Report on Oraefajokull (Iceland) — 20 December-26 December 2017
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
20 December-26 December 2017
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2017. Report on Oraefajokull (Iceland). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 20 December-26 December 2017. Smithsonian Institution and US Geological Survey.
64°N, 16.65°W; summit elev. 2010 m
All times are local (unless otherwise noted)
On 22 December IMO reported that activity at Öræfajökull had been fairly stable during the previous weeks, though still above background levels; the Aviation Color Code remained at Yellow. In December the largest earthquake detected was a M2.5, but most events were smaller than M1. Earthquakes were located close to the caldera at depths between 2 and 10 km.
Geological Summary. Öræfajökull, Iceland's highest peak, is a broad glacier-clad central volcano at the SE end of the Vatnajökull icecap. A 4 x 5 km subglacial caldera truncates the summit of the dominantly basaltic and rhyolitic volcano. The extensive summit icecap is drained through deep glacial valleys dissecting the SW-to-SE flanks. It is the largest-volume volcano in Iceland, and was mostly constructed during Pleistocene glacial and interglacial periods. Holocene activity has been dominated by explosive summit eruptions, although flank lava effusions have also occurred. A major silicic eruption in 1362 CE was Iceland's largest historical explosive eruption. It and another eruption during 1727-28 were accompanied by major jökulhlaups (glacier outburst floods) that caused property damage and fatalities.