Tridymite is a high temperature polymorph of silica and usually occurs as minute tabular white or colorless pseudo hexagonal crystals or scales in cavities in
Tridymite is a rare polymorph of the mineral Quartz However its crystals are very distinct and form very different habits from Quartz Many Tridymite specimens
The structural phase transitions of monoclinic tridymite that occur at elevated temper atures as tained by crushing a portion of the MC tridymite sample n
Name Tridymite RRUFF ID R040143 Ideal Chemistry SiO2 Locality Big Lue Mountain Highway 78 Greenlee County Arizona USA Source University of
Tridymite SiO2 c○2001 Mineral Data Publishing version 1 2 Crystal Data Orthorhombic pseudohexagonal triclinic below about 100 ±C Point Group 222 or
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