Biased Volcanic Hazard Assessment Due to Incomplete Eruption Records on Ocean Islands: An Example of Sete Cidades Volcano, Azores

Ulrich Kueppers,José Pacheco,Diego Perugini,Julia Neukampf,Francesca Forni,Adriano Pimentel,Ben Ellis,Gabriela Queiroz

doi:10.3389/feart.2019.00122

Abstract

Sete Cidades is the westernmost central volcano of Sao Miguel Island, Azores. Although currently dormant, it has been the most active volcano on the island in the past 5 ky, with at least 17 trachytic intra-caldera explosive eruptions, some of which of sub-Plinian. The last paroxysmal explosive eruption took place ~16 ka, enlarging the summit caldera to its present dimensions, and is recorded by the Santa Barbara Formation. It is well known that explosive eruptions pose serious hazards to local communities and may have worldwide impacts. However, the products of explosive eruptions on volcanic islands are almost inevitably incompletely preserved, thereby impeding our ability to precisely determine eruptive source parameters. These constraints are frequently observed on volcanic ocean islands, such as the Azores islands, where it is estimated that a significant portion of the erupted material is deposited into the sea. We here present evidence of a distal deposit (>25 km from the vent) that can be correlated with the pumice fall deposit of the Santa Barbara Formation based on deposit characteristics, textural features and geochemistry. This is the first evidence of a decimeter-thick distal deposit of Sete Cidades volcano in the central part of Sao Miguel Island, which allows to constrain eruptive source parameters and wind conditions. The predominant winds blowing from westerly directions makes Sete Cidades the most hazardous volcano for the entire island of Sao Miguel with its current population of >137,000 inhabitants. Most critically, the main harbor, only airport and hospital are located in the capital city of Ponta Delgada, ~12 km SE from Sete Cidades caldera. In case of a future explosive eruption, under westerly-blowing wind conditions, the impact on Sao Miguel will be catastrophic, with long-term economic consequences.

Highlights

Explosive volcanic eruptions are recognized as one of the most violent natural events that pose a plethora of hazards to local communities, economic sectors, and infrastructure, but may cause widespread disruption of air traffic (e.g., Mazzocchi et al, 2010; Wilson et al, 2012; Biass et al, 2014; Scaini et al, 2014)
Stratigraphic correlations were facilitated by the presence of magmatic mafic enclaves (MME) in juvenile pumice clasts, which increase in frequency and size toward the top of the pyroclastic sequence (Queiroz et al, 2015; Porreca et al, 2018)
The last major explosive eruption (∼16 ka) enlarged the summit caldera to its present-day dimensions and produced a complex pyroclastic sequence known as the Santa Bárbara Formation (SBF)

Summary

Introduction

Explosive volcanic eruptions are recognized as one of the most violent natural events that pose a plethora of hazards to local communities, economic sectors, and infrastructure, but may cause widespread disruption of air traffic (e.g., Mazzocchi et al, 2010; Wilson et al, 2012; Biass et al, 2014; Scaini et al, 2014). This threat is even greater for volcanic islands as the ocean is a strong impediment for the evacuation of large numbers of people. Ponta Delgada is frequently downwind from 7C under the predominant westerly winds, posing serious concerns regarding the assessment of volcanic hazard (Pimentel et al, 2006; Cole et al, 2008; Gaspar et al, 2015)

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