Mesolite
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Mesolite
Mesolite
Mesolite from Bombay, Hunterian Museum, Glasgow.jpg
Mesolite from Bombay collected in the 18th century by Dr John Hunter
General
CategoryTectosilicate
Zeolite
Formula
(repeating unit)
Na2Ca2(Al2Si3O10)3·8H2O
Strunz classification9.GA.05
Crystal systemOrthorhombic
Crystal classPyramidal (mm2)
(same H-M symbol)
Space groupFdd2
Unit cella = 18.4049(8) Å,
b = 56.655(6) Å,
c = 6.5443(4) Å; Z = 8
Identification
ColorColorless, white, gray, yellowish brown
Crystal habitAs elongated prismatic crystals, commonly in hairlike tufts and aggregates of fibers; radiating compact masses; stalactitic; porcelaneous
TwinningCharacteristically twinned on {010} or {100}
CleavagePerfect on {110} and {110}
FractureUneven
TenacityBrittle, masses tough
Mohs scale hardness5
LusterVitreous, silky when fibrous
StreakWhite
DiaphaneityTransparent to translucent, opaque
Specific gravity2.26
Optical propertiesBiaxial (+)
Refractive indexn? = 1.505 n? = 1.505 n? = 1.505
Birefringence? = 0.001
2V angleMeasured: 80°
Other characteristicsMay exhibit a small pyroelectric effect; piezoelectric
References[1][2][3][4]

Mesolite is a tectosilicate mineral with formula Na2Ca2(Al2Si3O10)3·8H2O. It is a member of the zeolite group and is closely related to natrolite which it also resembles in appearance.

Mesolite crystallizes in the orthorhombic system and typically forms fibrous, acicular prismatic crystals or masses.[2] Radiating sprays of needlelike crystals are not uncommon. It is vitreous in luster and clear to white in color. It has a Mohs hardness of 5 to 5.5 and a low specific gravity of 2.2 to 2.4. The refractive indices are n?=1.505 n?=1.505 n?=1.506.

Occurrence

It was first described in 1816 for an occurrence in the Cyclopean Islands near Catania, Sicily.[4] From the Greek mesos, "middle", as its composition lies between natrolite and scolecite.[3][4] Like other zeolites, mesolite occurs as void fillings in amygdaloidal basalt also in andesites and hydrothermal veins.[2]

Images

References



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Mesolite
 



 



 
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