Ekanite | |
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A cut crystal of ekanite | |
General | |
Category | Silicate mineral |
Formula (repeating unit) | Ca 2ThSi 8O 20 or (Ca,Fe,Pb) 2(Th,U)Si 8O 20 |
IMA symbol | Ek [1] |
Strunz classification | 9.EA.10 |
Crystal system | Tetragonal |
Crystal class | Trapezohedral (422) H-M symbol: (4 2 2) |
Space group | I422 |
Identification | |
Color | Green, yellow, dark red |
Crystal habit | Pyramidal crystals, granular to massive |
Cleavage | Distinct on {101} |
Fracture | Brittle, uneven |
Mohs scale hardness | 4.5 |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.95 – 3.28 |
Optical properties | Uniaxial (−) |
Refractive index | nω = 1.580 nε = 1.568 |
Birefringence | δ = 0.012 |
2V angle | 10 – 15° |
Other characteristics |
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References | [2] [3] [4] |
Ekanite is an uncommon
silicate mineral with chemical formula Ca
2ThSi
8O
20 or (Ca,Fe,Pb)
2(Th,U)Si
8O
20. 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, [2] where it was first described in 1955 by F. L. D. Ekanayake, a Sri Lankan scientist, [5] [6] and it is named after him. [5]
In Sri Lanka the mineral specimens occur as detrital pebbles. In the Tombstone Mountains of Yukon, Canada, the mineral is found in a syenitic glacial erratic boulder. [3] In the Alban Hills of Italy it is found in volcanic ejecta. [2]
Ekanite can be uranium-lead dated with ekanite from Okkampitiya in the Monaragala District of Sri Lanka being dated to around 560 million years old. [7]