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KUNZITE

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Source
Encyclopaedia Britannica (1911) / britannica_1911
License
public_domain
Chunk ID
1911:kunzite:608ff7f182a6
Section
Hash Algorithm
sha256
Stored Hash
ae21062135c96146c4f58a12e4a1c926ae19ab85a1737a5a2c572ed478328103
Computed Hash
ae21062135c96146c4f58a12e4a1c926ae19ab85a1737a5a2c572ed478328103
Normalizer
ggnorm 1.0
Observed
2026-02-08 18:43:13
Source URL

Verified Text

kunzite, a transparent lilac-coloured variety of spodumene, used as a gem-stone. it was discovered in 1902 near pala, in san diego county, california, not far from the locality which yields the fine specimens of rubellite and lepidolite, well known to mineralogists. the mineral was named by dr c. baskerville after dr george f. kunz, the gem expert of new york, who first described it. analysis by r. o. e. davis showed it to be a spodumene. kunzite occurs in large crystals, some weighing as much as 1000 grams each, and presents delicate hues from rosy lilac to deep pink. it is strongly dichroic. near the surface it may lose colour by exposure. kunzite becomes strongly phosphorescent under the rontgen rays, or by the action of radium or on exposure to ultra-violet rays. (see spodumene.)