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For more on marking an answer as the "Best Answer", please visit our FAQ.Cristobalite is the rare, cubic, high temperature polymorph of quartz, though it is meta-stable below something like 1400�C (off the top of my head).
Below these temperatures, it will tend to revert to the lower T� polymorphs, hexagonal �-quartz, or trigonal quartz ('low quartz').
Where a reversion to, say, a low T� polymorph occurs, but the mineral retains the crystal system of the high T� polymorph, it, as gen2 says, is called a pseudomorph.