Description
Fluorite – Teal Tumbled Stones
Teal Fluorite can be formed in primary, secondary or even tertiary processes. The largest amounts come to us from magmatic origins where Fluorite arises as a component of acid magmatic rocks or in passages and clefts. It is more rare for it to be formed in a secondary process through the action of fluoric acid that is released during the weathering of calcium bearing rock.
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