Pyrope is a magnesium-rich member of the garnet group, prized for its vivid red color. It is typically found in peridotites and kimberlites, often forming as a breakdown product from high-pressure metamorphic environments.
Is this pyrope?
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 pyrope with a known reference. Pyrope 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: red, purplish-red, orangey-red, blood red, orange red, purple red, pink, black red.
- 5Look at form & habitCrystal system: cubic. Typical habit: crystalline, granular, lamellar.
Often confused with
Pyrope vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pyrope
Minerals reported to co-occur with pyrope. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₃Al₂(SiO₄)₃
- Mohs hardness
- 7-7.5
- Density
- 3.582 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Cubic
- Crystal habit
- Crystalline, granular, lamellar
- Cleavage
- None
- Rarity
- Common
- Uses
- Gemstone, Collector, Abrasive
- Host rock
- In ultramafic rocks, as peridotites, kimberlites, eclogites, serpentinites, and in "hornblende" -garnet-plagioclase rocks and anorthosites
Where rockhounds find pyrope
2 mapped spotsClassic worldwide localities
- Masons' Mountain, near Cowee Creek, USA
- Macon Co., North Carolina, and from Buell Park, near Fort Defiance, Apache Co., Arizona, USA
- Mĕrunice (Meronitz), Czech Republic
- Dora-Maira massif, Parigi, near Martiniana Po, Piedmont, Italy
- Zöblitz and Greifendorf Saxony, Germany
- Diamond mines around Kimberley, Cape Province, South Africa
Field-hunting tip
Where it forms: In ultramafic rocks, as peridotites, kimberlites, eclogites, serpentinites, and in "hornblende" -garnet-plagioclase rocks and anorthosites. If you start seeing ilmenite, phlogopite, olivine in float, you are in the right ground. Typical habit: crystalline, granular, lamellar. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Alabama, Utah. Start trip planning there.









