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The results presented here – that the visible tephra layers OxT-5163, -5165, and -5166<br />
correlate to the Hekla 1693 eruption – provide further chronological information about the<br />
Vatnsfjörður site. Further integration of tephrochronogical analysis with archaeological<br />
interpretation, will aid in reconstructing the sequence at the site as well as its position within<br />
the wider region over time.<br />
Acknowledgements<br />
The author thanks Hertford College, Oxford, for providing partial funding for this research.<br />
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