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High-intensity jökulhlaups have the ability to break off large boulders from bedrock and emplace and rotate them.
These rocks originally carried a remanent magnetization parallel to the geomagnetic field during their formation.
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Floods with recurrence periods on historic time scales may pose an important natural hazard.
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For risk management and planning, it is imperative to understand the history and recurrence of these and similar events.
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The protocol was tested on 44 boulders from 2 historical jökulhlaups in Iceland and found to yield good order-of-magnitude estimates: 72 yr (confidence limits 11–360 yr) versus known 155 yr at the Sólheimajökull jökulhlaup and 290 yr (confidence limits 80–2300 yr) versus known 288 yr for the Kotarjökull jökulhlaup.
The method can therefore be a valuable tool for future dating of cataclysmic events.
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