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Ore Variscite On White Background. Variscite Is A Secondary Mineral Formed By Direct Deposition From Phosphate-Bearing Water That Has Reacted With Aluminium-Rich Rocks In A Near-Surface Environment.[4] It Occurs As Fine-Grained Masses In Nodules, Cavity Fillings, And Crusts. Variscite Often Contains White Veins Of The Calcium Aluminium Phosphate Mineral Crandallite.

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Ore Variscite on white background. Variscite is a secondary mineral formed by direct deposition from phosphate-bearing water that has reacted with aluminium-rich rocks in a near-surface environment.[4] It occurs as fine-grained masses in nodules, cavity fillings, and crusts. Variscite often contains white veins of the calcium aluminium phosphate mineral crandallite.

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