TY - JOUR
T1 - Distal deposition of tephra from the Eyjafjallajökull 2010 summit eruption
AU - Stevenson, John
AU - Loughlin, Susan
AU - Rae, C.
AU - Thordarson, Thorvaldur
AU - Milodowski, Antoni
AU - Gilbert, Jennie
AU - Harangi, Szabolcs
AU - Lukács, Reka
AU - Højgaard, Bartal
AU - Árting, Uni
AU - Pyne-O'Donnell, Sean
AU - MacLeod, Alison
AU - Whitney, Bronwen
AU - Cassidy, Mike
PY - 2012/9
Y1 - 2012/9
N2 - The 2010 Eyjafjallajökull lasted 39 days and had 4 different phases, of which the first and third (14–18 April and 5–6 May) were most intense. Most of this period was dominated by winds with a northerly component that carried tephra toward Europe, where it was deposited in a number of locations and was sampled by rain gauges or buckets, surface swabs, sticky-tape samples and air filtering. In the UK, tephra was collected from each of the Phases 1–3 with a combined range of latitudes spanning the length of the country. The modal grain size of tephra in the rain gauge samples was 25 μm, but the largest grains were 100 μm in diameter and highly vesicular. The mass loading was equivalent to 8–218 shards cm−2, which is comparable to tephra layers from much larger past eruptions. Falling tephra was collected on sticky tape in the English Midlands on 19, 20 and 21st April (Phase 2), and was dominated by aggregate clasts (mean diameter 85 μm, component grains
AB - The 2010 Eyjafjallajökull lasted 39 days and had 4 different phases, of which the first and third (14–18 April and 5–6 May) were most intense. Most of this period was dominated by winds with a northerly component that carried tephra toward Europe, where it was deposited in a number of locations and was sampled by rain gauges or buckets, surface swabs, sticky-tape samples and air filtering. In the UK, tephra was collected from each of the Phases 1–3 with a combined range of latitudes spanning the length of the country. The modal grain size of tephra in the rain gauge samples was 25 μm, but the largest grains were 100 μm in diameter and highly vesicular. The mass loading was equivalent to 8–218 shards cm−2, which is comparable to tephra layers from much larger past eruptions. Falling tephra was collected on sticky tape in the English Midlands on 19, 20 and 21st April (Phase 2), and was dominated by aggregate clasts (mean diameter 85 μm, component grains
KW - Eyjafjallajökull
KW - Iceland
KW - dispersal
KW - explosive
KW - tephra
KW - tephrochronology
U2 - 10.1029/2011JB008904
DO - 10.1029/2011JB008904
M3 - Article
SN - 0148-0227
VL - 117
JO - Journal of Geophysical Research: Solid Earth
JF - Journal of Geophysical Research: Solid Earth
IS - B9
ER -