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 — that is 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.







