Abstract
Mossbauer spectra of samples from the 2010 Fimmvorðuhals/Eyjafjallajokull eruption are presented with determinations of the Fe3 + /FeTot ratios. Mossbauer spectra of time series of samples from the Eyjafjallajokull eruption show a change in the characteristics of the erupted material mid-way in the eruption, suggesting changing access of water to the eruption.
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