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{{ | {{Infobox mountain | ||
| | | name=Mount Pinatubo | ||
| | | other_name = ''Bulkang Pinatubo'' | ||
| | | photo=Pinatubo91eruption clark air base.jpg | ||
| photo_caption=The [[eruption column]] of Mount Pinatubo on June 12, 1991, three days before the climactic eruption. | |||
| elevation_m=1,486 | |||
| elevation_ref={{small|(current)}}<br />1,745 m (5,725 ft) {{small|(before 1991 eruption)}} | |||
| prominence= | |||
| language=Filipino | |||
| pronunciation={{IPAc-en|ˌ|p|iː|n|ə|ˈ|t|uː|b|oʊ}} | |||
| location=Provinces of [[Zambales]], [[Tarlac province|Tarlac]] and [[Pampanga]] on [[Luzon]] island, [[Philippines]] | |||
| range=[[Zambales Mountains]] | |||
| coordinates={{Coord|15|08|30|N|120|21|00|E|type:mountain_region:PH|display=inline,title}} | |||
| topo= | |||
| type=[[Stratovolcano]]<ref>[http://www.volcano.si.edu/world/volcano.cfm?vnum=0703-083 Pinatubo], [[Global Volcanism Program]].</ref> | |||
| age=Between 635,000 ± 80,000<br />and 1.1 ±; 0.09 million years<ref>{{cite web | |||
|url=http://volcano.phivolcs.dost.gov.ph/update_VMEPD/Volcano/VolcanoList/pinatubo.htm | |||
|title=Pinatubo Volcano | |||
|publisher=The [[Philippine Institute of Volcanology and Seismology]] (PHIVOLCS) }}</ref> | |||
| last_eruption=1993 | |||
| first_ascent= | |||
| easiest_route= | |||
}} | }} | ||
'''Mount Pinatubo''' is an [[active volcano|active]] [[stratovolcano]] located on the island of [[Luzon]], near the [[tripoint]] of the [[Philippine province]]s of [[Zambales]], [[Tarlac]], and [[Pampanga]].<ref name="Topo">[http://www.lib.utexas.edu/maps/ams/philippines/txu-oclc-6539351-nd51-1-450.jpg "Tarlac map"]. University of Texas in Austin Library. Retrieved on 2011-08-02.</ref> It is located in the Cabusilan Mountains<ref name="Topo"/><ref>[http://books.google.com/books?id=Hv9GAQAAIAAJ "Report of the Philippine Commission to the President, 1901 Vol. III"], pg. 141. Government Printing Office, Washington, 1901.</ref> separating the west coast of Luzon from the central plains. Before the volcanic activities of 1991, its eruptive history was unknown to most people. It was heavily [[erosion|eroded]], inconspicuous and obscured from view. It was covered with dense [[forest]] which supported a population of several thousand indigenous people, the [[Aeta]]s, who fled to the mountains during the [[Spanish Empire|Spanish]] [[History of the Philippines (1521-1898)|conquest]] of the Philippines. | |||
The volcano's [[Plinian]] / [[Ultra-Plinian]] eruption on June 15, 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of [[Novarupta]] in the [[Alaska Peninsula]].<ref name=Pinatubo1991>{{cite web|title=The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines|url=http://pubs.usgs.gov/fs/1997/fs113-97/|accessdate=2007-04-09}}</ref> Complicating the eruption was the arrival of Typhoon Yunya bringing a lethal mix of ash and rain. Successful predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but the surrounding areas were severely damaged by [[pyroclastic flow]]s, ash deposits, and subsequently, by the [[lahar]]s caused by rainwaters re-mobilizing earlier volcanic deposits destroying thousands of infrastructures and altering the river systems months to years after the eruption.<ref name=Pinatubo1991/><ref>Rodolfo, Umbal, and Alonso. [http://pubs.usgs.gov/pinatubo/rodolfo/index.html "Two Years of Lahars on the Western Flank of Mount Pinatubo: Initiation, Flow Processes, Deposits, and Attendant Geomorphic and Hydraulic Changes"]. USGS Publications. Retrieved on 2012-03-07.</ref> | |||
The effects of the eruption were felt worldwide. It ejected roughly {{convert|10000000000|t|ST|lk=on}} or {{convert|10|km3|cumi|abbr=on}} of magma, and {{convert|20000000|t|ST|abbr=on}} {{chem|S|O|2|link=Sulfur_dioxide}}, bringing vast quantities of minerals and metals to the surface environment. It injected large amounts of [[Particulate|aerosol]] into the [[stratosphere]] – more than any eruption since that of [[Krakatoa]] in 1883. Over the following months, the aerosols formed a global layer of [[sulfuric acid]] haze. Global temperatures dropped by about {{convert|0.5|C-change|F-change|1}}, and [[ozone]] depletion temporarily increased substantially.<ref name="Science News">{{cite web|url=http://www.thefreelibrary.com/Mt.+Pinatubo's+cloud+shades+global+climate.-a012467057|title=Mt. Pinatubo's cloud shades global climate|publisher=Science News|accessdate=2010-03-07}}</ref> | |||
==Overview of the area== | |||
[[File:Tephra fall from 1991 eruption of Mt Pinatubo.gif|thumb|300px|left|Location of Mount Pinatubo, showing area over which ash from the 1991 eruption fell]] | |||
The volcano is located {{convert|87|km|mi|abbr=on}} northwest of [[Manila]], the capital of the Philippines. Near Mount Pinatubo, the United States maintained two large military bases in the region. The [[U.S. Naval Base Subic Bay]] was located {{convert|37|km|mi|abbr=on}} south of Pinatubo, while the extent of [[Clark Air Base]] was just {{convert|14|km|mi|abbr=on}} to the east of the volcano's summit.<ref name=K-118B>Tactical Pilotage Chart, Sheet K-11B, Defense Mapping Agency, Department of Defense, 1982.</ref> Clark Air Base's residential areas and petroleum storage facilities were in much closer proximity to the volcano than the airfield complex and neighboring [[Angeles City]]. | |||
===The Aetas=== | |||
An indigenous group of people, the [[Aetas]] (also spelled as Ayta/Ita), had lived on the slopes of the volcano and in surrounding areas for several centuries, having fled the lowlands to escape persecution by the Spanish during their [[History of the Philippines (1521-1898)|conquest]] of the Philippines which began in 1565. They were a [[hunter-gatherer]] people who were extremely successful in surviving in the dense jungles of the area. These people also grew some staple crops such as [[wheat]], [[barley]], [[rice]] and raised animals. | |||
In total, about 30,000 people lived on the flanks of the volcano in about 25 established [[barangay]]s (villages) and other small settlements like Tarukan village and Maruglu. The dense jungle covering most of the mountain and surrounding peaks supported the hunter-gathering Aeta, while on the surrounding flatter areas, the abundant rainfall of almost {{convert|4|m}} annually) provided by the [[monsoon]] climate and the fertile volcanic soils provided excellent conditions for [[agriculture]]. | |||
==Geological history== | |||
Mount Pinatubo's summit before the 1991 eruption was {{convert|1745|m|ft|abbr=on}} above sea level, only about {{convert|600|m|ft|abbr=on}} above nearby [[plain]]s, and only about {{convert|200|m|ft|abbr=on}} higher than surrounding peaks, which largely obscured it from view. It is part of a chain of [[volcanoes]] which lie along the western side of the edge of the island of [[Luzon]] called the [[Zambales Mountains]]. Pinatubo belongs to the Cabusilan Mountains, the central range of the Zambales Mountains, which consists of Mt. Cuadrado, Mt. Negron, Mt. Mataba and Mt. Pinatubo.<ref>U.S. War Department. [http://books.google.com/books?id=Hv9GAQAAIAAJ&pg=141#v=onepage&q&f=false "Report of the Philippine Commission, 1901 Vol. III"), pg. 141. Government Printing Office, Washington.]</ref> They are [[subduction]] volcanoes, formed by the [[Eurasian Plate]] sliding under the [[Philippine Mobile Belt]] along the [[Manila Trench]] to the west.<ref>{{cite web|url=http://vulcan.wr.usgs.gov/Volcanoes/Philippines/Pinatubo/description_pinatubo.html|title=Description: Mount Pinatubo, Philippines|date=July 13, 2009|author=Topinka, Lyn|accessdate=April 18, 2010|publisher=[[United States Geological Survey]]}}</ref> Mount Pinatubo and the other volcanoes on this [[volcanic belt]] arise due to [[magma]] occlusion from this [[subduction]] [[plate tectonics|plate]] boundary. | |||
Pinatubo is flanked on the west by the Zambales [[Ophiolite]] Complex, which is an easterly-dipping section of [[Eocene]] oceanic crust which was uplifted during the late [[Oligocene]]. The Tarlac Formation consists of marine, nonmarine and volcaniclastic sediments in the north, east and southeast of Pinatubo which were formed in the late [[Miocene]] and [[Pliocene]].<ref name="Newhall"/> | |||
The most recent study of Mount Pinatubo prior to the activities of 1991 was the overall geological study in 1983 and 1984 made by F. G. Delfin for the [[Philippine National Oil Company]] as part of the surface investigations of the area prior to the exploratory drilling and well testing for [[geothermal energy|geothermal]] sources in 1988 to 1990. He recognized two life histories of the mountain, which he classified as 'ancestral' and 'modern' Pinatubo.<ref name="Newhall"/><ref>Delfin, F.G.; Villarosa, H.G.; and Layugan, D.B. [http://pubs.usgs.gov/pinatubo/delfin/index.html "Geothermal Exploration of the pre-1001 Mount Pinatubo Hydrothermal System"]. United States Geological Survey Publications. Retrieved on 2012-03-07.</ref> | |||
===Ancestral Pinatubo=== | |||
[[File:Pre-eruption Pinatubo.jpg|thumb|Pinatubo before the major eruption of 1991.]] | |||
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. Its center was roughly in the same location of the current volcano. The projected height of the mountain is up to {{convert|2300|m|abbr=on}} above [[sea level]] if it was a lone peak, based on profile fitting to the remaining lower slopes, or lower if it had more than one peak.<ref name="Newhall"/> | |||
The old volcano is exposed in the walls of an old {{convert|3.5|x|4.5|km|abbr=on}} wide [[caldera]], referred to as ''Tayawan Caldera'' by Delfin. Some of the nearby peaks are the remnants of ancestral Pinatubo, left behind when the softer parts of the old mountain slopes were eroded by [[weathering]]. Ancestral Pinatubo is a [[somma volcano]] with 'Modern' Pinatubo as the new cone. Its remaining caldera rim includes Mount Donald MacDonald, forming the southeast rim, and Mount Tayawan, the longer north to northeast rim, after which the caldera was named. Mount Dorst, to the east, is part of the dip slope of the ancestral Pinatubo. Several mountains near modern Pinatubo are old satellite vents of ancestral Pinatubo, forming [[volcanic plug]]s and [[lava dome]]s. These satellite vents were probably active around the same time as the ancestral volcano and include the domes of Mount Negron, Mount Cuadrado, Mount Mataba, and the Bituin and Tapungho plugs.<ref name="Newhall"/> | |||
===Modern Pinatubo=== | |||
After a long period of [[dormant volcano|dormancy]], Modern Pinatubo was born in the cataclysmic and the most explosive eruption of Pinatubo around 35,000 years ago. The eruption, which was estimated to be five times larger than the 1991 eruption, deposited [[pyroclastic flow]] material up to {{convert|100|m}} thick on all sides of the mountain. The total volume of pyroclastic flows deposited around the volcano may have been up to {{convert|25|km3|cumi|abbr=on}}, but the total volume of volcanic material ejected during the eruption is unknown. The removal of this amount of material from the underlying [[magma chamber]] led to the formation of the Tayawan [[caldera]]. The eruptive period started by the eruption is referred to by Delfin as the ''Inararo Eruptive Period'', named after a village that was destroyed in the 1991 eruption.<ref name="Newhall"/> | |||
Later eruptions of Modern Pinatubo occurred episodically and lasted for periods much shorter than the repose intervals between them. Subsequent eruptions and eruptive period occurred about ~17,000 (''Sacobia Eruptive Period''); ~9000 (''Pasbul Eruptive Period''); ~6000–5000 (''Crow Valley Eruptive Period''); ~3,900–2,300 (''Maraunot Eruptive Period''); and ~500 years ago (''Buag Eruptive Period''). Each of these eruptions seems to have been very large, ejecting more than 10 km³ of material and covering large parts of the surrounding areas with pyroclastic flow deposits. Some eruptive periods have lasted decades and perhaps as much as several centuries and might appear to include multiple large explosive eruptions.<ref name="Newhall"/> | |||
The maximum size of eruptions in each eruptive period though have been getting smaller through the >35,000-yr history of modern Pinatubo, but this might be an artifact of erosion and (or) burial of older deposits. The oldest eruption of modern Pinatubo, Inararo, was also its largest. Those of the Pasbul period were as energetic, if not as voluminous as the Inararo eruptions. Although smaller than the Inararo eruptions, those of the Crow Valley and Maraunot periods were still about 2 to 3 times as big as that of 1991 based on the pyroclastic flow runout distances and depths of valley filling. Eruptions of the Buag period were roughly the same size as those of 1991. The 1991 eruption was among the smallest documented in its geologic record.<ref name="Newhall"/> | |||
The volcano has never grown very large in between eruptions, because it produces mostly unwelded, easily erodible deposits, and periodically destroys the viscous domes that fill its vents. After the Buag eruption (~500 years ago), the volcano lay dormant, its slopes becoming completely covered in dense [[rainforest]] and eroded into gullies and ravines. The ~500-year repose though between the Buag and present eruptive periods is among the shorter repose periods recognized in its geologic history.<ref name="Newhall">{{cite book|first=Christopher G.|last=Newhall|coauthors=Punongbayan, Raymundo S., eds.|chapter=Eruptive history of Mount Pinatubo|chapter-url=http://pubs.usgs.gov/pinatubo/newhall/index.html |title=FIRE and MUD: Eruptions and Lahars of Mount Pinatubo, Philippines |url=http://vulcan.wr.usgs.gov/Volcanoes/Philippines/Pinatubo/Publications/FireMud/about_the_book.html|publisher=Philippine Institute of Volcanology and Seismology; University of Washington Press|year=1996|isbn=0-295-97585-7 }}</ref> | |||
