Event | Date | Notes |
Eruption of Mount Panay | Pleistocene | Last eruptive activity is thought to be Pleistocene, about 500,000 years ago. |
Eruption of Mount Arayat | Holocene | There are no cultural records of historical eruptions. However, weak steaming is currently present in some of the heavily eroded vents on the North Western side of the summit. The ancient eruptions were said to have caused the formation of a Lava Dome on the Western Slopes of the mountain known as White Rock which makes a nice tourist destination and is usually a field trip destination for students of Pampanga Agricultural College. The Arayat amphitheatre is said to have been caused by the summit's collapse on the western side but a much deeper crater is present on the eastern side, it was said that the mountain was once a volcanic island, until eruptions covered the surrounding area with soil, eruptions were said to be the possible cause of a theorized re-route of Pampanga River which is said to have once passed on the western side rather than eastern side where it currently moves |
Eruption of Mount Natib | Pleistocene or Holocene | There are no historical eruptions within the Natib caldera complex. Studies in 1991 indicate that the last eruptive activity was probably Holocene to upper Pleistocene. An earlier study in 1971 dated the eruptive products between 69,000 +/- 27,000 years old. |
Eruption of Mt.Masaraga | Holocene | There are no historical eruptions from the volcano with the last eruptive activity dated as Holocene as reported by the Global Volcanism Program. Thick lava flows from that period are present on the flanks of Mount Masaraga, an understudied volcano in the Philippines. |
Eruption of Laguna Caldera | C28,000 BP | The caldera, whose lake surface is only 1m above sea level, may have formed by least two major eruptions of about 1 million and 27,000-29,000 years ago. |
Eruption of Mount Malinao | 60,000 BP | There are no historical eruptions from Malinao which is believed to have been active from about 500,000 years ago until 60,000 years ago. |
Eruption of Cuernos de Negros | 12,000 BC | An earlier study in 1971 dated the eruptive products between 69,000 +/- 27,000 years old. |
Eruption of Ancestral Pinatubo | Holocene 1.1 million years ago | The activity of Ancestral Pinatubo seems to have begun about 1.1 million years ago and probably ended tens of thousands or more before the birth of 'Modern Pinatubo'. Much of the rugged land surrounding the present volcano consists of remnants of 'ancestral' Pinatubo. It was an andesite and dacite stratovolcano with its eruptive activity much less explosive than modern Pinatubo. |
Eruption of Mt.Mariveles | 2050 BCE | There are no recorded historical eruptions from Mariveles caldera, with the last activity indicated by Radiocarbon dating occurring around mid-Holocene or about 2050 BCE. |
Period | Start Date | Extinction | Date | Cause |
Mid-Holocene | | Extinction of Large Mammals | 2050 BC | Volcanic Eruption. and Climate change |
Holocene | 500,000 years ago | Extinction of Large Animals | | Volcanic Eruptions.A volcanic eruption occurred In the present location of Taal lake, during Mid-Holocene, causes the Species of Proboscideans like Stegodon to become exitinct. |
Pleistocene | 2 million -13,000 yrs ago | Quaternary extinction event | 640,000, 74,000, and 13,000 years ago | Clovis comet? Eruption of Super Volcano? Hunting by humans? Climate change? |
Pliocene | | Pliocene–Pleistocene boundary marine extinction | 2 Ma | Supernova in the Scorpius-Centaurus OB association |