Lamproite is a rare, ultrapotassic volcanic or sub-volcanic rock known for its potential to host economic diamond deposits. It typically occurs as volcanic pipes and dikes, characterized by a complex mineralogy often dominated by phlogopite and leucite.
Is this lamproite?
3-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Read the lusterHold the specimen under a strong light. Lamproite typically shows a dull luster.
- 2Match the color rangeCompare against the expected color range: gray, greenish-gray, brown, dark-gray.
- 3Look at form & habitTypical habit: massive.
Often confused with
Lamproite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lamproite
Minerals reported to co-occur with lamproite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Density
- 2.5-2.8 g/cm³
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Rarity
- Rare
- Uses
- Geological Research, Diamond Prospecting
- Host rock
- Volcanic and Sub-volcanic Pipes and Dikes
Where rockhounds find lamproite
Classic worldwide localities
- Argyle Mine, Australia
- Leucite Hills, USA
- Spain
- India
Field-hunting tip
Look in volcanic and sub-volcanic pipes and dikes country — that is the host setting where lamproite typically forms. If you start seeing diamond, phlogopite, leucite 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.






