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Pinatubo

Volcano
The June 12, 1991 eruption column from Mount Pinatubo taken from the east side of Clark Air Base. U.S. Geological Survey Photograph taken on June 12, 1991, 08:51 hours, by Dave Harlow.
The June 12, 1991 eruption column from Mount Pinatubo taken from the east side of Clark Air Base. U.S. Geological Survey Photograph taken on June 12, 1991, 08:51 hours, by Dave Harlow.
Pinatubo volcano exploded spectacularly on 15 June 1991. The Pinatubo eruption on 15 June 1991 was the second largest volcanic eruption of the 20th century. Pinatubo is a complex of lava domes located 100 km NW of Manila city, Luzon Island, Philippines. Prior to the eruption, Pinatubo was a little known volcano and it had been dormant for 400 years. There were no known historic eruptions. Before the eruption in 1991 Pinatubo was 1745 m high (ca. 250 m more than now), and was only 200 m higher than the nearby peaks, which are remnants of older volcanic edifices of Mt Pinatubo and hid it from views from distance. Pinatubo mostly noted for a failed geothermal development project. Eruptions of Mount Pinatubo Pinatubo has had at least 6 periods of activity with large explosive eruptions in its past 35,000 years prior to the 1991 eruption. The 1991 eruption in this context actually ranks as one of the smaller eruptions. An eruption, which occurred 35,000 years ago and probably created the caldera, was likely much bigger.
Volcano type stratovolcano dormant
Location
Summit elevation 1486 m / 4,875 feet
Pinatubo volcano eruptions 1992, 1991 (Plinian eruption), 1450 ± 50 years, 1050 BC ± 500, 3550 BC (?), 7030 BC ± 300, 7460 BC ± 150, 15,000 BC, 33,000 BC
Typical eruption style explosive

Geology of Mt Pinatubo volcano



Regional setting:

Pinatubo is flanked to the west and probably underlain by by the Zambales Ophiolite Complex, an easterly-dipping section of Eocene oceanic crust which was uplifted in the late Oligocene.

The second unit are sediments of the Tarlac Formation, mostly sandstone and siltstone in the older parts, and conglomerates and volcanic sediments and dikes in the younger. The Tarlac formation is found in the north, east and southeast of Pinatubo and formed contemporary with the oldest known volcanic centers in the area, including Mount Mataba or the diorite of the Dizon Mine, the sub-surface remnant of an ancient vent.

The ancient volcanoes of the Tarlac Formation originated from the same east-dipping subduction along the Manila trench that continues to the present.



Ancient Pinatubo:

Pinatubo was formed in 2 stages. The ancestral Pinatubo started to form about 1 million years ago, and built an andesite - dacite stratovolcano whose center was at the same location as today. Remnants of this precessor are seen in the ancient 3.5x4.5 wide caldera. Ancient Pinatubo had a number of flank vents, that formed the domes of Mount Negron, Mount Cuadrado, Mataba, Bituin plug, and the volcanic plug of Tapungho.

Deep erosion in the Sacobia, Porac, Marimla, and Porac River valleys, and weathering of the lavas suggests that activity of the ancestral volcano ended several tens of thousands of years (or more) before the caldera-forming eruption and initial growth of the modern Pinatubo (ca. 35,000 years ago).



Modern Pinataubo:

After the 1991 eruption, scientists (mainly from PHILVOLCS & USGS) carried out intensive fieldwork on the deposits of present-day Pinatubo to analyze its eruptive history. They distinguished at least 6 eruptive periods of modern Pinatubo, characterized by repeated, large explosive eruptions:



Inararo Eruptive Period -- >35,000 14C yr B.P.

The largest eruption in the history of modern Pinatubo occurred 35,000 (radiocarbon) years ago. It deposited up to 100 m or more of pumice and ash flows on all sides of Mount Pinatubo.



Sacobia Eruptive Period -- ~17,000 yr B.P.

A phase of explosive eruptions occurred 17,000 years ago and produced 2 debris flow deposits which are visible on the north bank of the Sacobia River.



Pasbul Eruptive Period -- ~9,000 yr B.P.

A large explosive eruption occurred ca. 9000 years ago. It produced pyroclastic-flow and tephra-fall layers exposed along the road between Sitio Pasbul, Camias, Porac, and the Gumain River. The pyroclastic flows overtopped the southeastern rim of the Tayawan caldera and nearly or completely filled the valley of the Gumain River.



Crow Valley Eruptive Period -- ~6,000-5,000 yr B.P.

Large eruptions 6,000-5,000 years ago produced pyroclastic flow deposits on both sides of upper Crow valley.



Maraunot Eruptive Period -- ~3,900(?)-2,300 yr B.P.

Eruptions in this period produced pyroclastic flows and lahars.



Buag Eruptive Period -- ca. 1450 AD

The last activity cycle prior to the 1991 eruption was in 1450 ± 50 AD. It produced pyroclastic flows that entered all valley of Pinatubo except the Gumain and Porac rivers.



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Sources of information

The most comprehensive information about Pinatubo volcano is collected in 62 scientific papers in the following volume:

- Newhall et al (1996) "Eruptive history of Mount Pinatubo", in NEWHALL, C.G. and PUNONGBAYAN, R.G. (eds.) (1996) "FIRE AND MUD: ERUPTIONS AND LAHARS OF MOUNT PINATUBO, PHILIPPINES", Philippine Institute of Volcanology and Seismology (PHILVOLCS) / USGS / University of Washington Press (online at pubs.usgs.gov/pinatubo/index.html)

- GVP Pinatubo volcano information

- Mount Pinatubo, Philippines USGS / CVO website about Pinatubo

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Pinatubo Aeta people



The forested area of Pinatubo mountain was also known as home for a tribe of the Aeta people,- the small, dark skinned, and kinky haired people believed to be the nearest descendants of the original inhabitants of the Philippines, who arrived through land bridges that linked the Philippines with the Asian mainland some 30,000 years ago. They considered the mountain the home of Apo Namalyari, the Great Protector and Provider. (Source: CCP Encyclopedia of Arts)

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