==The 1991 eruption== | |||
{{refimprove section|date=June 2011}} | |||
===Possible precursor in 1990=== | |||
On July 16, 1990, the major [[1990 Luzon earthquake]] of [[Moment Magnitude|magnitude]] 7.7 struck central Luzon. This was the largest earthquake recorded in 1990,<ref>{{cite web|author=USGS|title=Earthquake Information for 1990|url=http://neic.usgs.gov/neis/eq_depot/1990/|accessdate= 2010-03-06}}</ref><ref name="USGSMagPolicy">[http://earthquake.usgs.gov/aboutus/docs/020204mag_policy.php USGS Earthquake Magnitude Policy]</ref> | |||
comparable in size to the [[1906 San Francisco earthquake]] and the [[2008 Sichuan earthquake]]. Its epicenter was in [[Rizal, Nueva Ecija]] municipality,<ref> | |||
{{cite web|last=|first=|authorlink=|coauthors=|title=The July 16 Luzon Earthquake: A Technical Monograph|work=Inter-Agency Committee for Documenting and Establishing Database on the July 1990 Earthquake|publisher=[[Philippine Institute of Volcanology and Seismology]]|year=2001|url= http://earthquake.phivolcs.dost.gov.ph/update_SOEPD/Earthquake/1990LuzonEQ_Monograph/foreword.html|doi=|accessdate=2009-01-07}}</ref> | |||
about 100 km northeast of Pinatubo, and faulted northwest-southeast through three provinces. It also followed the [[Philippine Fault System]] west as far as [[Baguio City]], which was devastated, and is located about {{convert|80|km}} north-northeast of Pinatubo, leading volcanologists to speculate that it might ultimately have triggered the 1991 eruption, although this is impossible to prove conclusively. Two weeks after the earthquake, local residents reported [[steam]] coming from the volcano, but scientists who visited the mountain in response found only small [[landslide]]s rather than any eruptive activity. | |||
===1991 activities leading to the eruption=== | |||
On March 15, 1991, a succession of earthquakes was felt by villagers on the northwestern side of the volcano. Further [[Harmonic tremor|earthquakes of increasing intensity]] were felt over the next two weeks, and it became clear some kind of volcanic activity was likely. On April 2, the volcano awoke, with [[phreatic eruption]]s occurring near the summit along a {{convert|1.5|km|abbr=on}} long [[Fracture (geology)|fissure]]. Over the next few weeks, small eruptions continued, dusting the surrounding areas with [[volcanic ash]]. [[Seismograph]]s recorded hundreds of small earthquakes every day. | |||
Scientists immediately installed monitoring equipment and analyzed the volcano for clues as to its previous eruptive history. [[Radiocarbon dating]] of charcoal found in old volcanic deposits revealed the last three major explosive eruption periods in recent [[millennia]], about 5500, 3500 and 500 years ago. Geological mapping showed that much of the surrounding plains were formed by [[lahar]] deposits from previous eruptions. | |||
Volcanic activity increased throughout May. Measurements of [[sulfur dioxide]] emissions showed a rapid increase from {{convert|500|t|ST|abbr=on}} per day by May 13 to {{convert|5000|t|ST|abbr=on}} per day by May 28. This implied that there was a rising column of fresh [[magma]] beneath the volcano. After May 28, the amount of {{chem|S|O|2}} being emitted decreased substantially, raising fears that the degassing of the magma had been blocked somehow, leading to a [[pressure]] build-up in the [[magma chamber]] and a high likelihood of explosive eruptions. | |||
The first [[magma]]tic eruptions occurred on June 3, and the first large explosion on June 7 generated an ash column {{convert|7|km|mi|abbr=on}} high. The [[Philippine Institute of Volcanology and Seismology]] (PHIVOLCS) issued a warning indicating the possibility of a major eruption within two weeks. | |||
===Evacuations=== | |||
[[File:Pinatubo evacuation areas.gif|thumb|300px|Map of Pinatubo showing nearby peaks and the evacuation zones]] | |||
Given all the signs that a very large eruption was imminent, [[PHIVOLCS]] – assisted by the [[U.S. Geological Survey]] – worked to convince local inhabitants of the severity of the threat. A false warning might have led to cynicism about any later warnings, but delaying a warning until an eruption began might lead to thousands of deaths, so the [[volcanologists]] were under some pressure to deliver a timely and accurate assessment of the volcanic risk. | |||
Three successive evacuation zones were defined, the innermost containing everything within 10 km of the volcano's summit, the second extending from 10 to 20 km from the summit, and the third extending from {{convert|20|-|40|km|mi|abbr=on}} from the summit ([[Clark Air Base]] and [[Angeles City]] were in this zone). The {{convert|10|km|abbr=on}} and {{convert|10|–|20|km|mi|abbr=on}} zones had a total population of about 40,000, while some 331,000 people lived in the {{convert|20|–|40|km|mi|abbr=on}} zone. Five stages of volcanic alert were defined, from level 1 (low level seismic disturbances) up to level 5 (major eruption in progress). Daily alerts were issued stating the alert level and associated danger area, and the information was announced in major national and local [[newspaper]]s, on [[radio]] and [[television]] stations, by [[nongovernmental organization]]s (NGOs), and directly to the endangered inhabitants. | |||
Many of the [[Aeta]] who lived on the slopes of the volcano left their villages of their own volition when the first explosions began in April, gathering in a village about {{convert|12|km|mi}} from the summit. They moved to increasingly distant villages as the eruptions escalated, some Aeta moving up to nine times in the two months preceding the cataclysmic eruption. | |||
The first formal evacuations were ordered from the {{convert|10|km|mi|abbr=on}} zone on April 7. Evacuation of the {{convert|10|–|20|km|mi|abbr=on}} zone was ordered when a level 4 alert was issued on June 7. A level 5 alert triggered evacuation of the {{convert|20|–|40|km|mi|abbr=on}} zone on June 13, and in all some 60,000 people had left the area within {{convert|30|km|mi}} of the volcano before June 15. Most people temporarily relocated to [[Manila]] and [[Quezon City]], with some 30,000 using the [[Amoranto Velodrome]] in Quezon City as an [[Emergency evacuation|evacuee camp]]. | |||
===Climactic eruption buildup=== | |||
[[File:VulcanoPinatuboJune1991.gif|thumb|The eruption cloud shortly before the climactic eruption]] | |||
In early June, [[tiltmeter]] measurements had shown that the volcano was inflating, evidently due to growing amounts of magma filling the reservoir beneath the summit. At the same time, seismic activity, previously concentrated at a depth of a few kilometers below a point about {{convert|5|km|mi}} northwest of the summit, shifted to shallow depths just below the summit. On June 7, the first magmatic eruptions took place with the formation of a [[lava dome]] at the summit of the volcano. The dome grew substantially over the next five days, reaching a maximum diameter of about {{convert|200|m|ft|abbr=on}} and a height of {{convert|40|m|ft|abbr=on}}. | |||
A small explosion at 03:41 on June 12 marked the beginning of a new, more violent phase of the eruption. A few hours later, large explosions lasting about half an hour generated an [[eruption column]] which quickly reached heights of over {{convert|19|km|mi}}, and which generated [[pyroclastic flow]]s extending up to {{convert|4|km|mi|abbr=on}} from the summit in some river [[valley]]s. Fourteen hours later, a 15-minute eruption hurled ash to heights of {{convert|24|km|mi|abbr=on}}. Friction in the uprushing ash column generated abundant [[lightning]]. | |||
A third large eruption began at 08:41 on June 13, after an intense swarm of small earthquakes over the previous two hours. It lasted about five minutes, and the eruption column once again reached 24 km. After three hours of quiet, seismic activity began, growing more and more intense over the next 24 hours, until a three-minute eruption generated a {{convert|21|km|mi|abbr=on}} high eruption column at 13:09 on June 14. | |||
[[Tephra]] fall from these four large eruptions was extensive to the southwest of the volcano. Two hours after the last of these four explosions, a series of eruptions began which lasted for the next 24 hours, and which saw the production of much larger pyroclastic flows and surges which traveled several kilometres down river valleys on the flanks of the volcano. | |||
[[Dacite]] was the [[igneous rock]] making up the tephra in these eruptions and in the following climactic event. The most abundant [[phenocryst]] minerals were [[hornblende]] and [[plagioclase]], but an unusual phenocryst mineral was also present—the [[calcium sulfate]], [[anhydrite]]. The dacite [[magma]] was more oxidized than most magmas, and the sulfur-rich nature of the eruption was probably causally related to the [[mineral redox buffer|redox state]]. | |||
===The climactic eruption=== | |||
All the seismographs at [[Clark Air Base]] had been rendered inoperative by 14:30 on June 15, mostly by pyroclastic density currents. Intense [[Earth's atmosphere|atmospheric]] pressure variation was also recorded. | |||
[[File:Pinatubo91 lateral blast plume pinatubo 06-15-91-resized.jpg|thumb|left|On June 15, 1991, the eruption plume hours before the climactic eruption.]] | |||
On the same day, [[1991 Pacific typhoon season|Typhoon Yunya (1991)]] struck the island, passing about {{convert|75|km|mi|abbr=on}} north of the volcano. The typhoon rains made direct visual observations of the eruption impossible, but measurements showed that ash was ejected to heights of {{convert|34|km|mi|abbr=on}} by the most violent phase of the eruption, which lasted about three hours. [[Pyroclastic flow]]s poured from the summit, reaching as far as {{convert|16|km|mi|abbr=on}} away from it. [[Typhoon]] rains mixed with the ash deposits caused massive [[lahars]]. | |||
The ash cloud from the volcano covered an area of some {{convert|125000|km2|sqmi|abbr=on}}, bringing total darkness to much of central Luzon. Almost all of the island received some ashfall, which formed a heavy, rain-saturated snow-like blanket. [[Tephra]] fell over most of the [[South China Sea]] and ashfall was recorded as far away as [[Vietnam]], [[Cambodia]] and [[Malaysia]]. | |||
Twelve days after the first magmatic eruptions of June 3, on June 15, 1991, by about 22:30, and about nine hours after the onset of the most recent climactic phase, atmospheric pressure waves had decreased to the pre-eruption levels. No seismic records were available at this time, but volcanologists believe 22:30 marked the end of the climactic eruption. | |||
Vast quantities of minerals and metals were brought to the surface. Overall, introduced to the surface environment, was an estimated {{convert|800000|t|ST|abbr=on}} of [[zinc]], {{convert|600000|t|ST|abbr=on}} of [[copper]], {{convert|550000|t|ST|abbr=on}} of [[chromium]], {{convert|300000|t|ST|abbr=on}} of [[nickel]], and massive amounts of toxic heavy metals such as {{convert|100000|t|ST|abbr=on}} of [[lead]], {{convert|10000|t|ST|abbr=on}} of [[arsenic]], {{convert|1000|t|ST|abbr=on}} of [[cadmium]], and {{convert|800|t|ST|abbr=on}} of [[Mercury (element)|mercury]].<ref>{{cite journal|doi=10.1080/10807030091124383|author=Garret, R.G.|year=2000|title=Natural sources of metals in the environment|journal=Human and Ecological Risk Assessment: an International Journal|volume=6|issue=6|month=November|pages=945–963}}</ref> | |||
===The eruption effects on aircraft=== | |||
At least sixteen commercial aircraft made damaging encounters with the ash cloud ejected by the June 15 eruption, as well as others on the ground. The encounters caused loss of power to one engine on each of two different aircraft. A total of 10 engines were damaged and replaced, including all four engines of a single jumbo jet. Longer term damage to aircraft and engines was reported, including accumulation of sulfate deposits on engines.<ref>[http://newsinfo.inquirer.net/inquirerheadlines/nation/view/20100417-264737/In-1991-it-was-Pinatubo In 1991, it was Pinatubo - INQUIRER.net, Philippine News for Filipinos<!-- Bot generated title -->]</ref> The eruption also forced the [[Philippine Air Force]] to retire their [[Vought F-8 Crusader|Vought F8Us]] from service.{{why|date=September 2012}}{{citation needed|date=September 2012}} | |||
==Aftermath of the 1991 eruption== | |||
[[File:Pinatubo early eruption 1991.jpg|thumb|Summit caldera as seen on Aug. 1, 1991]] | |||
===Explosivity of the eruption=== | |||
The June 15 eruption had a [[Volcanic Explosivity Index]] (VEI) of 6, and came some 450–500 years after the volcano's last known eruptive activity. The eruption ejected about {{convert|10|km3|cumi|abbr=on}} of material, making it the largest eruption since that of [[Novarupta]] in 1912 and some ten times larger than the [[1980 eruption of Mount St. Helens]]. Ejected material such as [[tephra]] fallout and pyroclastic flow deposits are much less dense than magma, and the volume of ejected material was equivalent to about {{convert|4|km3|cumi|abbr=on}} of unerupted material.<ref>{{cite web|url=http://www.ngdc.noaa.gov/seg/hazard/stratoguide/pinfact.html|title=Mt. Pinatubo, Luzon, Philippines|publisher=National Geophysical Data Center (U.S. NOAA)|accessdate=2007-12-02}}</ref> | |||
The former summit of the volcano was obliterated and replaced by a [[caldera]] {{convert|2.5|km|abbr=on}} wide. The highest point on the caldera rim now stood {{convert|1485|m|abbr=on}} above sea level, some {{convert|260|m|abbr=on}} lower than the pre-eruption summit. | |||
