Subglacial volcanic activity above a lateral dyke path during the 2014–2015 Bárdarbunga-Holuhraun rifting episode, Iceland

• Published in: Bulletin of volcanology 2017-06, Vol.79 (6), p.1, Article 38
• Main Authors: Reynolds, Hannah I., Gudmundsson, Magnús T., Högnadóttir, Thórdís, Magnússon, Eyjólfur, Pálsson, Finnur
• Format: Article
• Language: English
• Subjects: Aircraft; Altimetry; Convection; Earth and Environmental Science; Earth Sciences; Echoes; Echosounding; Evolution; Geologic depressions; Geology; Geophysics/Geodesy; Glaciers; Graben; Groundwater; Groundwater storage; Heat transfer; Hydrothermal activity; Ice; Lava; Magma; Meltwater; Mineralogy; Products; Radar; Research Article; Rifting; Sedimentology; Soundings; Storage capacity; Storage conditions; Time series; Volcanic activity; Volcanic eruptions; Volcanology; Water
• ISSN: 0258-8900; 1432-0819
• DOI: 10.1007/s00445-017-1122-z

The rifting episode associated with the Bárdarbunga-Holuhraun eruption in 2014–2015 included the first observations of major dyke propagation under ice. Three shallow ice depressions (ice cauldrons) with volumes ranging from 1 to 18 million m 3 formed in Dyngjujökull glacier above the 48-km-long lateral path of the magma, at 4, 7 and 12 km from the northern glacier edge. Aircraft-based radar altimetry profiling was used to map the evolution of the cauldrons and construct a time series of the heat transfer rates. Out of the three scenarios explored: (1) onset or increase of hydrothermal activity, (2) convection within vertical fissures filled with water overlying intruded magma and (3) subglacial eruptions, the last option emerges as the only plausible mechanism to explain the rapid heat transfer observed in a location far from known geothermal areas. The thermal signals at two of the cauldrons are consistent with effusive subglacial eruptions. The formation of the northernmost cauldron was more rapid, indicating faster heat transfer rates. Radio-echo sounding data indicate that in contrast to the other two cauldrons, an intrusion of eruptive products occurred into the glacier, reaching 50–60 m above bedrock with the increased magma-ice contact explaining the more rapid heat transfer. We propose that the ~2-m widening associated with graben formation increased the groundwater storage capacity of the bedrock, creating space for the meltwater to be stored, explaining the absence of meltwater pulses draining from Dyngjujökull.