high tridymite
mineral
Also known as: beta2-tridymite, high-tridymite
Quick Summary
Tridymite is a mineral composed of silica (SiO2) that is stable at temperatures between 870° and 1,470° C (1,598° and 2,678° F). It is one of several forms of silica, including quartz and cristobalite, which share the same chemical composition but have different crystal structures. Tridymite typically forms thin, hexagonal, twinned plates and is commonly found in igneous rocks like trachytes. It can also be present in meteorites. The name "tridymite" refers to its common occurrence in groups of three crystals.123
Summary created from Britannica articles
using AI.
AI can make mistakes, so verify using Britannica articles.
4 Britannica Sources
Ask Britannica AI about this topic
Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.