===Death toll=== | |||
A reported 847 people were killed by the eruption mostly by roofs collapsing under the weight of accumulated wet ash, a hazard that was amplified by the simultaneous arrival of Typhoon Yunya.<ref>[http://www.coolgeography.co.uk/GCSE/Year11/Managing%20Hazards/Volcanoes/mount_pinatubo.htm CoolGeography - Mount Pinatubo]</ref><ref>{{cite book|chapter-url=http://expo.edu.ph/pinatubo/page5.html|chapter=Ashfall, Pyroclastic Flow, Lahar: The Aftermath|url=http://expo.edu.ph/pinatubo/|title=Pinatubu Volcano: The Sleeping Giant Awakens|publisher=[http://expo.edu.ph expo.edu.ph]}}.</ref> The evacuation in the days preceding the eruption certainly saved tens of thousands of lives, and has been hailed as a great success for [[volcanology]] and eruption prediction. However, damage to [[healthcare]] facilities, and the spread of illnesses in relocation facilities due to poor sanitation, led to rising death tolls in the months following the eruption.{{Citation needed|date=September 2011}} | |||
After the eruption, about 500,000 people continue to live within {{convert|40|km|mi|abbr=on}} of the mountain, with population centers including the 150,000 in [[Angeles City]], and 30,000 at [[Clark Freeport Zone]]. | |||
===Effects on agriculture=== | |||
Many [[reforestation]] projects were destroyed in the eruption, with a total area of {{convert|150|km2|acre|lk=on|abbr=on}} valued at 125 million pesos destroyed. [[Agriculture]] was heavily disrupted, with {{convert|800|km2|acre|abbr=on}} of [[rice]]-growing farmland destroyed, and almost 800,000 head of livestock and [[poultry]] killed, destroying the livelihoods of thousands of farmers. The cost to agriculture of eruption effects was estimated to be 1.5 billion pesos. | |||
Many farmers near Pinatubo began growing crops such as peanuts, cassava and sweet potatoes, which are quick ripening and could be harvested before the threat of lahar flows during the late summer rainy season.<ref name=reilly2009p70 /> | |||
[[File:Pinatubo dust layer.jpg|thumb|Space Shuttle (Mission [[STS-43]]) photograph of the Earth over South America taken on August 8, 1991, showing double layer of Pinatubo aerosol cloud (dark streaks) above high cumulonimbus tops]] | |||
===Local economic and social effects=== | |||
In total, 364 communities and 2.1 million people were affected by the eruption, with livelihoods and houses being damaged or destroyed. More than 8,000 houses were completely destroyed, and a further 73,000 were damaged. In addition to the severe damage sustained by these communities, roads and communications were damaged or destroyed by pyroclastic flows and lahar throughout the areas surrounding the volcanoes. Total losses in 1991 and 1992 alone were estimated at 10.6 and 1.2 billion pesos respectively, including damage to public infrastructure estimated at 3.8 billion pesos (~US$92,000,000). [[Education]] for thousands of children was seriously disrupted by the destruction of [[school]]s in the eruption.<ref>{{cite book|author1=Joan Martí|author2=Gerald Ernst|title=Volcanoes and the environment|url=http://books.google.com/books?id=F0LFIdaao-AC|year=2005|publisher=Cambridge University Press|isbn=978-0-521-59254-3|pages=[http://books.google.com/books?id=F0LFIdaao–AC&pg=PA450 450]}}</ref> | |||
The eruption of Pinatubo severely hampered the [[economic development]] of the surrounding areas. The gross regional domestic product of the Pinatubo area accounted for about 10% of the total Philippine [[gross domestic product]]. The GRDP had been growing at 5% annually before the eruption, but fell by more than 3% from 1990 to 1991. In 1991, damage to crops and property was estimated at $374 million, to which continuing lahar flows added a further $69 million in 1992. 42 percent of the cropland around the volcano was affected by mudflows, dealing a severe blow to the agricultural economy in the region.<ref name=reilly2009p69>{{Harvnb|Reilly|2009|p=69}}.</ref> | |||
===Lahars=== | |||
[[File:River valley filled in by pyroclastic flows, Mt. Pinatubo.jpg|thumb|Before and after the eruption: a river valley filled in by [[pyroclastic flow]] deposits]] | |||
Since the eruption, each onset of heavy rain brought [[lahars]] from the mountain range, causing the displacement of thousands of people. Inflicting extensive damage to buildings and [[infrastructure]] costing billions to repair, a large supply of funds were spent in constructing [[dike (construction)|dikes]] and [[dam]]s to control the post-eruption lahar flows.<ref name=reilly2009p70>{{Harvnb|Reilly|2009|p=70}}.</ref> | |||
Several important river systems stem from Mount Pinatubo, with the major rivers being the Abacan, Tarlac, Pasig-Potrero, Sta. Lucia, Bucao, Santo Tomas, Maloma, Tanguay, Ashley, and Kileng rivers. Before the eruption, these river systems were important [[ecosystem]]s, but the eruption filled many valleys with deep pyroclastic deposits. Since 1991, the rivers have been clogged with [[sediment]], and the valleys have seen frequent [[lahar]]s which continued for years after the eruption. Studies show that the river systems will take years to recover from the 1991 eruption.<ref name=reilly2009p70 /> | |||
===Clark Air Base and Subic Naval Base=== | |||
The [[United States Air Force]] initiated a massive [[airlift]] effort to evacuate American service members and their families during and immediately following the eruption, named [[Operation Fiery Vigil]]. Most personnel were initially relocated to [[Guam]], [[Okinawa]], and [[Hawaii]], although some returned to the continental [[United States]]. Clark Air Base was ultimately abandoned by the United States military, and Subic Bay reverted to Philippine control the next year following the breakdown of lease negotiations. | |||
===Global environmental effects=== | |||
The powerful eruption of such an enormous volume of lava and ash injected significant quantities of [[Particulate|aerosols]] and [[dust]] into the [[stratosphere]]. Sulfur dioxide oxidized in the atmosphere to produce a haze of [[sulfuric acid]] droplets, which gradually spread throughout the stratosphere over the year following the eruption. The injection of aerosols into the stratosphere is thought to have been the largest since the eruption of [[Krakatoa]] in 1883, with a total mass of {{chem|S|O|2}} of about {{convert|17000000|t|ST|abbr=on}} being injected—the largest volume ever recorded by modern instruments (see [[:Image:TOMS SO2 time nov03.png|chart]] and [[:Image:TOMS SO2 Jun17 91.gif|figure]]). | |||
This very large stratospheric injection resulted in a reduction in the normal amount of [[sunlight]] reaching the Earth's surface by roughly 10% (see [[:Image:Mauna Loa atmospheric transmission.png|figure]]). This led to a decrease in [[northern hemisphere]] average temperatures of {{convert|0.5|-|0.6|C-change|F-change|1}} and a global fall of about {{convert|0.4|C-change|F-change|1}}.<ref name="Science News"/><ref>{{cite journal | author = Ward, Peter L. | authorlink = Peter Langdon Ward | date = 2 April 2009 | title = Sulfur Dioxide Initiates Global Climate Change in Four Ways | journal = Thin Solid Films | volume = 517 | issue = 11 | pages = 3188–3203 | doi = 10.1016/j.tsf.2009.01.005 | url= http://www.tetontectonics.org/Climate/SO2InitiatesClimateChange.pdf |accessdate= 2010-03-19|bibcode = 2009TSF...517.3188W }}</ref> At the same time, the temperature in the stratosphere rose to several degrees higher than normal, due to absorption of radiation by the aerosol. The stratospheric cloud from the eruption persisted in the atmosphere for three years after the eruption. | |||
[[File:TOMS AI Jun16 91.gif|thumb|right|Satellite measurements of ash and [[Particulate|aerosol]] emissions from Mount Pinatubo.]] | |||
The eruption had a significant effect on [[ozone]] levels in the atmosphere, causing a large increase in the destruction rate of ozone. Ozone levels at mid-latitudes reached their lowest recorded levels, while in the [[southern hemisphere]] winter of 1992, the [[ozone hole]] over [[Antarctica]] reached its largest ever size until then, with the fastest recorded ozone depletion rates. The eruption of [[Mount Hudson]] in [[Chile]] in August 1991 also contributed to southern hemisphere ozone destruction, with measurements showing a sharp decrease in ozone levels at the [[tropopause]] when the aerosol clouds from Pinatubo and Hudson arrived. | |||
<!-- commenting this out for now, don't trust this source but am looking for papers which might back this up. | |||
Another noticeable effect of the dust in the atmosphere was the appearance of [[lunar eclipse]]s. Normally even at mid-eclipse, the moon is still visible although much dimmed, but in the year following the Pinatubo eruption, the moon was hardly visible at all during eclipses, due to much greater absorption of sunlight by dust in the atmosphere. | |||
It has also been suggested that excess [[cloud condensation nuclei]] from the eruption were responsible for the "[[Great Flood of 1993]]" in the United States<ref>{{Cite web|url=http://k12s.phast.umass.edu/stem/sess/snyder/Adiabatic_Change_and_Cloud.doc|title=Adiabatic Change and Cloud Formation|format=MS Word|publisher=[http://k12s.phast.umass.edu/ umassk12]: [http://k12s.phast.umass.edu/stem/ STEM Education Institute]}}{{copyvio source|date=February 2010}}</ref>--> | |||
===Impact on the indigenous people of Pinatubo=== | |||
The Aeta people were the hardest hit by the eruption. After the areas surrounding the volcano were declared safe, many Aetas returned to their old villages only to find them destroyed by pyroclastic and lahar deposits. Some were able to return to their former way of life, but most moved instead to government-organized resettlement areas. Conditions on these were poor, with each family receiving only small plots of land not ideal for growing crops. Many Aeta found casual labor working for lowland [[farmer]]s, and overall Aeta society became much more fragmented, and reliant on and integrated with lowland culture.<ref>Shimizu, Hiromu (2002), ''[http://web.archive.org/web/20040815181730/http://www.scs.kyushu-u.ac.jp/~hs1/anthro/shimizu_hp/introduction/essay/Ayta_Struggling.htm Struggling for Existence after the Pinatubo Eruption 1991: Catastrophe, Suffering and Rebirth of Ayta Communities]''. Paper presented inter-congress of the International Union of Anthropological and Ethnological Sciences, Tokyo, Japan. Retrieved from [http://www.scs.kyushu-u.ac.jp/~hs1/anthro/shimizu_hp/introduction/essay/Ayta_Struggling.htm the original] on 2004-08-15.</ref> | |||
===Aftermath of the eruptions in pictures=== | |||
<center><gallery> | |||
File:Vertical eruption at Pinatubo, 1991.jpg|Explosive eruption, late June 1991 | |||
File:Ashfall from Pinatubo, 1991.jpg|Snow-like ashfall caused by heavy rain mixing with ash columns | |||
File:Pinatubo - pyroclastic fall.jpg|Erosional dissection of ash deposits on Pinatubo | |||
File:Collapsed hangars at Clark Air Base.jpg|Aircraft hangars at [[Clark Air Base]] destroyed by ashfall | |||
File:Lahars from Pinatubo volcano.jpg|Lahars from Pinatubo volcano fill the broad Santo Tomás River valley SW of the volcano | |||
File:Ash_from_Mount_Pinatubo_covers_NS_Subic_Bay.jpg|Ashes from the then eruption of Pinatubo covers the [[U.S. Naval Base Subic Bay|U.S. Naval Base]] in [[Subic Bay]], [[Zambales]] | |||
</gallery></center> | |||
==Activity since 1991== | |||
[[File:Mount Pinatubo 20081229 01.jpg|thumb|[[Lake Pinatubo]], the resulting crater lake of the 1991 eruption pictured here in 2008]] | |||
[[File:Mount Pinatubo 6.jpg|thumb|Aerial view of Mt. Pinatubo and [[Lake Pinatubo]]]] | |||
Following the climactic eruption of June 15, 1991, activity at the volcano continued at a much lower level, with continuous ash eruptions lasting until August 1991 and episodic eruptions continuing for another month. Activity then remained low until July 1992 when a new [[lava dome]] started growing in the [[caldera]]. Volcanologists suspected that further violent eruptions could be possible, and some areas were evacuated. However, the eruption was only minor and since that episode, the volcano has been quiet. | |||
===Lake Pinatubo=== | |||
The 1991 caldera was subsequently filled with water from monsoon rains and a [[crater lake]], [[Lake Pinatubo]], was formed. In 1992, the growth of a [[lava dome]] formed an [[island]], which was eventually flooded by the lake. Initially, the lake was hot and highly [[acid]]ic, with a minimum [[pH]] of 2 and a temperature of about {{convert|40|C|F}}. Subsequent rainfall cooled and diluted the lake, lowering the temperature to {{convert|26|C|F}} and raising the pH to 5.5 by 2003. | |||
The lake increased in depth by about {{convert|1|m|ft|abbr=on}} per month on average eventually submerging the lava dome, until September 2001, when fears that the walls of the crater might be unstable prompted the Philippine government to order a controlled draining of the lake. An estimated 9,000 people were once again evacuated from surrounding areas in case a large [[flood]] was accidentally triggered. Workers cut a {{convert|5|m|abbr=on}} notch in the crater rim, and successfully drained about a quarter of the lake's volume.<ref>(2001_0907). [http://news.bbc.co.uk/2/hi/asia-pacific/1530182.stm "Filipinos return as volcano lake drains"]. BBC News.</ref> | |||
===Recent activity=== | |||
On the 26th of July 2011, a 5.9 magnitude earthquake struck close to Pinatubo, however no major damages or casualties were reported.<ref>Gonzaga, Robert and Orejas, Tonette (2011-07-26). [http://newsinfo.inquirer.net/30559/5-9-magnitude-quake-jolts-households-in-luzon-metro-areas "5.9-magnitude quake jolts households in Luzon, Metro areas"]. Inquirer News.</ref> | |||
