Nuummite
Nuummite is a natural metamorphic rock from the Nuuk region of West Greenland, made almost entirely of orthoamphiboles of the anthophyllite–gedrite series. Its grains consist of alternating submicroscopic lamellae of anthophyllite and gedrite, which produce iridescence in gold, blue, green and other colors on a gray to black ground when the stone is cut. Nuummite is a trade name, not an approved mineral name; it means "from Nuuk" in Greenlandic.
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Full material guide
What the material is, where it comes from or how it is made, identification and care, from the cited sources.
Properties
| Material type | Natural rock (metamorphic) |
| Composition | Orthoamphiboles of the anthophyllite–gedrite series, with small amounts of pyrrhotite, chalcopyrite, pyrite, magnetite, molybdenite, gahnite, biotite or cordierite |
| Color | Light gray to almost black ground, with iridescent grains in green, metallic blue, yellow to golden, reddish and rarely violet |
| Optical effect | Iridescence from interference in alternating anthophyllite and gedrite lamellae |
| Refractive index | About 1.64 to 1.66 (birefringence about 0.02) |
| Specific gravity | 3.18 to 3.37 (commonly about 3.24) |
| Mohs hardness | About 6 |
Origins & sources
Nuummite has been found at eight localities within about 50 km of Nuuk, the capital of Greenland, in orthoamphibole layers and pods within Archean supracrustal rocks and gneisses (described as the Malene supracrustals, in the Akulleq terrane). Gemological studies describe the host rocks as more than three billion years old; material from Simiuttat island has been dated to about 2,732 to 2,707 million years. A further occurrence has been described at Kangerluarsuk in the Maniitsoq region. Mindat notes that some "pseudo-nuummites" come from China and India.
Identification
The iridescence is rarely visible on rough pieces and appears clearly only after cutting; most cabochons show one or two colors. In golden material from Simiuttat, transmission electron microscopy showed that it comes from interference of light reflected from alternating gedrite and anthophyllite exsolution lamellae with an average spacing of about 180 nm, a spacing that gives yellow iridescence. Cabochons smaller than 0.5 cm usually contain too few iridescent grains to look attractive. The rock fluoresces dark violet under ultraviolet light. Because pseudo-nuummites from other countries are on the market, the name alone does not establish a Greenland origin.
Care
Orthoamphiboles have a hardness of about 6. In a test reported in Gems & Gemology, nuummite cabochons placed in a window in sunshine for more than a year showed no change in appearance. Fresh material is generally massive without pervasive cracks, but material from near the surface tends to have small cracks.
History
Iridescent orthoamphibole from the Nuuk area was first collected by K. L. Giesecke in 1810 and described by O. B. Bøggild in 1905 and 1924. The geologist Peter W. Uitterdijk Appel of the Geological Survey of Greenland rediscovered it as a gem material in 1982. The Nuuk town council gave it the trade name Nuummite, a company owned by the Nuuk municipality received an exploration concession and permission to make and sell jewelry, and the stone was launched on the Greenlandic market before Christmas 1986.
Cultural meanings
Not collected yet
Traditional beliefs
Not collected yet
Collected Oct 23, 2026
- A New Gem Material from Greenland: Iridescent Orthoamphibole (Gems & Gemology 23(1), 1987) GIA Gems & Gemology (Peter W. U. Appel, Geological Survey of Greenland; Aage Jensen, University of Copenhagen) · Accessed Oct 23, 2026 OverviewPropertiesOrigins & sourcesIdentificationCareHistory
- Nuummite: Mineral information, data and localities. Mindat.org (Hudson Institute of Mineralogy) · Accessed Oct 23, 2026 OverviewPropertiesOrigins & sourcesIdentificationHistory
- A nuummite occurrence from Kangerluarsuk in the Maniitsoq Region, West Greenland (IGC 2023 abstract) International Gemmological Conference · Accessed Oct 23, 2026 PropertiesOrigins & sourcesHistory
- The origin of iridescence in anthophyllite-gedrite from Simiuttat, Nuuk district, southern West Greenland (Mineralogical Magazine 64(5), 2000, abstract) Mineralogical Magazine (Pamela E. Champness, Kerry A. Rodgers) · Accessed Oct 23, 2026 OverviewPropertiesIdentification