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Complex hazard cascade culminating in the Anak Krakatau sector collapse
Thomas R Walter1, Mahmud Haghshenas Haghighi2,3, Felix M Schneider2
1GFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, Telegrafenberg, 14473, Potsdam, Germany. twalter@gfz-potsdam.de.
Nature Communications
|October 3, 2019
Summary
Anak Krakatau volcano
Area of Science:
- Volcanology
- Geophysics
- Natural Hazards
Background:
- Volcanic islands are prone to flank instability and sector collapses.
- Sector collapses can trigger devastating tsunamis, as seen at Anak Krakatau.
Purpose of the Study:
- To investigate the precursor processes leading to the Anak Krakatau sector collapse and tsunami.
- To understand the hazard cascade and improve early detection of flank instability.
Main Methods:
- Utilized multiparametric ground-based and space-borne data.
- Analyzed seismic signals, thermal anomalies, and surface deformation.
Main Results:
- Anak Krakatau showed precursory thermal anomalies and increased surface area before collapse.
- A gradual seaward flank motion was detected on a dipping décollement.
- A small earthquake preceded the flank collapse by two minutes, triggering a fatal tsunami.
Conclusions:
- The Anak Krakatau event highlights a complex hazard cascade initiated by flank instability.
- Understanding precursor processes is crucial for early warning systems for volcanic flank collapses.
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