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Polymorphism can increase outside of pure symmetry written content. The aluminosilicates are a bunch of 3 minerals – kyanite, andalusite, and sillimanite – which share the chemical system Al2SiO5. Kyanite is triclinic, when andalusite and sillimanite are each orthorhombic and belong for the dipyramidal stage group. These dissimilarities occur