Black Point – Pyroclasts of a Surtseyan eruption show no change during edifice growth to the surface from 100 m water depth

A. Verolino*, J. D.L. White, T. Dürig, F. Cappuccio

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)

Abstract

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

Original languageEnglish
Pages (from-to)85-102
Number of pages18
JournalJournal of Volcanology and Geothermal Research
Volume384
DOIs
Publication statusPublished - 15 Oct 2019

Bibliographical note

Publisher Copyright:
© 2019 Elsevier B.V.

Other keywords

  • Black Point
  • Mono Lake
  • Particle shape analysis
  • PARTISAN©
  • Surtseyan
  • Vesicularity

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