Kimberlite is a rare, potassic volcanic rock best known as the primary host rock for diamonds. It typically occurs in vertical, carrot-shaped structures known as volcanic pipes and is characterized by a porphyritic texture containing phenocrysts of olivine and phlogopite within a fine-grained matrix.
Is this kimberlite?
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 kimberlite with a known reference. Kimberlite sits at Mohs 3-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kimberlite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Kimberlite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: dark gray, bluish gray, greenish gray, brown.
- 5Look at form & habitTypical habit: massive.
Often confused with
Kimberlite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kimberlite
Minerals reported to co-occur with kimberlite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-5
- Density
- 2.6-2.9 g/cm³
- Streak
- Gray
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector, Geological Study
- Host rock
- Volcanic Pipes
- Typical price
- $10-100 per specimen
Where rockhounds find kimberlite
Classic worldwide localities
- Kimberley, South Africa
- Yakutia, Russia
- Ellendale, Australia
- Ekati, Canada
- Argyle, Australia
Field-hunting tip
Look in volcanic pipes country, the host setting where kimberlite typically forms. If you start seeing diamond, phlogopite, olivine in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.