==Cultural history== | |||
The word ''pinatubo'' could mean a fertile place where one can make crops grow or could mean "made to grow" in [[Tagalog language|Tagalog]] and [[Sambal language|Sambal]], which may suggest a knowledge of its previous eruption in about 1500 AD. There is a local oral tradition that is suggestive of a folk memory of earlier large eruptions; ancient legend tells of Bacobaco, the terrible spirit of the sea, who could metamorphose into a huge turtle and who threw fire from his mouth. When being chased by the spirit hunters, Bacobaco fled to the mountain and dug a great hole in its summit showering the surrounding land with rock, mud, dust and fire for three days; howling so loudly that the earth shook.<ref>Rodolfo, K.S. & Umbal, J.V. (2008) "A prehistoric lahar-dammed lake and eruption of Mount Pinatubo described in a Philippine aborigine legend", J. Volcanol. Geotherm. Res., '''176''', 432-437</ref> | |||
===History among Aetas=== | |||
[[Aeta peoples|Aeta]] elders tell many stories about the history of the mountain, the best known being that it was once a Batung Mabye (Kapampangan for living stone). It was said to have been planted on a kingdom by a displeased sorcerer but relocated by a hero. The mountain was soon turned into the abode of Apo Namalyari ("The lord of happenings/ events"), the pagan deity of the Sambal, Aeta, and Kapampangans living on the Zambales range. It was said to comprise the whole mountain range until Sinukuan of [[Mount Arayat]] (the god of the Kapampangans) became a strong rival of Namalyari. Their fight, which took place over the center plains, involved the shattering of the mountain into smaller bodies while Mount Arayat lost its center peak. Other versions have it that Pinatubo's peak shattered because of Namalyari's immense fury in an attempt to teach humans the meaning of fear and show how misdeeds will be punished.{{Citation needed|date=August 2011}} | |||
According to the elders, Apo Namalyari, caused the 1991 eruption because of displeasure toward illegal loggers and [[Philippine National Oil Company]] executives who performed deep exploratory drilling and well testing on the mountain looking for geothermal heat from 1988 to 1990.<ref>{{cite news|url=http://community.seattletimes.nwsource.com/archive/?date=19910721&slug=1295627|title=Natives Who Worship Pinatubo Feel Its Wrath|last=Loeb|first=Vernon|date=1991-07-21|work=[[Seattle Times]]|accessdate=2008-11-22}}</ref> Discouraging results from the wells forced the abandonment of the prospect 13 months before the April 2, 1991 explosions.<ref>Delfin Jr., F.G., Villarosa, H.G.. [http://pubs.usgs.gov/pinatubo/delfin/index.html "Geothermal Exploration of the pre-1991 Mount Pinatubo Hydrothermal System"]. USGS. Retrieved on 2011-08-14.</ref> | |||
==Aetas granted ownership of Pinatubo== | |||
After being driven away by the 1991 eruption of Mount Pinatubo, in May 2009 some 454 Aeta families in Pampanga were given the first clean ancestral land ownership on Mount Pinatubo with the Certificate of Ancestral Domain Title (CADT) by the National Commission on Indigenous Peoples (NCIP), the government agency that deals with issues concerning indigenous people of the Philippines. The approved and declared net land area of {{convert|7,440.1|ha|acre|lk=on|abbr=on}} covers the [[barangay]]s of Mawakat and Nabuklod in [[Floridablanca, Pampanga]], plus a portion of [[San Marcelino, Zambales]], and a portion of Barangay Batiawan in [[Subic, Zambales]].<ref>(2009-05-27). [http://www.scribd.com/doc/35827181/Aetas-in-Pampanga-Awarded-Land-Title "Aetas in Pampanga awarded first clean title of ancestral domain"]. Scribd. Retrieved on 2011-08-14.</ref> | |||
On January 14, 2010, some 7,000 Aeta families from Zambales were officially granted the Certificate of Ancestral Domain Title (CADT) covering the Zambales side of Pinatubo which includes the summit and Lake Pinatubo, officially becoming their '''''lutan tua''''' (ancestral land). The ancestral domain title covers {{convert|15984|ha|acre|abbr=on}} and includes the villages of Burgos, Villar, Moraza and Belbel in Botolan and portions of the towns of [[Cabangan, Zambales|Cabangan]], [[San Felipe, Zambales|San Felipe]] and [[San Marcelino, Zambales|San Marcelino]].<ref>Orejas, Tonette (2009-11-27). [http://www.piplinks.org/it%E2%80%99s-official%3A-pinatubo-now-owned-aetas "It’s official: Pinatubo is now owned by Aetas"]. Piplinks (originally from Philippine Daily Inquirer). Retrieved on 2011-08-14.</ref><ref name="Preda"/> | |||
Having the land title will protect them from others — including foreigners — from exploiting their land without compensation to the indigenous tribes. In the past, the Aetas had to contend with mining companies, loggers, and, recently, tourist companies who earn from Mount Pinatubo but do not compensate the local tribes.<ref name="Preda">Valdez, Katrina Mennen A. (2010-01-14). [http://www.preda.org/main/archives/2010/r10011401.html "Aetas to receive title to domain at Mt. Pinatubo"]. Preda Foundation. Retrieved on 2011-08-14.</ref> | |||
Ancestral domain titles are awarded to a certain community or indigenous group who have occupied or possessed the land continuously in accordance with their customs and traditions since time immemorial. They have the legal right to collectively possess and to enjoy the land and its natural resources to the exclusion of others.<ref name="Preda"/> | |||
==Pinatubo in popular culture== | |||
Long before Mt. Pinatubo became famous for its cataclysmic eruption, [[President of the Philippines|Philippine President]] [[Ramon Magsaysay]], a native of Zambales, named his [[C-47 Skytrain|C-47]] presidential plane "Mt. Pinatubo". The [[1957 Cebu Douglas C-47 crash|plane crashed in 1957]], killing the President and 24 others on board.<ref>{{cite news|author=Dominico C. Moneva|title=Speak out: Magsaysay’s death|url=http://www.sunstar.com.ph/static/ceb/2006/03/18/oped/dominico.c..moneva..html|publisher=Sun Star Cebu|date=2006-03-18|accessdate=2008-03-21}}</ref> | |||
==Hiking Pinatubo== | |||
The caldera formed and [[Lake Pinatubo]] has since become a tourist attraction with the preferred route through Barangay Santa Juliana in [[Capas, Tarlac]].<ref>{{cite news|title=Trekking-Mt-Pinatubo: Inquirer.net article|url=http://lifestyle.inquirer.net/2bu/2bu/view/20100529-272636/Trekking-Mt-Pinatubo|accessdate=13 June 2012|date=2010-05-29}}</ref> | |||
==See also== | |||
* [[Active volcanoes in the Philippines]] | |||
* [[Inactive volcanoes in the Philippines]] | |||
* [[Potentially active volcanos in the Philippines]] | |||
* [[List of volcanic eruptions by death toll]] | |||
* [[Timetable of major worldwide volcanic eruptions]] | |||
==Notes== | |||
{{reflist|2}} | |||
==References== | |||
{{refbegin|2}} | |||
* Decker, R. and Decker, B. (1997) ''Volcanoes'', 3rd edition, WH Freeman, New York. | |||
* {{cite journal|author=McCormick, M. Patrick et al.|year=1995|title=Atmospheric effects of the Mt Pinatubo eruption|journal=[[Nature (journal)|Nature]]|volume=373|issue=6513|pages=399–404|doi=10.1038/373399a0|bibcode = 1995Natur.373..399M }} | |||
* {{cite book|title=Geological Disasters In The Philippines: The July 1990 Earthquake And The June 1991 Eruption of Mount Pinatubo. Description, effects and lessons learned|last=Rantucci|first=Giovanni|authorlink=|coauthors=|year=1994|publisher=Philippine Institute of Volcanology and Seismology (PHIVOLCS)|location=|isbn=978-0-7881-2075-6|page=|pages=|url=http://books.google.com/?id=qK3uy9oMzccC|accessdate=2009-08-15}} | |||
* {{cite book|last=Reilly|first=Benjamin |title=Disaster and human history: case studies in nature, society and catastrophe|url=http://books.google.com/books?id=mI77lmwmVDkC|year=2009|publisher=McFarland|isbn=978-0-7864-3655-2|ref=harv}} | |||
* {{Cite document | |||
|last= Self |first= S. |coauthors= Zhao, Jing-Xia, Holasek, R.E., Torres, R.C., and King, A.J. |date= 1998 |contribution= The atmospheric impact of the 1991 Mount Pinatubo eruption |title= Fire and Mud, Eruptions and Lahars of Mount Pinatubo, Philippines |editors= Newhall, C.G., Punongbayan, R.S. |publisher= Smithsonian Institution - Global Volcanism Program |place= Washington |issue= |pages= 1126 |url= http://pubs.usgs.gov/pinatubo/self/index.html |accessdate= 2010-04-21 |doi = | |||
|postscript= <!--None--> }} | |||
* Scaillet, B. and Evans, B. W. (1999) ''The June 15, 1991 Eruption of Mount Pinatubo. I. Phase Equilibria and Pre-eruption P–T–fO2–fH2O Conditions of the Dacite Magma.'' Journal of Petrology, v. 40, 381–411. | |||
* Stimac J.A., Goff F., Counce D., Larocque A.C.L., Hilton D.R. (2003), ''The crater lake and hydrothermal system of Mount Pinatubo, Philippines: evolution in the decade after eruption'', Bulletin of Volcanology, v. 66, p. 149–167 | |||
* Wiesner, M.G., Wetzel, A. Catane, S.G., Listanco, E.L. and Mirabueno, H.T. (2004) Grain size, areal thickness distribution and controls on sedimentation of the 1991 Mount Pinatubo tephra layer in the South China Sea. Bulletin of Volcanology, v. 66, 226–242. | |||
* Dhot, S. Mt Pinatubo Safety. | |||
{{refend}} | |||
==External links== | |||
{{Commons category}} | |||
{{Spoken Wikipedia|Mount_Pinatubo.ogg|2006-01-31}} | |||
* [http://pubs.usgs.gov/pinatubo/contents.html ''Fire and Mud. Eruptions and Lahars of Mount Pinatubo''], [[United States Geological Survey]] site | |||
* [http://volcano.phivolcs.dost.gov.ph/update_VMEPD/Volcano/VolcanoList/pinatubo.htm ''Mount Pinatubo page'']. Philippine Institute of Volcanology and Seismology | |||
* [http://eos.higp.hawaii.edu/education/slide_set1/ ''Weather effects of the 1991 eruption''] EOS Volcanology. | |||
* [http://vulcan.wr.usgs.gov/Volcanoes/Philippines/Pinatubo/images.html ''CVO Pinatubo photo archive''] Cascades Volcano Observatory | |||
* [http://pubs.usgs.gov/fs/1997/fs113-97/fs113-97.pdf ''The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines'']. United States Geological Survey site | |||
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[[Category:Crater lakes]] | |||
[[Category:Mountains of the Philippines]] | |||
[[Category:Natural disasters in the Philippines]] | |||
[[Category:Stratovolcanoes]] | |||
[[Category:Subduction volcanoes]] | |||
[[Category:VEI-6 volcanoes]] | |||
[[Category:Volcanic calderas]] | |||
[[Category:Volcanic events]] | |||
[[Category:Volcanoes of Luzon]] | |||
[[Category:Zambales]] | |||
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Revision as of 21:28, 7 December 2012
Template loop detected: Template:Infobox mountain
Mount Pinatubo is an active stratovolcano located on the island of Luzon, near the tripoint of the Philippine provinces of Zambales, Tarlac, and Pampanga.[1] It is located in the Cabusilan Mountains[1][2] separating the west coast of Luzon from the central plains. Before the volcanic activities of 1991, its eruptive history was unknown to most people. It was heavily eroded, inconspicuous and obscured from view. It was covered with dense forest which supported a population of several thousand indigenous people, the Aetas, who fled to the mountains during the Spanish conquest of the Philippines.
The volcano's Plinian / Ultra-Plinian eruption on June 15, 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in the Alaska Peninsula.[3] Complicating the eruption was the arrival of Typhoon Yunya bringing a lethal mix of ash and rain. Successful predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but the surrounding areas were severely damaged by pyroclastic flows, ash deposits, and subsequently, by the lahars caused by rainwaters re-mobilizing earlier volcanic deposits destroying thousands of infrastructures and altering the river systems months to years after the eruption.[3][4]
The effects of the eruption were felt worldwide. It ejected roughly Template:Convert/t or Template:Convert/km3Template:Convert/test/Aon of magma, and Template:Convert/tTemplate:Convert/test/Aon Template:Chem, bringing vast quantities of minerals and metals to the surface environment. It injected large amounts of aerosol into the stratosphere – more than any eruption since that of Krakatoa in 1883. Over the following months, the aerosols formed a global layer of sulfuric acid haze. Global temperatures dropped by about Template:Convert/C-change, and ozone depletion temporarily increased substantially.[5]
Overview of the area
The volcano is located Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon northwest of Manila, the capital of the Philippines. Near Mount Pinatubo, the United States maintained two large military bases in the region. The U.S. Naval Base Subic Bay was located Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon south of Pinatubo, while the extent of Clark Air Base was just Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon to the east of the volcano's summit.[6] Clark Air Base's residential areas and petroleum storage facilities were in much closer proximity to the volcano than the airfield complex and neighboring Angeles City.
The Aetas
An indigenous group of people, the Aetas (also spelled as Ayta/Ita), had lived on the slopes of the volcano and in surrounding areas for several centuries, having fled the lowlands to escape persecution by the Spanish during their conquest of the Philippines which began in 1565. They were a hunter-gatherer people who were extremely successful in surviving in the dense jungles of the area. These people also grew some staple crops such as wheat, barley, rice and raised animals.
