Deposit types/Diamonds
Kimberlite and lamproite pipe
Carrot-shaped pipes of volcanic breccia that carry diamonds up from the mantle.
What it is
Carrot-shaped pipes of volcanic breccia that carry diamonds up from the mantle.1
How it forms
Kimberlite or lamproite magma climbs fast from the mantle along deep fractures, quenches and fills a pipe (diatreme) with breccia. Diamonds are scattered through it as crystals picked up on the way. Pipes weather quickly into hollows.1
Host rocks
Kimberlite diatreme breccia; olivine and leucite lamproite.1
Where it forms
Ancient stable cratons, often along major basement fractures or domed areas; not tied to mountain building.1
How old
Most productive pipes about 80 to 100, 250 and 1,000 to 1,100 Ma1
Typical grade
Mined kimberlites yield 0.1 to 0.6 ppm diamond1
How geologists look for it
Indicator minerals in soil and stream sediment (pyrope garnet, magnesian ilmenite, phlogopite, chromium and nickel anomalies); lamproite pipes lack ilmenite.1
Mines of this type
- Kimberley Big Hole1871
- Jagersfontein diamond mine1852
- Venetia
- Orapa1971
- Jwaneng1982
- Mir diamond mine1957
- Udachnaya pipe (Udachny mine)1971
- Argyle diamond mine
- Catoca1996
- Ekati1998
- Diavik2003
Story cards
Where next
Sources
- Mineral Deposit Models (Bulletin 1693, Cox and Singer, eds., 1986) US Geological Survey
From the Prospector Trails mining history dataset: each fact links to the source it was checked against. Figures are as the source gives them, in the money of their day. Not investment advice.
Keep exploring
Stories with these minerals

The world runs on rockThe MagnetRare earths that turn power into motion

All mining storiesThe world runs on rockAll mineralsMining by country
Cover photos from Wikimedia Commons: Super Pit, Kalgoorlie by Kgbo, CC BY-SA 4.0; Draglines by Roy Luck, CC BY 2.0.