The bell tower of the Manila Cathedral after the series of destructive earthquakes of July 1880.The ruins of Loon Church after the 2013 Bohol earthquake.
Ten deadliest recorded earthquakes in the Philippines since the 1600s
Only the church tower remains of the Cagsawa Church, which was buried by the 1814 eruption of Mayon Volcano.The eruption column of the modern Mount Pinatubo on June 12, 1991, three days before the climactic eruption.Map of Pinatubo showing nearby peaks and the evacuation zones.
This section needs to be updated. Please help update this article to reflect recent events or newly available information.(June 2026)
There was a scare in 1995 but PHIVOLCS investigation at the time did not disclose any unusual activity, and no unusual activity has been reported since.
Currently on eruption since January 12, 2020. Eruptions have also destroyed numerous lakeside towns, burying them with volcanic ash or submerged them by rising lake waters displaced by the erupted material. The towns of Lipa, Taal, Sala, Bauan and Tanauan were formerly located along Taal Lake. Presently, only three towns are on the lake's shore. Remnants of the old lakeside towns are reported to be seen under the lake's waters.[50]
The most destructive eruption of Mayon occurred on February 1, 1814 (VEI=4). Lava flowed but not as much compared to the 1766 eruption; Instead, the volcano was belching dark ash and eventually bombarded the town of Cagsawa with tephra that buried it. Trees were burned; rivers were certainly damaged. Proximate areas were also devastated by the eruption, with ash accumulating to 9m (30ft) in depth. In Albay, a total of 2,200 locals perished in what is considered to be the most lethal eruption in Mayon's history; estimates by PHIVOLCS list the casualties at about 1,200, however. The eruption is believed to have contributed to the accumulation of atmospheric ash,[citation needed] capped by the catastrophic eruption of Mount Tambora in 1815, that led to the Year Without a Summer in 1816.
The most active volcano in the Visayas, Kanlaon has erupted 26 times since 1919. Eruptions are typically phreatic explosions of small-to-moderate size that produce minor ash falls near the volcano. In 1902, the eruption was classified as strombolian, typified by the ejection of incandescentcinder, lapilli and lava bombs.
Bulusan is generally known for its sudden steam-driven or phreatic explosions. It has erupted 16 times since 1885 and is considered as the 4th most active volcano in the Philippines after Mayon, Taal, and Kanlaon. There are evacuation procedures in place for parts of the peninsula, the farms nearest the volcano are evacuated, and many of the village schools are closed if it is considered possible that a more destructive eruption could occur.
On February 16, 1871, earthquakes and subterranean rumblings began to be felt in Camiguin, which increased in severity until April 30 when a volcanic fissure opened up 400 yards southwest of the village of Catarman, on the northwest flank of the Hibok-Hibok Volcano. From the opening, lava was continuously ejected and poured into the sea for four years destroying the town. At the same time, the vent started gaining in height and width thus forming Mt. Vulcan. In 1875, the Challenger expedition visited the area, and described the mountain as a dome, about 1,950 feet (590m) in height, without any crater, but still smoking and incandescent at the top.[52]
↑"Significant earthquakes: Philippines". National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information. Retrieved 2023-12-18.
↑Del Rosario, Eduardo D (August 9, 2011). Final Report on Typhoon "Yolanda" (Haiyan)(PDF) (Report). Philippine National Disaster Risk Reduction and Management Council. pp.77–148. Archived(PDF) from the original on November 5, 2020. Retrieved March 27, 2022.
↑Olavo Rasquinho; Jae Hyun Shim; Yun Tae Kim; Jae Chan Ahn; Chi Hun Lee; In Sung Jung; Gmma Dalena; Preminda Joseph Fernando; Susan R. Espinueva; Socrates F. Paat Jr.; Nivagine Nievares & Tess Pajarillo (December 2012). Assessment Report of the Damages Caused by Tropical Storm Washi(PDF) (Report). ESCAP/WMO Typhoon Committee. ISBN978-99965-817-6-2. Retrieved May 1, 2015.
12J. L. H. Paulhaus (1973). World Meteorological Organization Operational Hydrology Report No. 1: Manual For Estimation of Probable Maximum Precipitation. World Meteorological Organization. p.178.
↑Padgett, Gary; Kevin Boyle; John Wallace; Huang Chunliang; Simon Clarke (October 26, 2006). "Monthly Global Tropical Cyclone Summary June 2004". Australian Severe Weather Index. Jimmy Deguara. Retrieved January 13, 2007.
↑Narciso O. Itoralba (December 1981). Annual Tropical Cyclone Report 1977. Philippine Atmospheric, Geophysical and Astronomical Services Administration. p.65.
↑Del Rosario, Eduardo D (13 November 2015). Final Report on Typhoon "Yolanda" (Haiyan)(PDF) (Report). Philippine National Disaster Risk Reduction and Management Council. Archived from the original(PDF) on 5 November 2020. Retrieved 8 October 2025.
↑Ramos, Benito T (25 December 2012). Sitrep No: 38 re: Effects of Typhoon "Pablo" (Bopha)(PDF) (Report). Philippine National Disaster Risk Reduction and Management Council. Archived(PDF) from the original on 21 January 2013. Retrieved 1 October 2025.
↑Gile, Rob P; Bulquerin, J. E. M; Duran, Samuel F (22 August 2023). Tropical Cyclone Preliminary Report: Super Typhoon Egay (Doksuri)(PDF) (Report). Philippine Atmospheric, Geophysical and Astronomical Services Administration. Archived(PDF) from the original on 26 April 2025. Retrieved 27 September 2025.