahedral or trapezohedral crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







