TY - JOUR
T1 - Three magmatic components in the 1973 eruption of Eldfell volcano, Iceland
T2 - Evidence from plagioclase crystal size distribution (CSD) and geochemistry
AU - Higgins, Michael D.
AU - Roberge, Julie
N1 - Funding Information:
We thank Ármann Höskuldsson for his hospitality on the island of Heimaey and his assistance in the field. We also thank Judit Ozoray and Kathy Cashman for previous revisions, suggestions and helpful discussions of many topics included in this paper. The careful reviews by Hannes Mattsson and Alex Mock improved the manuscript. We express our gratitude to Diana Roman, and our colleagues at the Université du Québec à Chicoutimi and the University of Oregon, for their advice and help. This research was partly funded by grants from the Natural Science and Engineering Research Council of Canada to M. D. Higgins.
PY - 2007/3/15
Y1 - 2007/3/15
N2 - The 1973 eruption of Eldfell volcano, Iceland, appears to have been a short, simple event, but textural and geochemical evidence suggest that it may have had three different magmatic components. The first-erupted fissure magmas were chemically evolved, rich in plagioclase (∼ 18%) and had shallow, straight crystal size distribution (CSD) curves. The early lavas were less evolved chemically, had lower plagioclase contents (∼ 13%) and steeper, slightly concave up CSDs. The late lavas were chemically similar to the early lavas, but even richer in plagioclase than the initial magmas (∼ 24%) and had the steepest CSDs. There was no chemical evidence for plagioclase fractionation, but compositional diversity could be produced by clinopyroxene fractionation which must have occurred at depth. We propose that the eruption started with old, coarsened (Ostwald ripened) magma left over from a previous eruption, possibly that which produced Surtsey Island ten years earlier. The early flows may be mixtures of small amounts of this old magma with a new, low crystallinity, uncoarsened magma or a completely new magma. The late flows are another new magma from depth, chemically similar to the early flows, but which has grown plagioclase under increasing saturation (undercooling) perhaps during its ascent. All three magmatic components may have originated from the same parent, but had varying degrees of clinopyroxene fractionation, plagioclase nucleation and growth, and coarsening.
AB - The 1973 eruption of Eldfell volcano, Iceland, appears to have been a short, simple event, but textural and geochemical evidence suggest that it may have had three different magmatic components. The first-erupted fissure magmas were chemically evolved, rich in plagioclase (∼ 18%) and had shallow, straight crystal size distribution (CSD) curves. The early lavas were less evolved chemically, had lower plagioclase contents (∼ 13%) and steeper, slightly concave up CSDs. The late lavas were chemically similar to the early lavas, but even richer in plagioclase than the initial magmas (∼ 24%) and had the steepest CSDs. There was no chemical evidence for plagioclase fractionation, but compositional diversity could be produced by clinopyroxene fractionation which must have occurred at depth. We propose that the eruption started with old, coarsened (Ostwald ripened) magma left over from a previous eruption, possibly that which produced Surtsey Island ten years earlier. The early flows may be mixtures of small amounts of this old magma with a new, low crystallinity, uncoarsened magma or a completely new magma. The late flows are another new magma from depth, chemically similar to the early flows, but which has grown plagioclase under increasing saturation (undercooling) perhaps during its ascent. All three magmatic components may have originated from the same parent, but had varying degrees of clinopyroxene fractionation, plagioclase nucleation and growth, and coarsening.
KW - CSD
KW - Eldfell
KW - Iceland
KW - basalt
KW - coarsening
KW - crystal size distribution
KW - magma mixing
KW - texture
UR - http://www.scopus.com/inward/record.url?scp=33846928020&partnerID=8YFLogxK
U2 - 10.1016/j.jvolgeores.2006.12.002
DO - 10.1016/j.jvolgeores.2006.12.002
M3 - Artículo
SN - 0377-0273
VL - 161
SP - 247
EP - 260
JO - Journal of Volcanology and Geothermal Research
JF - Journal of Volcanology and Geothermal Research
IS - 3
ER -