
This type of quartz derives its distinctive milky white or cream from inclusions of gas and liquid bubbles. Their education of milkyness depends upon the amount and size inclusions present. Crystals are hexagonal prisms with pyramidal ends.
Large crystals are present in Siberia. Other localities include Brazil, the European Alps, Madagascar, the united states and Namibia.
When polished or cut “en cabochon”, it might be wrongly identified as opal.
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