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= Historical eruptions and hazards at Bogoslof volcano, Alaska =
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Bogoslof volcano is a submarine volcano in the southern<br />
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Bering Sea (53.9272°N, 168.0344°W), located 100 kilometers<br />
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(km) west of Dutch Harbor/Unalaska, and 40 km north<br />
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of Umnak Island. The volcano has a relatively long history of<br />
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scientific investigation and several of its historical eruptions<br />
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have been documented during brief visits to the area since the<br />
      "name": "Historical eruptions and hazards at Bogoslof volcano, Alaska",
late 1700s. The purpose of this report is to provide a modern<br />
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volcanological perspective on past eruptions of Bogoslof and<br />
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to readdress some of the eruptive phenomena described in<br />
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historical documents and reports. We also present for the first<br />
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time a brief analysis of the hazards posed by Bogoslof eruptions.<br />
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While this report was being prepared, Bogoslof volcano<br />
          "url": "https://pubs.usgs.gov/publication/sir20185085"
was in an ongoing state of eruptive activity that began in<br />
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mid-December 2016. Detectable eruptive activity ended in late<br />
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August 2017 and the volcano has remained quiet since then.<br />
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Because we have not yet visited Bogoslof Island and have<br />
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only a few distal tephra samples from two eruptive events,<br />
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we will not discuss in detail the 2016–17 eruptive sequence,<br />
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but will provide some information for comparative purposes.<br />
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When more detailed data has been collected, a more extensive<br />
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review of the 2016–17 Bogoslof eruption should be the subject<br />
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of future reports.
          "value": "10.3133/sir20185085",
 
          "url": "https://doi.org/10.3133/sir20185085"
== Table of Contents ==
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* Preface
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* Introduction
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* Geologic Setting
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* Historical Accounts and Observations
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* Hazards Associated with Bogoslof Eruptions
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* References Cited
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      "abstract": "Bogoslof volcano is a submarine volcano in the southernBering Sea (53.9272\u00b0N, 168.0344\u00b0W), located 100 kilometers(km) west of Dutch Harbor/Unalaska, and 40 km northof Umnak Island. The volcano has a relatively long history ofscientific investigation and several of its historical eruptionshave been documented during brief visits to the area since thelate 1700s. The purpose of this report is to provide a modernvolcanological perspective on past eruptions of Bogoslof andto readdress some of the eruptive phenomena described inhistorical documents and reports. We also present for the firsttime a brief analysis of the hazards posed by Bogoslof eruptions.While this report was being prepared, Bogoslof volcanowas in an ongoing state of eruptive activity that began inmid-December 2016. Detectable eruptive activity ended in lateAugust 2017 and the volcano has remained quiet since then.Because we have not yet visited Bogoslof Island and haveonly a few distal tephra samples from two eruptive events,we will not discuss in detail the 2016\u201317 eruptive sequence,but will provide some information for comparative purposes.When more detailed data has been collected, a more extensivereview of the 2016\u201317 Bogoslof eruption should be the subjectof future reports. ",
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Latest revision as of 23:22, 14 August 2024

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