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HEULANDITE , a See also: mineral of the zeolite See also: group, consisting of hydrous calcium and aluminium silicate, H4CaAl2(SiO3)s + 3H20
.
Small amounts of sodium and potassium are usually See also: present replacing See also: part of the calcium
.
Crystals are See also: monoclinic, and have a characteristic coffin-shaped 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: 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
See also: water of See also: crystallization
.
The two minerals may, however, be readily dis-
tinguished by the fact that in heulandite the
acute See also: 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
.
See also: Brooke arrived at the same result, giving
the name heulandite, after the mineral See also: collector, HenryHeuland
.
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 Deccan traps of the See also: Sahyadri mountains near Bombay
.
Crystals of a brick-red 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 Baltimore in See also: Maryland
.
Isomorphous with heulandite is the strontium and barium zeolite brewsterite, named after See also: Sir See also: David Brewster
.
The greyish monoclinic crystals have the composition H4(Sr, Ba, Ca)Al2(SiOa)s+3H20, and are found in the See also: basalt of the 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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