Article
Article
- Earth Science
- Mineralogy and petrology
- Silica minerals
Silica minerals
Article By:
Drake, John C. Department of Geology, University of Vermont, Burlington, Vermont.
Last reviewed:January 2020
DOI:https://doi.org/10.1036/1097-8542.622400
- Crystal structure
- Properties
- Phase relationships and occurrences
- Related Primary Literature
- Additional Reading
Silica (SiO2) occurs naturally in at least nine different varieties (polymorphs), which include tridymite (high-, middle-, and low-temperature forms), cristobalite (high- and low-temperature forms), coesite, and stishovite, in addition to high (β) and low (α) quartz (Fig. 1). These forms have distinctive crystallography, optical characteristics, physical properties, pressure-temperature stability ranges, and occurrences (see table).
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