-Falljökull, Kotárjökull and Kvíárjökull.Floods resulting from fissure
eruptions on the upper flanks where the ice is 50–100 m thick. Expected melting
in eruptions is in the range 1,000–10,000 m3/s. Jökulhlaups of this
type can happen anywhere on the slopes from Virkisjökull in the west to
Hrútárjökull in the east. Floods resulting from hot
(
300–600°C) pyroclastic density currents in large
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