In total, about 30,000 people lived on the flanks of the volcano in about 25 established barangays (villages) and other small settlements like Tarukan village and Maruglu. The dense jungle covering most of the mountain and surrounding peaks supported the hunter-gathering Aeta, while on the surrounding flatter areas, the abundant rainfall of almost 4 metres (13 ft) annually) provided by the monsoon climate and the fertile volcanic soils provided excellent conditions for agriculture.
Geological history
Mount Pinatubo's summit before the 1991 eruption was Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above sea level, only about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above nearby plains, and only about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon higher than surrounding peaks, which largely obscured it from view. It is part of a chain of volcanoes which lie along the western side of the edge of the island of Luzon called the Zambales Mountains. Pinatubo belongs to the Cabusilan Mountains, the central range of the Zambales Mountains, which consists of Mt. Cuadrado, Mt. Negron, Mt. Mataba and Mt. Pinatubo.[7] They are subduction volcanoes, formed by the Eurasian Plate sliding under the Philippine Mobile Belt along the Manila Trench to the west.[8] Mount Pinatubo and the other volcanoes on this volcanic belt arise due to magma occlusion from this subduction plate boundary.
Pinatubo is flanked on the west by the Zambales Ophiolite Complex, which is an easterly-dipping section of Eocene oceanic crust which was uplifted during the late Oligocene. The Tarlac Formation consists of marine, nonmarine and volcaniclastic sediments in the north, east and southeast of Pinatubo which were formed in the late Miocene and Pliocene.[9]
The most recent study of Mount Pinatubo prior to the activities of 1991 was the overall geological study in 1983 and 1984 made by F. G. Delfin for the Philippine National Oil Company as part of the surface investigations of the area prior to the exploratory drilling and well testing for geothermal sources in 1988 to 1990. He recognized two life histories of the mountain, which he classified as 'ancestral' and 'modern' Pinatubo.[9][10]
Ancestral Pinatubo
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. Its center was roughly in the same location of the current volcano. The projected height of the mountain is up to Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above sea level if it was a lone peak, based on profile fitting to the remaining lower slopes, or lower if it had more than one peak.[9]
The old volcano is exposed in the walls of an old Template:Convert/xTemplate:Convert/test/Aon wide caldera, referred to as Tayawan Caldera by Delfin. Some of the nearby peaks are the remnants of ancestral Pinatubo, left behind when the softer parts of the old mountain slopes were eroded by weathering. Ancestral Pinatubo is a somma volcano with 'Modern' Pinatubo as the new cone. Its remaining caldera rim includes Mount Donald MacDonald, forming the southeast rim, and Mount Tayawan, the longer north to northeast rim, after which the caldera was named. Mount Dorst, to the east, is part of the dip slope of the ancestral Pinatubo. Several mountains near modern Pinatubo are old satellite vents of ancestral Pinatubo, forming volcanic plugs and lava domes. These satellite vents were probably active around the same time as the ancestral volcano and include the domes of Mount Negron, Mount Cuadrado, Mount Mataba, and the Bituin and Tapungho plugs.[9]
Modern Pinatubo
After a long period of dormancy, Modern Pinatubo was born in the cataclysmic and the most explosive eruption of Pinatubo around 35,000 years ago. The eruption, which was estimated to be five times larger than the 1991 eruption, deposited pyroclastic flow material up to 100 metres (330 ft) thick on all sides of the mountain. The total volume of pyroclastic flows deposited around the volcano may have been up to Template:Convert/km3Template:Convert/test/Aon, but the total volume of volcanic material ejected during the eruption is unknown. The removal of this amount of material from the underlying magma chamber led to the formation of the Tayawan caldera. The eruptive period started by the eruption is referred to by Delfin as the Inararo Eruptive Period, named after a village that was destroyed in the 1991 eruption.[9]
Later eruptions of Modern Pinatubo occurred episodically and lasted for periods much shorter than the repose intervals between them. Subsequent eruptions and eruptive period occurred about ~17,000 (Sacobia Eruptive Period); ~9000 (Pasbul Eruptive Period); ~6000–5000 (Crow Valley Eruptive Period); ~3,900–2,300 (Maraunot Eruptive Period); and ~500 years ago (Buag Eruptive Period). Each of these eruptions seems to have been very large, ejecting more than 10 km³ of material and covering large parts of the surrounding areas with pyroclastic flow deposits. Some eruptive periods have lasted decades and perhaps as much as several centuries and might appear to include multiple large explosive eruptions.[9]
The maximum size of eruptions in each eruptive period though have been getting smaller through the >35,000-yr history of modern Pinatubo, but this might be an artifact of erosion and (or) burial of older deposits. The oldest eruption of modern Pinatubo, Inararo, was also its largest. Those of the Pasbul period were as energetic, if not as voluminous as the Inararo eruptions. Although smaller than the Inararo eruptions, those of the Crow Valley and Maraunot periods were still about 2 to 3 times as big as that of 1991 based on the pyroclastic flow runout distances and depths of valley filling. Eruptions of the Buag period were roughly the same size as those of 1991. The 1991 eruption was among the smallest documented in its geologic record.[9]
The volcano has never grown very large in between eruptions, because it produces mostly unwelded, easily erodible deposits, and periodically destroys the viscous domes that fill its vents. After the Buag eruption (~500 years ago), the volcano lay dormant, its slopes becoming completely covered in dense rainforest and eroded into gullies and ravines. The ~500-year repose though between the Buag and present eruptive periods is among the shorter repose periods recognized in its geologic history.[9]
The 1991 eruption
Possible precursor in 1990
On July 16, 1990, the major 1990 Luzon earthquake of magnitude 7.7 struck central Luzon. This was the largest earthquake recorded in 1990,[11][12] comparable in size to the 1906 San Francisco earthquake and the 2008 Sichuan earthquake. Its epicenter was in Rizal, Nueva Ecija municipality,[13] about 100 km northeast of Pinatubo, and faulted northwest-southeast through three provinces. It also followed the Philippine Fault System west as far as Baguio City, which was devastated, and is located about 80 kilometres (50 mi) north-northeast of Pinatubo, leading volcanologists to speculate that it might ultimately have triggered the 1991 eruption, although this is impossible to prove conclusively. Two weeks after the earthquake, local residents reported steam coming from the volcano, but scientists who visited the mountain in response found only small landslides rather than any eruptive activity.
1991 activities leading to the eruption
On March 15, 1991, a succession of earthquakes was felt by villagers on the northwestern side of the volcano. Further earthquakes of increasing intensity were felt over the next two weeks, and it became clear some kind of volcanic activity was likely. On April 2, the volcano awoke, with phreatic eruptions occurring near the summit along a Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon long fissure. Over the next few weeks, small eruptions continued, dusting the surrounding areas with volcanic ash. Seismographs recorded hundreds of small earthquakes every day.
Scientists immediately installed monitoring equipment and analyzed the volcano for clues as to its previous eruptive history. Radiocarbon dating of charcoal found in old volcanic deposits revealed the last three major explosive eruption periods in recent millennia, about 5500, 3500 and 500 years ago. Geological mapping showed that much of the surrounding plains were formed by lahar deposits from previous eruptions.
Volcanic activity increased throughout May. Measurements of sulfur dioxide emissions showed a rapid increase from Template:Convert/tTemplate:Convert/test/Aon per day by May 13 to Template:Convert/tTemplate:Convert/test/Aon per day by May 28. This implied that there was a rising column of fresh magma beneath the volcano. After May 28, the amount of Template:Chem being emitted decreased substantially, raising fears that the degassing of the magma had been blocked somehow, leading to a pressure build-up in the magma chamber and a high likelihood of explosive eruptions.
The first magmatic eruptions occurred on June 3, and the first large explosion on June 7 generated an ash column Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon high. The Philippine Institute of Volcanology and Seismology (PHIVOLCS) issued a warning indicating the possibility of a major eruption within two weeks.
Evacuations
Given all the signs that a very large eruption was imminent, PHIVOLCS – assisted by the U.S. Geological Survey – worked to convince local inhabitants of the severity of the threat. A false warning might have led to cynicism about any later warnings, but delaying a warning until an eruption began might lead to thousands of deaths, so the volcanologists were under some pressure to deliver a timely and accurate assessment of the volcanic risk.
Three successive evacuation zones were defined, the innermost containing everything within 10 km of the volcano's summit, the second extending from 10 to 20 km from the summit, and the third extending from Template:Convert/-Template:Convert/test/Aon from the summit (Clark Air Base and Angeles City were in this zone). The Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon and Template:Convert/–Template:Convert/test/Aon zones had a total population of about 40,000, while some 331,000 people lived in the Template:Convert/–Template:Convert/test/Aon zone. Five stages of volcanic alert were defined, from level 1 (low level seismic disturbances) up to level 5 (major eruption in progress). Daily alerts were issued stating the alert level and associated danger area, and the information was announced in major national and local newspapers, on radio and television stations, by nongovernmental organizations (NGOs), and directly to the endangered inhabitants.
Many of the Aeta who lived on the slopes of the volcano left their villages of their own volition when the first explosions began in April, gathering in a village about 12 kilometres (Template:Rnd/- mi) from the summit. They moved to increasingly distant villages as the eruptions escalated, some Aeta moving up to nine times in the two months preceding the cataclysmic eruption.
The first formal evacuations were ordered from the Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon zone on April 7. Evacuation of the Template:Convert/–Template:Convert/test/Aon zone was ordered when a level 4 alert was issued on June 7. A level 5 alert triggered evacuation of the Template:Convert/–Template:Convert/test/Aon zone on June 13, and in all some 60,000 people had left the area within 30 kilometres (19 mi) of the volcano before June 15. Most people temporarily relocated to Manila and Quezon City, with some 30,000 using the Amoranto Velodrome in Quezon City as an evacuee camp.
Climactic eruption buildup
In early June, tiltmeter measurements had shown that the volcano was inflating, evidently due to growing amounts of magma filling the reservoir beneath the summit. At the same time, seismic activity, previously concentrated at a depth of a few kilometers below a point about 5 kilometres (Template:Rnd/- mi) northwest of the summit, shifted to shallow depths just below the summit. On June 7, the first magmatic eruptions took place with the formation of a lava dome at the summit of the volcano. The dome grew substantially over the next five days, reaching a maximum diameter of about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon and a height of Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon.
A small explosion at 03:41 on June 12 marked the beginning of a new, more violent phase of the eruption. A few hours later, large explosions lasting about half an hour generated an eruption column which quickly reached heights of over 19 kilometres (12 mi), and which generated pyroclastic flows extending up to Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon from the summit in some river valleys. Fourteen hours later, a 15-minute eruption hurled ash to heights of Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon. Friction in the uprushing ash column generated abundant lightning.
A third large eruption began at 08:41 on June 13, after an intense swarm of small earthquakes over the previous two hours. It lasted about five minutes, and the eruption column once again reached 24 km. After three hours of quiet, seismic activity began, growing more and more intense over the next 24 hours, until a three-minute eruption generated a Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon high eruption column at 13:09 on June 14.
Tephra fall from these four large eruptions was extensive to the southwest of the volcano. Two hours after the last of these four explosions, a series of eruptions began which lasted for the next 24 hours, and which saw the production of much larger pyroclastic flows and surges which traveled several kilometres down river valleys on the flanks of the volcano.
Dacite was the igneous rock making up the tephra in these eruptions and in the following climactic event. The most abundant phenocryst minerals were hornblende and plagioclase, but an unusual phenocryst mineral was also present—the calcium sulfate, anhydrite. The dacite magma was more oxidized than most magmas, and the sulfur-rich nature of the eruption was probably causally related to the redox state.
The climactic eruption
All the seismographs at Clark Air Base had been rendered inoperative by 14:30 on June 15, mostly by pyroclastic density currents. Intense atmospheric pressure variation was also recorded.
On the same day, Typhoon Yunya (1991) struck the island, passing about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon north of the volcano. The typhoon rains made direct visual observations of the eruption impossible, but measurements showed that ash was ejected to heights of Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon by the most violent phase of the eruption, which lasted about three hours. Pyroclastic flows poured from the summit, reaching as far as Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon away from it. Typhoon rains mixed with the ash deposits caused massive lahars.
The ash cloud from the volcano covered an area of some Template:Convert/km2Template:Convert/test/Aon, bringing total darkness to much of central Luzon. Almost all of the island received some ashfall, which formed a heavy, rain-saturated snow-like blanket. Tephra fell over most of the South China Sea and ashfall was recorded as far away as Vietnam, Cambodia and Malaysia.
Twelve days after the first magmatic eruptions of June 3, on June 15, 1991, by about 22:30, and about nine hours after the onset of the most recent climactic phase, atmospheric pressure waves had decreased to the pre-eruption levels. No seismic records were available at this time, but volcanologists believe 22:30 marked the end of the climactic eruption.
Vast quantities of minerals and metals were brought to the surface. Overall, introduced to the surface environment, was an estimated Template:Convert/tTemplate:Convert/test/Aon of zinc, Template:Convert/tTemplate:Convert/test/Aon of copper, Template:Convert/tTemplate:Convert/test/Aon of chromium, Template:Convert/tTemplate:Convert/test/Aon of nickel, and massive amounts of toxic heavy metals such as Template:Convert/tTemplate:Convert/test/Aon of lead, Template:Convert/tTemplate:Convert/test/Aon of arsenic, Template:Convert/tTemplate:Convert/test/Aon of cadmium, and Template:Convert/tTemplate:Convert/test/Aon of mercury.[14]
The eruption effects on aircraft
At least sixteen commercial aircraft made damaging encounters with the ash cloud ejected by the June 15 eruption, as well as others on the ground. The encounters caused loss of power to one engine on each of two different aircraft. A total of 10 engines were damaged and replaced, including all four engines of a single jumbo jet. Longer term damage to aircraft and engines was reported, including accumulation of sulfate deposits on engines.[15] The eruption also forced the Philippine Air Force to retire their Vought F8Us from service.Template:WhyTemplate:Citation needed
Aftermath of the 1991 eruption
Explosivity of the eruption
The June 15 eruption had a Volcanic Explosivity Index (VEI) of 6, and came some 450–500 years after the volcano's last known eruptive activity. The eruption ejected about Template:Convert/km3Template:Convert/test/Aon of material, making it the largest eruption since that of Novarupta in 1912 and some ten times larger than the 1980 eruption of Mount St. Helens. Ejected material such as tephra fallout and pyroclastic flow deposits are much less dense than magma, and the volume of ejected material was equivalent to about Template:Convert/km3Template:Convert/test/Aon of unerupted material.[16] The former summit of the volcano was obliterated and replaced by a caldera Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon wide. The highest point on the caldera rim now stood Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above sea level, some Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon lower than the pre-eruption summit.
