Geochemistry, dispersal, volumes and chronology of Holocene silicic tephra layers from the Katla volcanic system, Iceland

• Published in: Journal of Quaternary Science
• Main Authors: Larsen, Gudrún, Newton, Anthony J., Dugmore, Andrew J., Vilmundardóttir, Elsa G.
• Other Authors: Leverhulme Trust, Natural Environment Research Council (UK), National Science Foundation (USA), National Geographic Society, RANNÍS (Iceland)
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2001
• Subjects: Eldgjá; Katla; Iceland; North Atlantic
• Online Access: http://dx.doi.org/10.1002/jqs.587; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.587; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.587

Abstract At least 12 silicic tephra layers (SILK tephras) erupted between ca. 6600 and ca. 1675 yr BP from the Katla volcanic system, have been identified in southern Iceland. In addition to providing significant new knowledge on the Holocene volcanism of the Katla system which typically produces basaltic tephra, the SILK tephras form distinct and precise isochronous marker horizons in a climatically sensitive location close to both the atmospheric and marine polar fronts. With one exception the SILK tephras have a narrow compositional range, with SiO 2 between 63 and 67%. Geochemically they are indistinguishable from ocean transported pumice found on beaches in the North Atlantic region, although they differ significantly from the silicic component of the North Atlantic Ash Zone One (NAAZO). Volumes of airborne SILK tephra range from 0.05 to 0.3 km 3 . We present new isopach maps of the six largest layers and demonstrate that they originate within the Katla caldera. The apparently stable magma system conditions that produced the SILK tephras may have been established as a consequence of the eruption of the silicic component of NAAZO (ca. 10.3 ka) and disrupted by another large‐scale event, the tenth century ad Eldgjá eruption (ca. 1 ka). Despite the current long repose, silicic activity of this type may occur again in the future, presenting hitherto unknown hazards. Copyright © 2001 John Wiley & Sons, Ltd.