Crystal Forms and Aggregates |
Cristobalite is a always a pseudomorph after Beta Cristobalite, which crystallizes in the isometric system, and thus Cristobalite occurs in isometric shaped crystals. Click here for a detailed explanation on the crystal structure of Cristobalite and other forms of silica.
Crystals are usually in microscopic grains, and small octahedral crystals can be made out under magnification. The octahedral crystals may be twinned with Spinel twinning. Cristobalite is much more common in globular groups and as crusty rounded balls. It also occurs massive, platy, crusty, and stalactitic. Crystals are occasionally cubic. |
Other ID Marks |
1) Crystals exhibit a strong double refraction. 2) Sometimes fluorescent white or cream.
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Complex Tests |
When heated to 350ºF (180ºC), Cristobalite becomes clear and transparent. However, when it cools down afterwards, it returns to its translucent or opaque state and becomes whitish again. |
Striking Features |
Mode of occurrence and crystal habits |
Environment |
Cristobalite occurs in igneous rocks located in areas of volcanic
activity, often lining gas bubbles in the host rock.
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