Death toll
A reported 847 people were killed by the eruption mostly by roofs collapsing under the weight of accumulated wet ash, a hazard that was amplified by the simultaneous arrival of Typhoon Yunya.[17][18] The evacuation in the days preceding the eruption certainly saved tens of thousands of lives, and has been hailed as a great success for volcanology and eruption prediction. However, damage to healthcare facilities, and the spread of illnesses in relocation facilities due to poor sanitation, led to rising death tolls in the months following the eruption.Template:Citation needed
After the eruption, about 500,000 people continue to live within Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon of the mountain, with population centers including the 150,000 in Angeles City, and 30,000 at Clark Freeport Zone.
Effects on agriculture
Many reforestation projects were destroyed in the eruption, with a total area of Template:Convert/km2Template:Convert/test/Aon valued at 125 million pesos destroyed. Agriculture was heavily disrupted, with Template:Convert/km2Template:Convert/test/Aon of rice-growing farmland destroyed, and almost 800,000 head of livestock and poultry killed, destroying the livelihoods of thousands of farmers. The cost to agriculture of eruption effects was estimated to be 1.5 billion pesos.
Many farmers near Pinatubo began growing crops such as peanuts, cassava and sweet potatoes, which are quick ripening and could be harvested before the threat of lahar flows during the late summer rainy season.[19]
Local economic and social effects
In total, 364 communities and 2.1 million people were affected by the eruption, with livelihoods and houses being damaged or destroyed. More than 8,000 houses were completely destroyed, and a further 73,000 were damaged. In addition to the severe damage sustained by these communities, roads and communications were damaged or destroyed by pyroclastic flows and lahar throughout the areas surrounding the volcanoes. Total losses in 1991 and 1992 alone were estimated at 10.6 and 1.2 billion pesos respectively, including damage to public infrastructure estimated at 3.8 billion pesos (~US$92,000,000). Education for thousands of children was seriously disrupted by the destruction of schools in the eruption.[20]
The eruption of Pinatubo severely hampered the economic development of the surrounding areas. The gross regional domestic product of the Pinatubo area accounted for about 10% of the total Philippine gross domestic product. The GRDP had been growing at 5% annually before the eruption, but fell by more than 3% from 1990 to 1991. In 1991, damage to crops and property was estimated at $374 million, to which continuing lahar flows added a further $69 million in 1992. 42 percent of the cropland around the volcano was affected by mudflows, dealing a severe blow to the agricultural economy in the region.[21]
Lahars
Since the eruption, each onset of heavy rain brought lahars from the mountain range, causing the displacement of thousands of people. Inflicting extensive damage to buildings and infrastructure costing billions to repair, a large supply of funds were spent in constructing dikes and dams to control the post-eruption lahar flows.[19]
Several important river systems stem from Mount Pinatubo, with the major rivers being the Abacan, Tarlac, Pasig-Potrero, Sta. Lucia, Bucao, Santo Tomas, Maloma, Tanguay, Ashley, and Kileng rivers. Before the eruption, these river systems were important ecosystems, but the eruption filled many valleys with deep pyroclastic deposits. Since 1991, the rivers have been clogged with sediment, and the valleys have seen frequent lahars which continued for years after the eruption. Studies show that the river systems will take years to recover from the 1991 eruption.[19]
The United States Air Force initiated a massive airlift effort to evacuate American service members and their families during and immediately following the eruption, named Operation Fiery Vigil. Most personnel were initially relocated to Guam, Okinawa, and Hawaii, although some returned to the continental United States. Clark Air Base was ultimately abandoned by the United States military, and Subic Bay reverted to Philippine control the next year following the breakdown of lease negotiations.
Global environmental effects
The powerful eruption of such an enormous volume of lava and ash injected significant quantities of aerosols and dust into the stratosphere. Sulfur dioxide oxidized in the atmosphere to produce a haze of sulfuric acid droplets, which gradually spread throughout the stratosphere over the year following the eruption. The injection of aerosols into the stratosphere is thought to have been the largest since the eruption of Krakatoa in 1883, with a total mass of Template:Chem of about Template:Convert/tTemplate:Convert/test/Aon being injected—the largest volume ever recorded by modern instruments (see chart and figure).
This very large stratospheric injection resulted in a reduction in the normal amount of sunlight reaching the Earth's surface by roughly 10% (see figure). This led to a decrease in northern hemisphere average temperatures of Template:Convert/- and a global fall of about Template:Convert/C-change.[5][22] At the same time, the temperature in the stratosphere rose to several degrees higher than normal, due to absorption of radiation by the aerosol. The stratospheric cloud from the eruption persisted in the atmosphere for three years after the eruption.
The eruption had a significant effect on ozone levels in the atmosphere, causing a large increase in the destruction rate of ozone. Ozone levels at mid-latitudes reached their lowest recorded levels, while in the southern hemisphere winter of 1992, the ozone hole over Antarctica reached its largest ever size until then, with the fastest recorded ozone depletion rates. The eruption of Mount Hudson in Chile in August 1991 also contributed to southern hemisphere ozone destruction, with measurements showing a sharp decrease in ozone levels at the tropopause when the aerosol clouds from Pinatubo and Hudson arrived.
Impact on the indigenous people of Pinatubo
The Aeta people were the hardest hit by the eruption. After the areas surrounding the volcano were declared safe, many Aetas returned to their old villages only to find them destroyed by pyroclastic and lahar deposits. Some were able to return to their former way of life, but most moved instead to government-organized resettlement areas. Conditions on these were poor, with each family receiving only small plots of land not ideal for growing crops. Many Aeta found casual labor working for lowland farmers, and overall Aeta society became much more fragmented, and reliant on and integrated with lowland culture.[23]
Aftermath of the eruptions in pictures
- Vertical eruption at Pinatubo, 1991.jpg
Explosive eruption, late June 1991
- Ashfall from Pinatubo, 1991.jpg
Snow-like ashfall caused by heavy rain mixing with ash columns
- Pinatubo - pyroclastic fall.jpg
Erosional dissection of ash deposits on Pinatubo
- Collapsed hangars at Clark Air Base.jpg
Aircraft hangars at Clark Air Base destroyed by ashfall
- Lahars from Pinatubo volcano.jpg
Lahars from Pinatubo volcano fill the broad Santo Tomás River valley SW of the volcano
- Ash from Mount Pinatubo covers NS Subic Bay.jpg
Ashes from the then eruption of Pinatubo covers the U.S. Naval Base in Subic Bay, Zambales
Activity since 1991
Following the climactic eruption of June 15, 1991, activity at the volcano continued at a much lower level, with continuous ash eruptions lasting until August 1991 and episodic eruptions continuing for another month. Activity then remained low until July 1992 when a new lava dome started growing in the caldera. Volcanologists suspected that further violent eruptions could be possible, and some areas were evacuated. However, the eruption was only minor and since that episode, the volcano has been quiet.
Lake Pinatubo
The 1991 caldera was subsequently filled with water from monsoon rains and a crater lake, Lake Pinatubo, was formed. In 1992, the growth of a lava dome formed an island, which was eventually flooded by the lake. Initially, the lake was hot and highly acidic, with a minimum pH of 2 and a temperature of about Template:Convert/C. Subsequent rainfall cooled and diluted the lake, lowering the temperature to Template:Convert/C and raising the pH to 5.5 by 2003.
The lake increased in depth by about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon per month on average eventually submerging the lava dome, until September 2001, when fears that the walls of the crater might be unstable prompted the Philippine government to order a controlled draining of the lake. An estimated 9,000 people were once again evacuated from surrounding areas in case a large flood was accidentally triggered. Workers cut a Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon notch in the crater rim, and successfully drained about a quarter of the lake's volume.[24]
Recent activity
On the 26th of July 2011, a 5.9 magnitude earthquake struck close to Pinatubo, however no major damages or casualties were reported.[25]
Cultural history
The word pinatubo could mean a fertile place where one can make crops grow or could mean "made to grow" in Tagalog and Sambal, which may suggest a knowledge of its previous eruption in about 1500 AD. There is a local oral tradition that is suggestive of a folk memory of earlier large eruptions; ancient legend tells of Bacobaco, the terrible spirit of the sea, who could metamorphose into a huge turtle and who threw fire from his mouth. When being chased by the spirit hunters, Bacobaco fled to the mountain and dug a great hole in its summit showering the surrounding land with rock, mud, dust and fire for three days; howling so loudly that the earth shook.[26]
History among Aetas
Aeta elders tell many stories about the history of the mountain, the best known being that it was once a Batung Mabye (Kapampangan for living stone). It was said to have been planted on a kingdom by a displeased sorcerer but relocated by a hero. The mountain was soon turned into the abode of Apo Namalyari ("The lord of happenings/ events"), the pagan deity of the Sambal, Aeta, and Kapampangans living on the Zambales range. It was said to comprise the whole mountain range until Sinukuan of Mount Arayat (the god of the Kapampangans) became a strong rival of Namalyari. Their fight, which took place over the center plains, involved the shattering of the mountain into smaller bodies while Mount Arayat lost its center peak. Other versions have it that Pinatubo's peak shattered because of Namalyari's immense fury in an attempt to teach humans the meaning of fear and show how misdeeds will be punished.Template:Citation needed
According to the elders, Apo Namalyari, caused the 1991 eruption because of displeasure toward illegal loggers and Philippine National Oil Company executives who performed deep exploratory drilling and well testing on the mountain looking for geothermal heat from 1988 to 1990.[27] Discouraging results from the wells forced the abandonment of the prospect 13 months before the April 2, 1991 explosions.[28]
Aetas granted ownership of Pinatubo
After being driven away by the 1991 eruption of Mount Pinatubo, in May 2009 some 454 Aeta families in Pampanga were given the first clean ancestral land ownership on Mount Pinatubo with the Certificate of Ancestral Domain Title (CADT) by the National Commission on Indigenous Peoples (NCIP), the government agency that deals with issues concerning indigenous people of the Philippines. The approved and declared net land area of Template:Convert/haTemplate:Convert/test/Aon covers the barangays of Mawakat and Nabuklod in Floridablanca, Pampanga, plus a portion of San Marcelino, Zambales, and a portion of Barangay Batiawan in Subic, Zambales.[29]
On January 14, 2010, some 7,000 Aeta families from Zambales were officially granted the Certificate of Ancestral Domain Title (CADT) covering the Zambales side of Pinatubo which includes the summit and Lake Pinatubo, officially becoming their lutan tua (ancestral land). The ancestral domain title covers Template:Convert/haTemplate:Convert/test/Aon and includes the villages of Burgos, Villar, Moraza and Belbel in Botolan and portions of the towns of Cabangan, San Felipe and San Marcelino.[30][31]
Having the land title will protect them from others — including foreigners — from exploiting their land without compensation to the indigenous tribes. In the past, the Aetas had to contend with mining companies, loggers, and, recently, tourist companies who earn from Mount Pinatubo but do not compensate the local tribes.[31]
Ancestral domain titles are awarded to a certain community or indigenous group who have occupied or possessed the land continuously in accordance with their customs and traditions since time immemorial. They have the legal right to collectively possess and to enjoy the land and its natural resources to the exclusion of others.[31]
Pinatubo in popular culture
Long before Mt. Pinatubo became famous for its cataclysmic eruption, Philippine President Ramon Magsaysay, a native of Zambales, named his C-47 presidential plane "Mt. Pinatubo". The plane crashed in 1957, killing the President and 24 others on board.[32]
Hiking Pinatubo
The caldera formed and Lake Pinatubo has since become a tourist attraction with the preferred route through Barangay Santa Juliana in Capas, Tarlac.[33]
See also
- Active volcanoes in the Philippines
- Inactive volcanoes in the Philippines
- Potentially active volcanos in the Philippines
- List of volcanic eruptions by death toll
- Timetable of major worldwide volcanic eruptions
Notes
- ↑ 1.0 1.1 "Tarlac map". University of Texas in Austin Library. Retrieved on 2011-08-02.
- ↑ "Report of the Philippine Commission to the President, 1901 Vol. III", pg. 141. Government Printing Office, Washington, 1901.
- ↑ 3.0 3.1 "The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines". http://pubs.usgs.gov/fs/1997/fs113-97/. Retrieved 2007-04-09.
- ↑ Rodolfo, Umbal, and Alonso. "Two Years of Lahars on the Western Flank of Mount Pinatubo: Initiation, Flow Processes, Deposits, and Attendant Geomorphic and Hydraulic Changes". USGS Publications. Retrieved on 2012-03-07.
- ↑ 5.0 5.1 "Mt. Pinatubo's cloud shades global climate". Science News. http://www.thefreelibrary.com/Mt.+Pinatubo's+cloud+shades+global+climate.-a012467057. Retrieved 2010-03-07.
- ↑ Tactical Pilotage Chart, Sheet K-11B, Defense Mapping Agency, Department of Defense, 1982.
- ↑ U.S. War Department. "Report of the Philippine Commission, 1901 Vol. III"), pg. 141. Government Printing Office, Washington.
