Report on Eyjafjallajokull (Iceland) — 23 June-29 June 2010
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 23 June-29 June 2010
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2010. Report on Eyjafjallajokull (Iceland). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 23 June-29 June 2010. Smithsonian Institution and US Geological Survey.
63.633°N, 19.633°W; summit elev. 1651 m
All times are local (unless otherwise noted)
The Nordic Volcanological Center (NVC) at the Institute of Earth Sciences reported on 23 June that small ash clouds from Eyjafjallajökull's summit caldera were occasionally seen, but dispersed quickly. Water was slowly accumulating in the crater because ice was no longer in contact with hot material.
Geologic Background. Eyjafjallajökull (also known as Eyjafjöll) is located west of Katla volcano. It consists of an E-W-trending, elongated ice-covered stratovolcano with a 2.5-km-wide summit caldera. Fissure-fed lava flows occur on both the E and W flanks, but are more prominent on the western side. Although the 1666-m-high volcano has erupted during historical time, it has been less active than other volcanoes of Iceland's eastern volcanic zone, and relatively few Holocene lava flows are known. An intrusion beneath the S flank from July-December 1999 was accompanied by increased seismic activity and was constrained by tilt measurements, GPS-geodesy and InSAR. The last historical activity prior to an eruption in 2010 produced intermediate-to-silicic tephra from the central caldera during December 1821 to January 1823.
Source: Institute of Earth Sciences