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BRUCITE
, a See also:mineral consisting of See also:magnesium hydroxide, Mg(OH)2, and crystallizing in the See also:rhombohedral See also:system
.
It was first described in 1814 as " native See also:magnesia from New See also:Jersey by A
.
See also:Bruce, an See also:American mineralogist, after whom the See also:species was named by F
.
S
.
See also:Beudant in 1824; the same name had, however, been earlier applied to the mineral now known as chondrodite
.
Brucite is usually found as platy masses, some-times of considerable See also:size, which have a perfect cleavage parallel to the See also:surface of the plates
.
It is See also: Brucite is generally associated with other magnesian minerals, such as See also:magnesite and See also:dolomite, and is commonly found in See also:serpentine, or sometimes as small scales in phyllites and crystal-See also:line See also:schists; it has also been observed in metamorphosed magnesian See also:limestone, such as the See also:rock known as predazzite from Predazzo in See also:Tirol . The best crystals and foliated masses are from See also:Texas in See also:Pennsylvania, U.S.A., and from Swinaness in Unst, one of the See also:Shetland Isles, Nemalite is from See also:Hoboken, New Jersey, and from See also:Afghanistan . At all these localities the mineral forms See also:veins in serpentine . (L . J . |
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