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LEPIDOLITE

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Originally appearing in Volume V16, Page 464 of the 1911 Encyclopedia Britannica.
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LEPIDOLITE  , or LITHIA-See also:

MICA, a See also:mineral of the mica See also:group (see Mica) . It is a basic See also:aluminium, See also:potassium and See also:lithium fluo-silicate, with the approximate See also:formula KLi [Al(OH,F)2] Al(SiO3)3 . Lithia and See also:fluorine are each See also:present to the extent of about 5%; See also:rubidium and See also:caesium are sometimes present in small amounts . Distinctly See also:developed See also:monoclinic crystals or cleavage sheets of large See also:size are of rare occurrence, the mineral being usually found as scaly aggregates, and on this See also:account was named lepidolite (from Gr . XE7ric, See also:scale) by M . H . See also:Klaproth in 1792 . It is usually of a See also:lilac or See also:peach-blossom See also:colour, but is sometimes greyish-See also:white, and has a pearly lustre on the cleavage surfaces . The hardness is 21-4 and the sp. gr . 2.8-2.9, the optic axial See also:angle See also:measures 500-700 . It is found in See also:pegmatite-See also:veins, often in association with See also:pink See also:tourmaline (See also:rubellite) and some-times intergrown in parallel position with See also:muscovite . Scaly masses of considerable extent are found at Rozena near Bystrzitz in See also:Moravia and at Pala in See also:San Diego See also:county, See also:California .

The material from Rozena has been known since 1791, and has some-times been cut and polished for ornamental purposes: it has a See also:

pretty colour and spangled See also:appearance and takes a See also:good See also:polish, but is rather soft . At Pala it has been extensively See also:mined for the preparation of lithium and rubidium salts . Other localities for the mineral are the See also:island of UtS in See also:Sweden, and See also:Auburn and See also:Paris in See also:Maine, U.S.A.; at Alabashka near Mursinka in the Urals large isolated crystals have been found, and from Central See also:Australia transparent cleavage sheets of a See also:fine lilac colour are known . The lithium-See also:iron mica zinnwaldite or lithionite is closely allied to lepidolite, differing from it in containing some ferrous iron in addition to the constituents mentioned above . It occurs as greyish silvery scales with hexagonal outlines in the See also:tin-bearing granites of Zinnwald in the See also:Erzgebirge, Bohemia and of See also:Cornwall . (L . J .

End of Article: LEPIDOLITE
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Additional information and Comments

LEPIDOLITE. Experiments with Lepid from Cligga mine St Agnes Cornwall UK has been observed that Lepido is Thermochromic, the experiment was performed with 10 g of the rough (as found) massive Lepido, this occurs in the dumps of the old mine. 10 g was crushed fine to pass 250um siev and dried at 110 C for 2 hours, here it was found that the pink lavender Lipido had lost the bright colour to give a grey colour, upon cooling overnight the original colour returned. It is also possible that Lepido is photo sensitive due to the observation showing a remaining grey colour under the surface colour,after heating heating under a heat lamp there was no pink lavender colour but under the surface was the original colour, within a day or so the full colour returned fully. Further experiments are ongoing once sufficient material has been collected from the same sorce. David Bradbury..bradbury.arcana@btinternet.com
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