Report on Taal (Philippines) — 5 February-11 February 2020
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
5 February-11 February 2020
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2020. Report on Taal (Philippines). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 5 February-11 February 2020. Smithsonian Institution and US Geological Survey.
14.002°N, 120.993°E; summit elev. 311 m
All times are local (unless otherwise noted)
PHIVOLCS reported that whitish steam plumes rose as high as 300 m above Taal’s main vent during 5-11 February and drifted SW. Sulfur dioxide emissions ranged from values below detectable limits to a high of 116 tonnes per day (on 8 February). Weak steaming (plumes 10-20 m high) from ground cracks was visible along the Daang Kastila trail which connects the N part of Volcano Island to the N part of the main crater. According to the Disaster Response Operations Monitoring and Information Center (DROMIC) there were a total of 17,088 people in 110 evacuation centers, and an additional 211,729 people were staying at other locations as of 10 February. The Alert Level remained at 3 (on a scale of 0-5) and PHIVOLCS recommended no entry onto Volcano Island and Taal Lake, nor into towns W of the island within a 7-km radius.
Geological Summary. Taal is one of the most active volcanoes in the Philippines and has produced some of its most powerful historical eruptions. Though not topographically prominent, its prehistorical eruptions have greatly changed the landscape of SW Luzon. The 15 x 20 km Talisay (Taal) caldera is largely filled by Lake Taal, whose 267 km2 surface lies only 3 m above sea level. The maximum depth of the lake is 160 m, and several eruptive centers lie submerged beneath the lake. The 5-km-wide Volcano Island in north-central Lake Taal is the location of all historical eruptions. The island is composed of coalescing small stratovolcanoes, tuff rings, and scoria cones that have grown about 25% in area during historical time. Powerful pyroclastic flows and surges from historical eruptions have caused many fatalities.