Spessartine is a manganese-rich member of the garnet group, famous for its vivid 'mandarin' orange hue. Collectors often look for sharp dodecahedral crystals in pegmatites or gem-quality pieces suitable for faceting, as high-clarity specimens are highly sought after in the jewelry market.
Is this spessartine garnet?
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 spessartine garnet with a known reference. Spessartine Garnet 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. Spessartine Garnet leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Spessartine Garnet typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: orange, red-orange, yellow-orange, red-brown.
- 5Look at form & habitCrystal system: isometric. Typical habit: dodecahedral or trapezohedral crystals, often rounded.
Often confused with
Spessartine Garnet vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside spessartine garnet
Minerals reported to co-occur with spessartine garnet. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₃Al₂(SiO₄)₃
- Mohs hardness
- 6.5-7.5
- Density
- 4.12-4.20 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Isometric
- Crystal habit
- Dodecahedral or Trapezohedral Crystals, Often Rounded
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Gemstone, Collector
- Host rock
- Granite Pegmatites, Metamorphic Schists, And Skarns
- Typical price
- $20-200 per carat depending on color saturation and clarity
Where rockhounds find spessartine garnet
4 mapped spotsClassic worldwide localities
- Namibia
- Nigeria
- Brazil
- Madagascar
- USA
Field-hunting tip
Look in granite pegmatites, metamorphic schists, and skarns country — that is the host setting where spessartine garnet typically forms. If you start seeing quartz, microcline, albite in float, you are in the right ground. Field specimens usually show a dodecahedral or trapezohedral crystals, often rounded habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in California, Maine, New Hampshire — start trip planning there.







