In the past 24-hour period, the Taal Volcano Network recorded one hundred and sixty-four (164) volcanic earthquakes, including sixty-seven (67) episodes of volcanic tremor having durations of one (1) to two (2) minutes and three (3) hybrid events.
Activity at the Main Crater consisted of weak emission of steam-laden plumes from fumarolic vents that rose 20 meters high. Sulfur dioxide (SO2) emission that averaged 605 tonnes/day was measured yesterday, 17 March 2021.
Temperature highs of 71.8°C and pH of 1.59 were last measured from the Main Crater Lake respectively on 04 March and 12 February 2021.
Ground deformation parameters from electronic tilt, continuous GPS and InSAR data analysis indicated a very slow and steady inflation and expansion of the Taal region since after the January 2020 eruption. These parameters may indicate increased magmatic activity at shallow depths beneath the edifice.
Alert Level 2 (Increased Unrest) is maintained over Taal Volcano. DOST-PHIVOLCS reminds the public that at Alert Level 2, sudden steam-driven or phreatic explosions, volcanic earthquakes, minor ashfall, and lethal accumulations or expulsions of volcanic gas can occur and threaten areas within the Taal Volcano Island (TVI).
Taal Volcano records 164 volcanic earthquakes in past 24 hours
DOST-PHIVOLCS strongly recommends that entry into TVI, Taal’s Permanent Danger Zone or PDZ, especially the vicinities of the Main Crater and the Daang Kastila fissure, must remain strictly prohibited.
Civil aviation authorities must advise pilots to avoid flying close to the volcano as airborne ash and ballistic fragments from sudden explosions and wind-remobilized ash may pose hazards to aircraft.
DOST-PHIVOLCS is closely monitoring Taal Volcano’s activity and any new significant development will be immediately communicated to all stakeholders.
Meanwhile, Pinatubo Volcano’s monitoring network recorded twenty-six (26) volcanic earthquakes during the 24-hour observation period.
Alert Level 1 (Abnormal) prevails over Pinatubo Volcano, which means that there is low-level unrest that may be related to tectonic processes beneath its edifice and that no imminent eruption is foreseen.