What is Kimberlite?
Kimberlite is a volatile-rich ultramafic volcanic rock famous as the host of many diamonds and as a rapid messenger from the deep mantle.
Mineralogy and crystal structure
Reference formula: No single formula applies because this is a rock.. Kimberlite is a complex rock, not a single mineral species or fixed formula. It may contain olivine, phlogopite, serpentine, carbonates and accessory minerals; diamond-bearing potential cannot be inferred from appearance alone. Kimberlite is classified with a rock rather than one mineral class and has a not applicable to the rock as a whole crystal system. Typical hardness is 3–6 on the Mohs scale and specific gravity is approximately 2.4–3.3.
Colour, lustre and habit
Typical colours include green, blue-grey, black, brown. The usual massive, brecciated, porphyritic habit and dull, earthy, vitreous lustre help describe a specimen, but colour alone is not diagnostic.
Formation and notable localities
Kimberlite forms in or is associated with deep-sourced explosive volcanic pipes and diatremes. Important documented localities include South Africa, Botswana, Canada, Russia, Australia and Tanzania.
The rock behind the diamond story
Kimberlite gives a collection instant geological drama. Even a small fragment can anchor a display about mantle-derived magmas, diamond transport and the difference between a visually ordinary host rock and the exceptional crystals it may carry.
Collecting and care
Treat as a rock specimen; avoid dust and retain locality or mine provenance, especially where heavy minerals or alteration products are present.