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Encyclopedia Britannica



PREHNITE

This article appears in Volume V22, Page 277 of the Encyclopedia Britannica.

Encyclopedia Britannica - Main :: POL-PRE
PREHNITE , a
mineral
  consisting of calcium hydrogen orthosilicate, H2Ca2Al2(SiO4)3. It crystallizes in the hemimorphic class of the orthorhombic system, but the hemimorphic character is usually obscured by twinning. Crystals are generally platy in habit, but they rarely occur singly and distinctly shaped; almost invariably they are closely aggregated together to form barrel-shaped or globular groups with a crystalline surface. This form, together with the
pale
  oil-green colour, gives the
mineral
  a very characteristic
appearance
 . It is translucent and has a vitreous lustre. The hardness is rather over 6 and the spec. gray. 2.802.95. Crystals are pyro-electric. Prehnite is sometimes classed with the zeolites, since it occurs under the same conditions as these minerals and often in association with them: the small amount of water (4.4%) is, however, expelled only at a red heat and is therefore not water of crystallization.
Prehnite occurs as a mineral of secondary origin in the amygdaloidal cavities of basic igneous rocks, such as basalt and diabase, and less often, in veins in granite and gneiss. Fine specimens are found with zeolites in the volcanic rocks of several places in the
south
  of
Scotland
 , e.g. Old Kilpatrick in Dumbartonshire, Bishopton in Renfrewshirc, Campsie Hills in
Stirlingshire
  and in the neighbourhood of Edinburgh; also at Paterson and Bergen Hill in New
Jersey
 , and with native copper in the trap-rocks of the Lake Superior region. In the French (at Le Bourg d'Oisans) and Tyrolese Alps it occurs with
axinite
 ,
epidote
 , felspar, &c., lining crevices in gneiss. Large masses have been found at Credock in Cape Colony, from which locality it was brought in the 18th century by Colonel Prehn, the
governor
  of the colony; hence the names " Cape chrysolite " and prehnite (of A. G. Werner, 1789). Prehnite is sometimes cut and polished for small ornaments; it then somewhat resembles chrysoprase in
appearance
 .


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