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HEULANDITE
, a See also:mineral of the zeolite See also:group, consisting of hydrous See also:calcium and See also:aluminium silicate, H4CaAl2(SiO3)s + 3H20
.
Small amounts of See also:sodium and See also:potassium are usually See also:present replacing See also:part of the calcium
.
Crystals are See also:monoclinic, and have a characteristic See also:coffin-shaped See also:habit
.
They have a perfect cleavage parallel to the See also:plane of symmetry (M in the figure), on which the lustre is markedly pearly; on other faces the lustre is of the vitreous type
.
The mineral is usually colourless or See also: Heulandite occurs with stilbite and other See also:zeolites in the amygdaloidal cavities of basaltic volcanic rocks, and occasion-ally in See also:gneiss and metalliferous See also:veins . The best specimens are from the basalts of Berufjord, near Djupivogr, in See also:Iceland and the Faroe Islands, and the See also:Deccan traps of the See also:Sahyadri mountains near Bombay . Crystals of a brick-red See also:colour are from Campsie Fells in See also:Stirlingshire and the Fassathal in See also:Tirol . A variety known as beaumontite occurs as small yellow crystals on syenitic schist near See also:Baltimore in See also:Maryland . Isomorphous with heulandite is the See also:strontium and See also:barium zeolite brewsterite, named after See also:Sir See also:David See also:Brewster . The greyish monoclinic crystals have the See also:composition See also:H4(Sr, Ba, Ca)Al2(SiOa)s+3H20, and are found in the See also:basalt of the See also:Giant's See also:Causeway in Co . See also:Antrim, and with See also:harmotome in the See also:lead mines at Strontian in See also:Argyllshire . (L . J . |
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