4.7 Article

The 2020 Eruption and Large Lateral Dike Emplacement at Taal Volcano, Philippines: Insights From Satellite Radar Data

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 48, Issue 7, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021GL092803

Keywords

InSAR; lateral dike intrusion; Taal 2020 eruption; volcano crisis response; volcano geodesy

Funding

  1. National Aeronautics and Space Administration [281945.02.47.04.51]
  2. JPL RTD program [01STCR- R.18.245.034]
  3. MagmaPropagator project [ANR-18-CE92-0037-01]
  4. Agence Nationale de la Recherche (ANR) [ANR-18-CE92-0037] Funding Source: Agence Nationale de la Recherche (ANR)

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The eruption of Taal volcano in the Philippines after 43 years of dormancy affected over 500,000 people, with deformation analyses revealing a complex pattern of pressure changes in the magma reservoir. The study also highlighted the unique contribution of InSAR data in understanding the volcanic crisis and the recovery process of the magma reservoir post-eruption.
On January 12, 2020, Taal volcano, Philippines, erupted after 43 years of repose, affecting more than 500,000 people. Using interferometric synthetic aperture radar (InSAR) data, we present the pre- to post-eruption analyses of the deformation of Taal. We find that: (1) prior to eruption, the volcano experienced long-term deflation followed by short-term inflation, reflecting the depressurization-pressurization of its similar to 5 km depth magma reservoir; (2) during the eruption, the magma reservoir lost a volume of 0.531 +/- 0.004 km(3) while a 0.643 +/- 0.001 km(3) lateral dike was emplaced; and (3) post-eruption analyses reveal that the magma reservoir started recovery approximately 3 weeks after the main eruptive phase. We propose a conceptual analysis explaining the eruption and address why, despite the large volume of magma emplaced, the dike remained at depth. We also report the unique and significant contribution of InSAR data during the peak of the crisis.

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