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The formation of Helgafell, SW-Iceland, a monogenetic subglacial hyaloclastite ridge: Sedimentology, hydrology and ice-volcano interaction.
Helgafell, a little-eroded basaltic hyaloclastite ridge in southwest Iceland, formed in a single eruption under a Pleistocene ice sheet. The ice thickness at the eruption site was at least 500 m and it was probably located some 15 km from the glacier�s snout. The eruption created a 2 km long, 0.8
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