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cordierite
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cordierite

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Cordierite (mineralogy) or iolite (gemology) is a magnesium iron aluminium cyclosilicate. Iron is almost always present, and a solid solution exists between Mg-rich cordierite and Fe-rich sekaninaite with a series formula: to . A high-temperature polymorph exists, indialite, which is isostructural with beryl and has a random distribution of Al in the rings. Cordierite is also synthesized and used in high temperature applications such as catalytic converters and pizza stones.

Key facts

Mineral.color
Blue, smoky blue, bluish violet; greenish, yellowish brown, gray; colorless to very pale blue in thin section in transmitted light
Mineral.habit
Pseudo-hexagonal prismatic twins, as imbedded grains, and massive
Mineral.twinning
Common on {110}, {130}, simple, lamellar, cyclical
Mineral.cleavage
Fair on {100}, poor on {001} and {010}
Mineral.fracture
Subconchoidal
Mineral.tenacity
Brittle
Mineral.mohs
7–7.5
Mineral.luster
Greasy or vitreous
Mineral.diaphaneity
Transparent to translucent
Mineral.refractive
nα = 1.527 – 1.560 nβ = 1.532 – 1.574 nγ = 1.538 – 1.578 Indices increase with Fe content.
Mineral.opticalprop
Usually optically (-), sometimes (+); 2V = 0–90°
Mineral.pleochroism
X = pale yellow, green; Y = violet, blue-violet; Z = pale blue
Mineral.streak
White
Mineral.gravity
2.57–2.66
Mineral.diagnostic
Resembles quartz, can be distinguished by pleochroism. Can be distinguished from corundum by its lower hardness
Mineral.boxbgcolor
7e7066
Mineral.name
Cordierite
Mineral.boxtextcolor
fff

via Wikipedia infobox

~6 min read

Encyclopedic overview

8 sections
Contents
  • Name and discovery
  • Occurrence
  • Commercial use
  • Gem variety
  • Applications
  • See also
  • References
  • External links

{{Infobox mineral |boxbgcolor=#7e7066| name = Cordierite | boxtextcolor = #fff | category = Cyclosilicate | image = Cordierite-den07-06aa.jpg | imagesize = 260px | caption = | formula = | IMAsymbol = Crd | strunz = 9.CJ.10 | dana = 61.02.01.01 Cordierite group | system = Orthorhombic | class = Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | symmetry = Cccm | unit cell = a = 17.079 Å, b = 9.730 Å, c = 9.356 Å; Z = 4 | color = Blue, smoky blue, bluish violet; greenish, yellowish brown, gray; colorless to very pale blue in thin section in transmitted light | habit = Pseudo-hexagonal prismatic twins, as imbedded grains, and massive | twinning = Common on {110}, {130}, simple, lamellar, cyclical | cleavage = Fair on {100}, poor on {001} and {010} | fracture = Subconchoidal | tenacity = Brittle | mohs = 7–7.5 | luster = Greasy or vitreous | diaphaneity = Transparent to translucent | refractive = nα = 1.527 – 1.560 nβ = 1.532 – 1.574 nγ = 1.538 – 1.578 Indices increase with Fe content. | opticalprop = Usually optically (-), sometimes (+); 2V = 0–90° | pleochroism = X = pale yellow, green; Y = violet, blue-violet; Z = pale blue | streak = White | gravity = 2.57–2.66 | melt = | fusibility = on thin edges | diagnostic = Resembles quartz, can be distinguished by pleochroism. Can be distinguished from corundum by its lower hardness | solubility = | other = | references = }}

Cordierite (mineralogy) or iolite (gemology) is a magnesium iron aluminium cyclosilicate. Iron is almost always present, and a solid solution exists between Mg-rich cordierite and Fe-rich sekaninaite with a series formula: to . A high-temperature polymorph exists, indialite, which is isostructural with beryl and has a random distribution of Al in the rings. Cordierite is also synthesized and used in high temperature applications such as catalytic converters and pizza stones.

Excerpted from Wikipedia’s “cordierite” article, available under the CC BY-SA 4.0 licence.

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