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PHILLIPSITE
, a See also:mineral of the zeolite See also:group; a hydrated See also:potassium, See also:calcium and See also:aluminium silicate, approximating to (K2, Ca)AI2(SiOa)4.4H2O
.
It varies somewhat in See also:composition, and a variety (" pseudophillipsite ") containing rather less See also:silica has the See also:formula (K.2, Ca)2Al4Si5018.9H20
.
Crystals are See also:monoclinic, but only complex cruciform twins are known, these being exactly like twins of See also:harmotome (q.v.)
.
Crystals of phillipsite are, however, usually smaller and more transparent and glassy than those of harmotome
.
Spherical See also:groups with a. radially fibrous structure and bristled with crystals on the See also:surface are not uncommon
.
The hardness is 42, and the specific gravity 2.2
.
The See also:species was established by A
.
See also:Levy in 1825 and named after See also: See also:Minute spherical aggregates embedded in red See also:clay were dredged by the " Challenger " from the bottom of the Central Pacific, where they had been formed by the decomposition of See also:lava . (L . J . |
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