TY - JOUR
T1 - Black Point – Pyroclasts of a Surtseyan eruption show no change during edifice growth to the surface from 100 m water depth
AU - Verolino, A.
AU - White, J. D.L.
AU - Dürig, T.
AU - Cappuccio, F.
N1 - Publisher Copyright:
© 2019 Elsevier B.V.
PY - 2019/10/15
Y1 - 2019/10/15
N2 - Surtseyan eruptions have long been studied from their edifice deposits, emplaced subaqueously or subaerially. Here we characterize a Surtseyan eruption from both edifice and ash-sheet deposits using a combination of techniques. The volcano studied is Black Point, which erupted into Lake Russell about 13,000 years ago from a water depth of 105 m, producing a total of ~0.8 km3 of tephra. The techniques, applied to samples acquired by targeted sampling based on geological observations in the field, include geochemical characterization of the eruption products, grain-size analysis of the ash-size fraction at proximal and medial sites, three-dimensional characterization of vesicles in lapilli, and particle-shape analysis for ash grains using the recently introduced freeware PARTISAN
AB - Surtseyan eruptions have long been studied from their edifice deposits, emplaced subaqueously or subaerially. Here we characterize a Surtseyan eruption from both edifice and ash-sheet deposits using a combination of techniques. The volcano studied is Black Point, which erupted into Lake Russell about 13,000 years ago from a water depth of 105 m, producing a total of ~0.8 km3 of tephra. The techniques, applied to samples acquired by targeted sampling based on geological observations in the field, include geochemical characterization of the eruption products, grain-size analysis of the ash-size fraction at proximal and medial sites, three-dimensional characterization of vesicles in lapilli, and particle-shape analysis for ash grains using the recently introduced freeware PARTISAN
KW - Black Point
KW - Mono Lake
KW - Particle shape analysis
KW - PARTISAN©
KW - Surtseyan
KW - Vesicularity
UR - http://www.scopus.com/inward/record.url?scp=85069741096&partnerID=8YFLogxK
U2 - 10.1016/j.jvolgeores.2019.07.013
DO - 10.1016/j.jvolgeores.2019.07.013
M3 - Article
AN - SCOPUS:85069741096
SN - 0377-0273
VL - 384
SP - 85
EP - 102
JO - Journal of Volcanology and Geothermal Research
JF - Journal of Volcanology and Geothermal Research
ER -