Rhyolitic volcano–ice interactions in Iceland

• Published in: Journal of Volcanology and Geothermal Research
• Main Author: McGarvie, Dave
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2009
• Subjects: Bláhnúkur; Prestahnúkur; Iceland
• Online Access: https://oro.open.ac.uk/16340/; https://doi.org/10.1016/j.jvolgeores.2008.11.019

Iceland contains an abundance and diversity of rhyolitic edifices produced during volcano–ice interactions (glaciovolcanism) that is unmatched by any other volcanic province, with an estimated 350 km3 erupted during the past 0.8 Ma from at least fifteen volcanic systems. This review summarises research undertaken during the past decade and provides a new summary of the distribution of rhyolitic glaciovolcanic rocks erupted during the past 0.8 Ma. Descriptions of effusion-dominated edifices focus on the two best-studied edifices — the c.0.6 km3 and 570 m high Prestahnúkur edifice and the smaller-volume (< 0.1 km3) drape of Bláhnúkur. Both show little or no evidence of magmatic fragmentation (i.e. driven by volatile exsolution), but both show abundant evidence of quench fragmentation and meltback of ice walls. A particular feature of Prestahnúkur is its sheet-like lava bodies which are interpreted as sills that intruded the ice–edifice interface. Rhyolitic tuyas are products of sustained eruptions into thick ice, and form distinctive steep-sided edifices with flat or broad dome-like tops. They are 300–700 m high with volumes up to 2 km3 (though 0.5–1.0 km3 is more typical). Initial vigorous phreatomagmatic eruptions within well-drained ice vaults build steep-sided piles of tephra confined by ice walls. Gradual upwards increases in inflated clasts point to the decreasing involvement of meltwater and the increasing ability of the magma to vesiculate. As the eruption progresses and terminates, non-explosive degassing produces lava caps up to 300 m thick. Öræfajökull is a stratovolcano illustrating complex volcano–ice interactions generated when rhyolitic lavas erupt onto steeper slopes and encounter ice of variable thickness and properties (e.g. fracturing). Eruptive units record dramatic ice thickness fluctuations of up to 500 m in valley glaciers between eruptions, which emphasises that useful palaeoenvironmental information can be gleaned from detailed studies of volcano–ice interactions. Considerable value is ...