- ↑ Topinka, Lyn (July 13, 2009). "Description: Mount Pinatubo, Philippines". United States Geological Survey. http://vulcan.wr.usgs.gov/Volcanoes/Philippines/Pinatubo/description_pinatubo.html. Retrieved April 18, 2010.
- ↑ 9.0 9.1 9.2 9.3 9.4 9.5 9.6 9.7 Template:Cite book
- ↑ Delfin, F.G.; Villarosa, H.G.; and Layugan, D.B. "Geothermal Exploration of the pre-1001 Mount Pinatubo Hydrothermal System". United States Geological Survey Publications. Retrieved on 2012-03-07.
- ↑ USGS. "Earthquake Information for 1990". http://neic.usgs.gov/neis/eq_depot/1990/. Retrieved 2010-03-06.
- ↑ USGS Earthquake Magnitude Policy
- ↑ "The July 16 Luzon Earthquake: A Technical Monograph". Inter-Agency Committee for Documenting and Establishing Database on the July 1990 Earthquake. Philippine Institute of Volcanology and Seismology. 2001. http://earthquake.phivolcs.dost.gov.ph/update_SOEPD/Earthquake/1990LuzonEQ_Monograph/foreword.html. Retrieved 2009-01-07.
- ↑ Template:Cite journal
- ↑ In 1991, it was Pinatubo - INQUIRER.net, Philippine News for Filipinos
- ↑ "Mt. Pinatubo, Luzon, Philippines". National Geophysical Data Center (U.S. NOAA). http://www.ngdc.noaa.gov/seg/hazard/stratoguide/pinfact.html. Retrieved 2007-12-02.
- ↑ CoolGeography - Mount Pinatubo
- ↑ Template:Cite book.
- ↑ 19.0 19.1 19.2 Template:Harvnb.
- ↑ Template:Cite book
- ↑ Template:Harvnb.
- ↑ Template:Cite journal
- ↑ Shimizu, Hiromu (2002), Struggling for Existence after the Pinatubo Eruption 1991: Catastrophe, Suffering and Rebirth of Ayta Communities. Paper presented inter-congress of the International Union of Anthropological and Ethnological Sciences, Tokyo, Japan. Retrieved from the original on 2004-08-15.
- ↑ (2001_0907). "Filipinos return as volcano lake drains". BBC News.
- ↑ Gonzaga, Robert and Orejas, Tonette (2011-07-26). "5.9-magnitude quake jolts households in Luzon, Metro areas". Inquirer News.
- ↑ Rodolfo, K.S. & Umbal, J.V. (2008) "A prehistoric lahar-dammed lake and eruption of Mount Pinatubo described in a Philippine aborigine legend", J. Volcanol. Geotherm. Res., 176, 432-437
- ↑ Template:Cite news
- ↑ Delfin Jr., F.G., Villarosa, H.G.. "Geothermal Exploration of the pre-1991 Mount Pinatubo Hydrothermal System". USGS. Retrieved on 2011-08-14.
- ↑ (2009-05-27). "Aetas in Pampanga awarded first clean title of ancestral domain". Scribd. Retrieved on 2011-08-14.
- ↑ Orejas, Tonette (2009-11-27). "It’s official: Pinatubo is now owned by Aetas". Piplinks (originally from Philippine Daily Inquirer). Retrieved on 2011-08-14.
- ↑ 31.0 31.1 31.2 Valdez, Katrina Mennen A. (2010-01-14). "Aetas to receive title to domain at Mt. Pinatubo". Preda Foundation. Retrieved on 2011-08-14.
- ↑ Template:Cite news
- ↑ Template:Cite news
References
- Decker, R. and Decker, B. (1997) Volcanoes, 3rd edition, WH Freeman, New York.
- Template:Cite journal
- Template:Cite book
- Template:Cite book
- Template:Cite document
- Scaillet, B. and Evans, B. W. (1999) The June 15, 1991 Eruption of Mount Pinatubo. I. Phase Equilibria and Pre-eruption P–T–fO2–fH2O Conditions of the Dacite Magma. Journal of Petrology, v. 40, 381–411.
- Stimac J.A., Goff F., Counce D., Larocque A.C.L., Hilton D.R. (2003), The crater lake and hydrothermal system of Mount Pinatubo, Philippines: evolution in the decade after eruption, Bulletin of Volcanology, v. 66, p. 149–167
- Wiesner, M.G., Wetzel, A. Catane, S.G., Listanco, E.L. and Mirabueno, H.T. (2004) Grain size, areal thickness distribution and controls on sedimentation of the 1991 Mount Pinatubo tephra layer in the South China Sea. Bulletin of Volcanology, v. 66, 226–242.
- Dhot, S. Mt Pinatubo Safety.
External links
Template:Commons category Template:Spoken Wikipedia
- Fire and Mud. Eruptions and Lahars of Mount Pinatubo, United States Geological Survey site
- Mount Pinatubo page. Philippine Institute of Volcanology and Seismology
- Weather effects of the 1991 eruption EOS Volcanology.
- CVO Pinatubo photo archive Cascades Volcano Observatory
- The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines. United States Geological Survey site
Template:Link GA Template:Link GA Template:Link FA Template:Link FA [[zh:皮纳图博火 ]]
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Mount Pinatubo is an active stratovolcano located on the island of Luzon, near the tripoint of the Philippine provinces of Zambales, Tarlac, and Pampanga.[1] It is located in the Cabusilan Mountains[1][2] separating the west coast of Luzon from the central plains. Before the volcanic activities of 1991, its eruptive history was unknown to most people. It was heavily eroded, inconspicuous and obscured from view. It was covered with dense forest which supported a population of several thousand indigenous people, the Aetas, who fled to the mountains during the Spanish conquest of the Philippines.
The volcano's Plinian / Ultra-Plinian eruption on June 15, 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in the Alaska Peninsula.[3] Complicating the eruption was the arrival of Typhoon Yunya bringing a lethal mix of ash and rain. Successful predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but the surrounding areas were severely damaged by pyroclastic flows, ash deposits, and subsequently, by the lahars caused by rainwaters re-mobilizing earlier volcanic deposits destroying thousands of infrastructures and altering the river systems months to years after the eruption.[3][4]
The effects of the eruption were felt worldwide. It ejected roughly Template:Convert/t or Template:Convert/km3Template:Convert/test/Aon of magma, and Template:Convert/tTemplate:Convert/test/Aon Template:Chem, bringing vast quantities of minerals and metals to the surface environment. It injected large amounts of aerosol into the stratosphere – more than any eruption since that of Krakatoa in 1883. Over the following months, the aerosols formed a global layer of sulfuric acid haze. Global temperatures dropped by about Template:Convert/C-change, and ozone depletion temporarily increased substantially.[5]
Overview of the area
The volcano is located Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon northwest of Manila, the capital of the Philippines. Near Mount Pinatubo, the United States maintained two large military bases in the region. The U.S. Naval Base Subic Bay was located Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon south of Pinatubo, while the extent of Clark Air Base was just Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon to the east of the volcano's summit.[6] Clark Air Base's residential areas and petroleum storage facilities were in much closer proximity to the volcano than the airfield complex and neighboring Angeles City.
The Aetas
An indigenous group of people, the Aetas (also spelled as Ayta/Ita), had lived on the slopes of the volcano and in surrounding areas for several centuries, having fled the lowlands to escape persecution by the Spanish during their conquest of the Philippines which began in 1565. They were a hunter-gatherer people who were extremely successful in surviving in the dense jungles of the area. These people also grew some staple crops such as wheat, barley, rice and raised animals.
In total, about 30,000 people lived on the flanks of the volcano in about 25 established barangays (villages) and other small settlements like Tarukan village and Maruglu. The dense jungle covering most of the mountain and surrounding peaks supported the hunter-gathering Aeta, while on the surrounding flatter areas, the abundant rainfall of almost 4 metres (13 ft) annually) provided by the monsoon climate and the fertile volcanic soils provided excellent conditions for agriculture.
Geological history
Mount Pinatubo's summit before the 1991 eruption was Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above sea level, only about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above nearby plains, and only about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon higher than surrounding peaks, which largely obscured it from view. It is part of a chain of volcanoes which lie along the western side of the edge of the island of Luzon called the Zambales Mountains. Pinatubo belongs to the Cabusilan Mountains, the central range of the Zambales Mountains, which consists of Mt. Cuadrado, Mt. Negron, Mt. Mataba and Mt. Pinatubo.[7] They are subduction volcanoes, formed by the Eurasian Plate sliding under the Philippine Mobile Belt along the Manila Trench to the west.[8] Mount Pinatubo and the other volcanoes on this volcanic belt arise due to magma occlusion from this subduction plate boundary.
Pinatubo is flanked on the west by the Zambales Ophiolite Complex, which is an easterly-dipping section of Eocene oceanic crust which was uplifted during the late Oligocene. The Tarlac Formation consists of marine, nonmarine and volcaniclastic sediments in the north, east and southeast of Pinatubo which were formed in the late Miocene and Pliocene.[9]
The most recent study of Mount Pinatubo prior to the activities of 1991 was the overall geological study in 1983 and 1984 made by F. G. Delfin for the Philippine National Oil Company as part of the surface investigations of the area prior to the exploratory drilling and well testing for geothermal sources in 1988 to 1990. He recognized two life histories of the mountain, which he classified as 'ancestral' and 'modern' Pinatubo.[9][10]
Ancestral Pinatubo
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. Its center was roughly in the same location of the current volcano. The projected height of the mountain is up to Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above sea level if it was a lone peak, based on profile fitting to the remaining lower slopes, or lower if it had more than one peak.[9]
The old volcano is exposed in the walls of an old Template:Convert/xTemplate:Convert/test/Aon wide caldera, referred to as Tayawan Caldera by Delfin. Some of the nearby peaks are the remnants of ancestral Pinatubo, left behind when the softer parts of the old mountain slopes were eroded by weathering. Ancestral Pinatubo is a somma volcano with 'Modern' Pinatubo as the new cone. Its remaining caldera rim includes Mount Donald MacDonald, forming the southeast rim, and Mount Tayawan, the longer north to northeast rim, after which the caldera was named. Mount Dorst, to the east, is part of the dip slope of the ancestral Pinatubo. Several mountains near modern Pinatubo are old satellite vents of ancestral Pinatubo, forming volcanic plugs and lava domes. These satellite vents were probably active around the same time as the ancestral volcano and include the domes of Mount Negron, Mount Cuadrado, Mount Mataba, and the Bituin and Tapungho plugs.[9]
Modern Pinatubo
After a long period of dormancy, Modern Pinatubo was born in the cataclysmic and the most explosive eruption of Pinatubo around 35,000 years ago. The eruption, which was estimated to be five times larger than the 1991 eruption, deposited pyroclastic flow material up to 100 metres (330 ft) thick on all sides of the mountain. The total volume of pyroclastic flows deposited around the volcano may have been up to Template:Convert/km3Template:Convert/test/Aon, but the total volume of volcanic material ejected during the eruption is unknown. The removal of this amount of material from the underlying magma chamber led to the formation of the Tayawan caldera. The eruptive period started by the eruption is referred to by Delfin as the Inararo Eruptive Period, named after a village that was destroyed in the 1991 eruption.[9]
Later eruptions of Modern Pinatubo occurred episodically and lasted for periods much shorter than the repose intervals between them. Subsequent eruptions and eruptive period occurred about ~17,000 (Sacobia Eruptive Period); ~9000 (Pasbul Eruptive Period); ~6000–5000 (Crow Valley Eruptive Period); ~3,900–2,300 (Maraunot Eruptive Period); and ~500 years ago (Buag Eruptive Period). Each of these eruptions seems to have been very large, ejecting more than 10 km³ of material and covering large parts of the surrounding areas with pyroclastic flow deposits. Some eruptive periods have lasted decades and perhaps as much as several centuries and might appear to include multiple large explosive eruptions.[9]
The maximum size of eruptions in each eruptive period though have been getting smaller through the >35,000-yr history of modern Pinatubo, but this might be an artifact of erosion and (or) burial of older deposits. The oldest eruption of modern Pinatubo, Inararo, was also its largest. Those of the Pasbul period were as energetic, if not as voluminous as the Inararo eruptions. Although smaller than the Inararo eruptions, those of the Crow Valley and Maraunot periods were still about 2 to 3 times as big as that of 1991 based on the pyroclastic flow runout distances and depths of valley filling. Eruptions of the Buag period were roughly the same size as those of 1991. The 1991 eruption was among the smallest documented in its geologic record.[9]
The volcano has never grown very large in between eruptions, because it produces mostly unwelded, easily erodible deposits, and periodically destroys the viscous domes that fill its vents. After the Buag eruption (~500 years ago), the volcano lay dormant, its slopes becoming completely covered in dense rainforest and eroded into gullies and ravines. The ~500-year repose though between the Buag and present eruptive periods is among the shorter repose periods recognized in its geologic history.[9]
The 1991 eruption
Possible precursor in 1990
On July 16, 1990, the major 1990 Luzon earthquake of magnitude 7.7 struck central Luzon. This was the largest earthquake recorded in 1990,[11][12] comparable in size to the 1906 San Francisco earthquake and the 2008 Sichuan earthquake. Its epicenter was in Rizal, Nueva Ecija municipality,[13] about 100 km northeast of Pinatubo, and faulted northwest-southeast through three provinces. It also followed the Philippine Fault System west as far as Baguio City, which was devastated, and is located about 80 kilometres (50 mi) north-northeast of Pinatubo, leading volcanologists to speculate that it might ultimately have triggered the 1991 eruption, although this is impossible to prove conclusively. Two weeks after the earthquake, local residents reported steam coming from the volcano, but scientists who visited the mountain in response found only small landslides rather than any eruptive activity.
1991 activities leading to the eruption
On March 15, 1991, a succession of earthquakes was felt by villagers on the northwestern side of the volcano. Further earthquakes of increasing intensity were felt over the next two weeks, and it became clear some kind of volcanic activity was likely. On April 2, the volcano awoke, with phreatic eruptions occurring near the summit along a Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon long fissure. Over the next few weeks, small eruptions continued, dusting the surrounding areas with volcanic ash. Seismographs recorded hundreds of small earthquakes every day.
