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Volcanic and sedimentary processes during formation of the Saefell tuff-ring, Iceland

Published online by Cambridge University Press:  03 November 2011

Clyde A. Leys
Clyde A. Leys
Affiliation:
BP Minerals International Ltd, R. Padre Antonio Macedo 60, 7540 Santiago do Cacem, Portugal.
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Abstract

The Recent Saefell tuff-ring on Heimaey, Iceland was formed by surtseyan activity in shallow seawater. The tuff-ring has a basal diameter of about 3 km, a maximum rim height of 188 m above sea-level and a crater diameter of 1300 m. Three tuff-units are recognised, separated by unconformities on and inside the crater rim due to syndepositional slumping. The crater contains a nested rim which was constructed above slumped crater tuffs. Directional data indicate strongly directed blasts to the SW at a late stage in the activity.

Throughout the volcanic activity, base-surges formed antidunes, U-shaped channels, vesiculated tuffs, small ripples and plastering structures. One antidune reflects a decrease in surge flow power during deposition and subsequent slumping due to base-surge drag and instabilities developed during growth. On the basis of field characteristics, the structures are divided into those deposited by hot, dry, fast-moving surges and those by cooler, wet, slow-moving surges. Base-surges are compared with turbidity currents and deposition of distinct structures by the head, body and tail regions is interpreted.

Keywords

airfall tuffantidunebase-surgecraterdiatremedirected blastphreatomagmaticpyroclasticreworked tuffslumpingsurge modelSurtsey.
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 74 , Issue 1 , 1983 , pp. 15 - 22
Copyright
Copyright © Royal Society of Edinburgh 1983

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