Pectolite

From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
Pectolite
Pectolite-263712.jpg
General
CategoryInosilicate mineral
Formula
(repeating unit)
NaCa2Si3O8(OH)
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H-M symbol)
Space groupP1
Unit cella = 7.99 Å, b = 7.03 Å,
c = 7.03 Å; α = 90.51°,
β = 95.21°, γ = 102.53°; Z = 2
Identification
ColorColorless, whitish, grayish, yellowish
Crystal habitTabular to acicular, radiating fibrous, spheroidal, or columnar; massive
TwinningTwin axis [010] with composition plane [100], common
CleavagePerfect on {100} and {001}
FractureUneven
TenacityBrittle; tough when compact
Mohs scale hardness4.5 - 5
LusterSilky, subvitreous
DiaphaneityTranslucent to opaque
Specific gravity2.84 - 2.90
Optical propertiesBiaxial (+)
Refractive indexnα = 1.594 - 1.610 nβ = 1.603 - 1.614 nγ = 1.631 - 1.642
Birefringenceδ = 0.037
2V angleMeasured: 50° to 63°, Calculated: 42° to 60°
Dispersionr > v weak to very strong
References[1][2][3]

Pectolite is a white to gray mineral, NaCa2Si3O8(OH), sodium calcium hydroxide inosilicate. It crystallizes in the triclinic system typically occurring in radiated or fibrous crystalline masses. It has a Mohs hardness of 4.5 to 5 and a specific gravity of 2.7 to 2.9. The gemstone variety, larimar, is a pale to sky blue.

Occurrence[edit]

It was first described in 1828 at Mt. Baldo, Trento Province, Italy and named from the Greek pektos – "compacted" and lithos – "stone".[2][3]

It occurs as a primary mineral in nepheline syenites, within hydrothermal cavities in basalts and diabase and in serpentinites in association with zeolites, datolite, prehnite, calcite and serpentine. It is found in a wide variety of worldwide locations.

See also[edit]

References[edit]

External links[edit]