Barite typically appears as a colorless or white mineral but can also occur in shades of blue, yellow, green, or brown. It often forms in a crystalline structure, exhibiting a glassy luster, and can be found in distinct tabular or prismatic crystals. The mineral has a high specific gravity, giving it a dense feel, and it may also occur as massive or granular aggregates. Its distinctive properties make it easily recognizable in mineral collections and geological settings.
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