Formula: SiO2 tectosilicate (framework silicate)
Tridymite is the low pressure, high temperature, triclinic paramorph of quartz.
Specific gravity: 2.26 to 2.33
Hardness: 6½ to 7
Colour: White, colourless
Solubility: Soluble in HF and boiling Na2CO3
Volcanic igneous environments
Tridymite is chiefly found in magmatic rocks, especially felsic volcanic rocks. It is also a
constituent of some opal and
At atmospheric pressure, with increasing temperature beta quartz alters to tridymite at 870oC, and at 1,470oC tridymite alters to cristobalite. Tridymite, cristobalite and beta quartz can co-exist in equilibrium at a point with temperature about 1,400 oC and pressure 30 kbar (The quartz page).
In the San Juan Mountains, Colorado, USA, tridymite is abundant in groundmass and as phenocrysts in andesite-rhyolite (Dana).
At Yellowstone Park, Montana, USA, tridymite occurs in cavities in rhyolite and obsidian (Dana).
At Topaz Mountain, Utah, USA, tridymite occurs in cavities in rhyolite(Dana).
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