| Mayon | 1827 Jun 27-1828 Feb | 6 | | Vulcanian, pyroclastic flows, bombs, lava flows; 300 m high eruption column | | *Vulcanian | Camalig (lahar) | |
| Bulusan | 1916 Jan 18 | 6 | Summit Crater | No incandescence could be seen from Irosin but people in Monbon claim to have seen fire; the incandescence can be explained by static electricity, the particles of ash becoming electrified by friction and discharging in the moist atmosphere; Ejection of steam and fine solid not pumiceous sand | Phreatic | Phreatic | Plume southwest drift, ash reached 25- 30km radius; 0.5cm thick in Irosin town | V091 Goldsberry 1916, (Goldsberry, 1916); V116 Saderra Maso (Maso, n.d.) |
| Kanlaon | 1894 | 6 | crater | Normal explosions | | Phreatic | | (Padang, 1953) |
| Taal | 1641 | 6 | Main Crater | “two craters opened up” (PHIVOLCS, 1991, p.31) | Phreatic, tephra fall | Phreatic | Activity confined at Volcano Island | Delos Reyes et. al., 2018. “A synthesis and review of historical eruptions at Taal Volcano, Southern Luzon, Philippines" |
| Makaturing | 1858-Feb-18 | 6 | | | | | Numerous E-W shocks felt at Pollok and then Makaturing began erupting violently | |
| Ragang | 1871-Dec-08 | 6 | | | | | | |
| Didicas | 1978 Jan 6-9 | 6 | | | Explosive, phreatic | Phreatic | | |
| Smith | 1924 | 5 | flank | | Normal ash explosion | Phreatic | | |
| Mayon | 1814 Feb 1 | 5 | | Plinian, pyroclastic flows, volcanic lightning, lahar,bomb | | Plinian | Camalig, Cagsaua, Budiao, Guinobatan, half of Albay CASUALTIES: 1200; MOST DESTRUCTIVE ERUPTION | |
| Bulusan | 1894 | 5 | Summit Crater (implicit) | Light outburst with ejection of ashes. | Phreatic | | | V012 Saderra Maso (Maso, 1919) |
| Kanlaon | 1893 | 5 | crater | Considerable ashfall | | Phreatic | | (Becker, 1901); (Padang, 1953) |
| Taal | 1635 | 5 | Main Crater | | | | | Delos Reyes et. al., 2018. “A synthesis and review of historical eruptions at Taal Volcano, Southern Luzon, Philippines" |
| Makaturing | 1856-Dec-01 | 5 | | | | | Volcanic cloud obscured the sun at Pollok and ashes reached Zamboanga 230 km away | |
| Ragang | 1858-Feb-18 | 5 | | | | | | |
| Didicas | 1969-Mar-21 | 5 | | | Dome building, lava flow | | | |
| Iriga | 1110+-30 years BP (Conventional 14C age) | 4 | | | | Phreatomagmatic Explosive Eruption | It produced base surges that affected inner parts of the Buhi avalanche scar. The accompanying ashfall formed a 2-cm-thick layer of ash in the sediments of Buhi Lake. | Belousov et al, 2023 |
| Smith | 1918-May-17 | 4 | flank | | Normal ash explosion | Phreatic | | |
| Babuyan Claro | 1917 | 4 | crater | | Explosive | | | |
| Mayon | 1811 Oct 5-6 | 4 | | Vulcanian, lava flow, pyroclastic flows, bombs, ashfall | | *Vulcanian | | |
| Bulusan | 1892 | 4 | Summit Crater (implicit) | Mild eruption | Phreatic | Phreatic | | V239 MLBautista (Bautista, n.d.) |