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Large Tolbachik Fissure Eruption, S.A. Fedotov, Moscow 1984 p340, states that Cristobalite does not occur as independent mineral, but as inclusions in high temp sublimates. After dissolving the sublimates, Cristobalite was found in the residu.

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Original EntryLarge Tolbachik Fissure Eruption, S.A. Fedotov, Moscow 1984 p340, states that Cristobalite does not occur as independent mineral, but as inclusions in high temp sublimates. After dissolving the sublimates, Cristobalite was found in the residu.
Mindat Ref. ID15941518Long-form Identifiermindat:1:5:15941518:6
GUID01cf101b-2464-4597-8aa6-20f49d843c12
Full ReferenceLarge Tolbachik Fissure Eruption, S.A. Fedotov, Moscow 1984 p340, states that Cristobalite does not occur as independent mineral, but as inclusions in high temp sublimates. After dissolving the sublimates, Cristobalite was found in the residu.
Plain TextLarge Tolbachik Fissure Eruption, S.A. Fedotov, Moscow 1984 p340, states that Cristobalite does not occur as independent mineral, but as inclusions in high temp sublimates. After dissolving the sublimates, Cristobalite was found in the residu.

Mineral Occurrences

LocalityMineral(s)
Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russiaβ“˜ Cristobalite


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