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Through the actions of volcanism, the deposited forests were covered with deep ash layers creating an anoxic atmosphere, as metres of ash covered the lands, the depositing layers of ash and silts helped the anaerobic environment to persist whilsy soluble minerals in the water were forced through the tissues of flora at molecular levels, cell by cell the vascular system of these floras transformed into quartz-rich, semi-precious petrified historical statements.

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