Iridescence is very often observed on the glassy surface of freshly erupted basaltic tephra like those erupted by Piton de la Fournaise volcano;

On one side, it disappears quickly on samples collected soon after an eruption; on the other sides, it can be observed on clasts erupted centuries ago; multiple physico-chemical processes are possibly responsible of this intriguing phenomenon (chemical attack by acid gases; thin film effects; microvesicularity; density contrasts; quench rate etc); Better understanding that might help making a more quantitative link with fragmentation processes and eruptive dynamics;

Is anyone aware of recent or old studies which could help in understanding the appearance and change of iridescence on basaltic glass surfaces? Thanks in advance,

Best, Andrea

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