Schorlomite is a rare titanium-rich member of the garnet group, typically identified by its striking black color and brilliant sub-metallic to vitreous luster. It is most frequently found in alkaline igneous complexes and carbonatites, often appearing as distinct dodecahedral crystals. Collectors prize it for its unique chemistry and rarity compared to more common garnet species.
Is this schorlomite?
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 schorlomite with a known reference. Schorlomite sits at Mohs 7-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schorlomite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Schorlomite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals, massive.
Often confused with
Schorlomite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside schorlomite
Minerals reported to co-occur with schorlomite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Ti₂Fe₂SiO₁₂
- Mohs hardness
- 7-7.5
- Density
- 3.8-3.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks, Carbonatites
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find schorlomite
Classic worldwide localities
- Magnet Cove, Arkansas, USA
- Kaiserstuhl, Germany
- Kola Peninsula, Russia
- Ontario, Canada
Field-hunting tip
Look in alkaline igneous rocks, carbonatites country — that is the host setting where schorlomite typically forms. If you start seeing nepheline, aegirine, calcite in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, massive habit, so train your eye for that shape before scanning the outcrop.






