ekanite

{{Infobox mineral | boxbgcolor = #5d6240 | boxtextcolor = #fff | name = Ekanite | category = Phyllosilicate minerals | image = Ekanitef13.JPG | imagesize = | caption = A cut crystal of ekanite | formula = or | IMAsymbol = Ek | molweight = | strunz = 9.EA.10 | system = Tetragonal | class = Trapezohedral (422) H-M symbol: (4 2 2) | symmetry = I422 | color = Green, yellow, dark red | habit = Pyramidal crystals, granular to massive | cleavage = Distinct on {101} | fracture = Brittle, uneven | mohs = 4.5 | luster = Vitreous | refractive = nω = 1.580 nε = 1.568 | opticalprop = Uniaxial (−) | 2V = 10 – 15° | birefringence = δ = 0.012 | streak = White | gravity = 2.95 – 3.28 | diaphaneity = Transparent to translucent | other = 25px Radioactive, metamict | references = }} Ekanite is an uncommon silicate mineral with chemical formula or . It is a member of the steacyite group. It is among the few gemstones that are naturally radioactive. Most ekanite is mined in Sri Lanka, although deposits also occur in Russia and North America. Clear and well-colored stones are rare as the radioactivity tends to degrade the crystal matrix over time in a process known as metamictization.

The type locality is Eheliyagoda, Ratnapura District, Sabaragamuwa Province, Sri Lanka, where it was first described in 1955 by F. L. D. Ekanayake, a Sri Lankan scientist, and it is named after him.