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Kimberlite rock is an igneous rock best known for sometimes containing diamonds. It is difficult to find and mine kimberlite rocks as they often occur as small volumes called kimberlite pipes or dykes. Let's look at some frequently asked questions about kimberlite rock near you.
Kimberlite rock is a type of potassic igneous rock known for sometimes containing diamonds. It is a rare form of ultramafic volcanism derived from deep underground originating from the Earth's mantle. Kimberlite rock has a composition dominated by olivine, serpentine, calcite and magnesium-rich silicates.
Some areas where kimberlite rock pipes or dykes may be located within a few hours drive include parts of Northern and Central Ontario in Canada as well as regions in South Africa, Siberia, Greenland and Colorado in the United States.
Kimberlite rock has a distinctive blue groundmass and may contain olivine grains which make the rock dark blue in colour. Under a microscope, kimberlite rock can be identified by the presence of yellow, green and blue pyrope garnets and orange chromium-rich ilmenite.
Kimberlite pipes are vertical shafts or funnels created by the eruption of deep-origin kimberlite magma. They have a carrot-like or tapered shape and can extend over 1 kilometer deep into the Earth's crust. Diamonds may form within or be carried to the surface by kimberlite magma in these pipes.
It is possible but not guaranteed to find diamonds when mining kimberlite rock formations such as pipes or dykes. Only a small fraction of 1% of the kimberlite rock volume may contain diamond crystals. Professional geological surveying, sampling, drying and sorting is needed to detect potential diamonds in kimberlite rock.
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