Online Encyclopedia

HEULANDITE

Online Encyclopedia
Originally appearing in Volume V13, Page 416 of the 1911 Encyclopedia Britannica.
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HEULANDITE  , a

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mineral of the zeolite
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group, consisting of hydrous calcium and aluminium silicate, H4CaAl2(SiO3)s + 3H20 . Small amounts of sodium and potassium are usually
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present replacing
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part of the calcium . Crystals are
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monoclinic, and have a characteristic coffin-shaped habit . They have a perfect cleavage parallel to the
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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 white, sometimes brick-red, and varies from transparent to translucent . The hardness is 31-4, and the specific gravity 2.2 . Heulandite closely resembles stilbite (q.v.) in appearance, and differs from it chemically only in containing rather less
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water of crystallization . The two minerals may, however, be readily dis- tinguished by the fact that in heulandite the acute positive bisectrix of the optic axes emerges perpendicular to the cleavage . Heulandite was first separated from stilbite by A . Breithaupt in 1818, and named by him euzeolite (meaning beautiful zeolite); independ- ently, in 1822, H . J . Brooke arrived at the same result, giving the name heulandite, after the mineral
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collector, HenryHeuland .

Heulandite occurs with stilbite and other

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zeolites in the amygdaloidal cavities of basaltic volcanic rocks, and occasion-ally in
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gneiss and metalliferous
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veins . The best specimens are from the basalts of Berufjord, near Djupivogr, in Iceland and the Faroe Islands, and the Deccan traps of the
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Sahyadri mountains near Bombay . Crystals of a brick-red colour are from Campsie Fells in
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Stirlingshire and the Fassathal in Tirol . A variety known as beaumontite occurs as small yellow crystals on syenitic schist near Baltimore in
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Maryland . Isomorphous with heulandite is the strontium and barium zeolite brewsterite, named after
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Sir David Brewster . The greyish monoclinic crystals have the composition H4(Sr, Ba, Ca)Al2(SiOa)s+3H20, and are found in the
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basalt of the Giant's
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Causeway in Co . Antrim, and with
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harmotome in the lead mines at Strontian in
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Argyllshire . (L . J .

End of Article: HEULANDITE
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