Scientists immediately installed monitoring equipment and analyzed the volcano for clues as to its previous eruptive history. Radiocarbon dating of charcoal found in old volcanic deposits revealed the last three major explosive eruption periods in recent millennia, about 5500, 3500 and 500 years ago. Geological mapping showed that much of the surrounding plains were formed by lahar deposits from previous eruptions.
Volcanic activity increased throughout May. Measurements of sulfur dioxide emissions showed a rapid increase from Template:Convert/tTemplate:Convert/test/Aon per day by May 13 to Template:Convert/tTemplate:Convert/test/Aon per day by May 28. This implied that there was a rising column of fresh magma beneath the volcano. After May 28, the amount of Template:Chem being emitted decreased substantially, raising fears that the degassing of the magma had been blocked somehow, leading to a pressure build-up in the magma chamber and a high likelihood of explosive eruptions.
The first magmatic eruptions occurred on June 3, and the first large explosion on June 7 generated an ash column Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon high. The Philippine Institute of Volcanology and Seismology (PHIVOLCS) issued a warning indicating the possibility of a major eruption within two weeks.
Evacuations
Given all the signs that a very large eruption was imminent, PHIVOLCS – assisted by the U.S. Geological Survey – worked to convince local inhabitants of the severity of the threat. A false warning might have led to cynicism about any later warnings, but delaying a warning until an eruption began might lead to thousands of deaths, so the volcanologists were under some pressure to deliver a timely and accurate assessment of the volcanic risk.
Three successive evacuation zones were defined, the innermost containing everything within 10 km of the volcano's summit, the second extending from 10 to 20 km from the summit, and the third extending from Template:Convert/-Template:Convert/test/Aon from the summit (Clark Air Base and Angeles City were in this zone). The Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon and Template:Convert/–Template:Convert/test/Aon zones had a total population of about 40,000, while some 331,000 people lived in the Template:Convert/–Template:Convert/test/Aon zone. Five stages of volcanic alert were defined, from level 1 (low level seismic disturbances) up to level 5 (major eruption in progress). Daily alerts were issued stating the alert level and associated danger area, and the information was announced in major national and local newspapers, on radio and television stations, by nongovernmental organizations (NGOs), and directly to the endangered inhabitants.
Many of the Aeta who lived on the slopes of the volcano left their villages of their own volition when the first explosions began in April, gathering in a village about 12 kilometres (Template:Rnd/- mi) from the summit. They moved to increasingly distant villages as the eruptions escalated, some Aeta moving up to nine times in the two months preceding the cataclysmic eruption.
The first formal evacuations were ordered from the Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon zone on April 7. Evacuation of the Template:Convert/–Template:Convert/test/Aon zone was ordered when a level 4 alert was issued on June 7. A level 5 alert triggered evacuation of the Template:Convert/–Template:Convert/test/Aon zone on June 13, and in all some 60,000 people had left the area within 30 kilometres (19 mi) of the volcano before June 15. Most people temporarily relocated to Manila and Quezon City, with some 30,000 using the Amoranto Velodrome in Quezon City as an evacuee camp.
Climactic eruption buildup
In early June, tiltmeter measurements had shown that the volcano was inflating, evidently due to growing amounts of magma filling the reservoir beneath the summit. At the same time, seismic activity, previously concentrated at a depth of a few kilometers below a point about 5 kilometres (Template:Rnd/- mi) northwest of the summit, shifted to shallow depths just below the summit. On June 7, the first magmatic eruptions took place with the formation of a lava dome at the summit of the volcano. The dome grew substantially over the next five days, reaching a maximum diameter of about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon and a height of Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon.
A small explosion at 03:41 on June 12 marked the beginning of a new, more violent phase of the eruption. A few hours later, large explosions lasting about half an hour generated an eruption column which quickly reached heights of over 19 kilometres (12 mi), and which generated pyroclastic flows extending up to Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon from the summit in some river valleys. Fourteen hours later, a 15-minute eruption hurled ash to heights of Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon. Friction in the uprushing ash column generated abundant lightning.
A third large eruption began at 08:41 on June 13, after an intense swarm of small earthquakes over the previous two hours. It lasted about five minutes, and the eruption column once again reached 24 km. After three hours of quiet, seismic activity began, growing more and more intense over the next 24 hours, until a three-minute eruption generated a Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon high eruption column at 13:09 on June 14.
Tephra fall from these four large eruptions was extensive to the southwest of the volcano. Two hours after the last of these four explosions, a series of eruptions began which lasted for the next 24 hours, and which saw the production of much larger pyroclastic flows and surges which traveled several kilometres down river valleys on the flanks of the volcano.
Dacite was the igneous rock making up the tephra in these eruptions and in the following climactic event. The most abundant phenocryst minerals were hornblende and plagioclase, but an unusual phenocryst mineral was also present—the calcium sulfate, anhydrite. The dacite magma was more oxidized than most magmas, and the sulfur-rich nature of the eruption was probably causally related to the redox state.
The climactic eruption
All the seismographs at Clark Air Base had been rendered inoperative by 14:30 on June 15, mostly by pyroclastic density currents. Intense atmospheric pressure variation was also recorded.
On the same day, Typhoon Yunya (1991) struck the island, passing about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon north of the volcano. The typhoon rains made direct visual observations of the eruption impossible, but measurements showed that ash was ejected to heights of Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon by the most violent phase of the eruption, which lasted about three hours. Pyroclastic flows poured from the summit, reaching as far as Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon away from it. Typhoon rains mixed with the ash deposits caused massive lahars.
The ash cloud from the volcano covered an area of some Template:Convert/km2Template:Convert/test/Aon, bringing total darkness to much of central Luzon. Almost all of the island received some ashfall, which formed a heavy, rain-saturated snow-like blanket. Tephra fell over most of the South China Sea and ashfall was recorded as far away as Vietnam, Cambodia and Malaysia.
Twelve days after the first magmatic eruptions of June 3, on June 15, 1991, by about 22:30, and about nine hours after the onset of the most recent climactic phase, atmospheric pressure waves had decreased to the pre-eruption levels. No seismic records were available at this time, but volcanologists believe 22:30 marked the end of the climactic eruption.
Vast quantities of minerals and metals were brought to the surface. Overall, introduced to the surface environment, was an estimated Template:Convert/tTemplate:Convert/test/Aon of zinc, Template:Convert/tTemplate:Convert/test/Aon of copper, Template:Convert/tTemplate:Convert/test/Aon of chromium, Template:Convert/tTemplate:Convert/test/Aon of nickel, and massive amounts of toxic heavy metals such as Template:Convert/tTemplate:Convert/test/Aon of lead, Template:Convert/tTemplate:Convert/test/Aon of arsenic, Template:Convert/tTemplate:Convert/test/Aon of cadmium, and Template:Convert/tTemplate:Convert/test/Aon of mercury.[14]
The eruption effects on aircraft
At least sixteen commercial aircraft made damaging encounters with the ash cloud ejected by the June 15 eruption, as well as others on the ground. The encounters caused loss of power to one engine on each of two different aircraft. A total of 10 engines were damaged and replaced, including all four engines of a single jumbo jet. Longer term damage to aircraft and engines was reported, including accumulation of sulfate deposits on engines.[15] The eruption also forced the Philippine Air Force to retire their Vought F8Us from service.Template:WhyTemplate:Citation needed
Aftermath of the 1991 eruption
Explosivity of the eruption
The June 15 eruption had a Volcanic Explosivity Index (VEI) of 6, and came some 450–500 years after the volcano's last known eruptive activity. The eruption ejected about Template:Convert/km3Template:Convert/test/Aon of material, making it the largest eruption since that of Novarupta in 1912 and some ten times larger than the 1980 eruption of Mount St. Helens. Ejected material such as tephra fallout and pyroclastic flow deposits are much less dense than magma, and the volume of ejected material was equivalent to about Template:Convert/km3Template:Convert/test/Aon of unerupted material.[16] The former summit of the volcano was obliterated and replaced by a caldera Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon wide. The highest point on the caldera rim now stood Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon above sea level, some Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon lower than the pre-eruption summit.
Death toll
A reported 847 people were killed by the eruption mostly by roofs collapsing under the weight of accumulated wet ash, a hazard that was amplified by the simultaneous arrival of Typhoon Yunya.[17][18] The evacuation in the days preceding the eruption certainly saved tens of thousands of lives, and has been hailed as a great success for volcanology and eruption prediction. However, damage to healthcare facilities, and the spread of illnesses in relocation facilities due to poor sanitation, led to rising death tolls in the months following the eruption.Template:Citation needed
After the eruption, about 500,000 people continue to live within Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon of the mountain, with population centers including the 150,000 in Angeles City, and 30,000 at Clark Freeport Zone.
Effects on agriculture
Many reforestation projects were destroyed in the eruption, with a total area of Template:Convert/km2Template:Convert/test/Aon valued at 125 million pesos destroyed. Agriculture was heavily disrupted, with Template:Convert/km2Template:Convert/test/Aon of rice-growing farmland destroyed, and almost 800,000 head of livestock and poultry killed, destroying the livelihoods of thousands of farmers. The cost to agriculture of eruption effects was estimated to be 1.5 billion pesos.
Many farmers near Pinatubo began growing crops such as peanuts, cassava and sweet potatoes, which are quick ripening and could be harvested before the threat of lahar flows during the late summer rainy season.[19]
Local economic and social effects
In total, 364 communities and 2.1 million people were affected by the eruption, with livelihoods and houses being damaged or destroyed. More than 8,000 houses were completely destroyed, and a further 73,000 were damaged. In addition to the severe damage sustained by these communities, roads and communications were damaged or destroyed by pyroclastic flows and lahar throughout the areas surrounding the volcanoes. Total losses in 1991 and 1992 alone were estimated at 10.6 and 1.2 billion pesos respectively, including damage to public infrastructure estimated at 3.8 billion pesos (~US$92,000,000). Education for thousands of children was seriously disrupted by the destruction of schools in the eruption.[20]
The eruption of Pinatubo severely hampered the economic development of the surrounding areas. The gross regional domestic product of the Pinatubo area accounted for about 10% of the total Philippine gross domestic product. The GRDP had been growing at 5% annually before the eruption, but fell by more than 3% from 1990 to 1991. In 1991, damage to crops and property was estimated at $374 million, to which continuing lahar flows added a further $69 million in 1992. 42 percent of the cropland around the volcano was affected by mudflows, dealing a severe blow to the agricultural economy in the region.[21]
Lahars
Since the eruption, each onset of heavy rain brought lahars from the mountain range, causing the displacement of thousands of people. Inflicting extensive damage to buildings and infrastructure costing billions to repair, a large supply of funds were spent in constructing dikes and dams to control the post-eruption lahar flows.[19]
Several important river systems stem from Mount Pinatubo, with the major rivers being the Abacan, Tarlac, Pasig-Potrero, Sta. Lucia, Bucao, Santo Tomas, Maloma, Tanguay, Ashley, and Kileng rivers. Before the eruption, these river systems were important ecosystems, but the eruption filled many valleys with deep pyroclastic deposits. Since 1991, the rivers have been clogged with sediment, and the valleys have seen frequent lahars which continued for years after the eruption. Studies show that the river systems will take years to recover from the 1991 eruption.[19]
The United States Air Force initiated a massive airlift effort to evacuate American service members and their families during and immediately following the eruption, named Operation Fiery Vigil. Most personnel were initially relocated to Guam, Okinawa, and Hawaii, although some returned to the continental United States. Clark Air Base was ultimately abandoned by the United States military, and Subic Bay reverted to Philippine control the next year following the breakdown of lease negotiations.
Global environmental effects
The powerful eruption of such an enormous volume of lava and ash injected significant quantities of aerosols and dust into the stratosphere. Sulfur dioxide oxidized in the atmosphere to produce a haze of sulfuric acid droplets, which gradually spread throughout the stratosphere over the year following the eruption. The injection of aerosols into the stratosphere is thought to have been the largest since the eruption of Krakatoa in 1883, with a total mass of Template:Chem of about Template:Convert/tTemplate:Convert/test/Aon being injected—the largest volume ever recorded by modern instruments (see chart and figure).
This very large stratospheric injection resulted in a reduction in the normal amount of sunlight reaching the Earth's surface by roughly 10% (see figure). This led to a decrease in northern hemisphere average temperatures of Template:Convert/- and a global fall of about Template:Convert/C-change.[5][22] At the same time, the temperature in the stratosphere rose to several degrees higher than normal, due to absorption of radiation by the aerosol. The stratospheric cloud from the eruption persisted in the atmosphere for three years after the eruption.
The eruption had a significant effect on ozone levels in the atmosphere, causing a large increase in the destruction rate of ozone. Ozone levels at mid-latitudes reached their lowest recorded levels, while in the southern hemisphere winter of 1992, the ozone hole over Antarctica reached its largest ever size until then, with the fastest recorded ozone depletion rates. The eruption of Mount Hudson in Chile in August 1991 also contributed to southern hemisphere ozone destruction, with measurements showing a sharp decrease in ozone levels at the tropopause when the aerosol clouds from Pinatubo and Hudson arrived.
Impact on the indigenous people of Pinatubo
The Aeta people were the hardest hit by the eruption. After the areas surrounding the volcano were declared safe, many Aetas returned to their old villages only to find them destroyed by pyroclastic and lahar deposits. Some were able to return to their former way of life, but most moved instead to government-organized resettlement areas. Conditions on these were poor, with each family receiving only small plots of land not ideal for growing crops. Many Aeta found casual labor working for lowland farmers, and overall Aeta society became much more fragmented, and reliant on and integrated with lowland culture.[23]
Aftermath of the eruptions in pictures
- Vertical eruption at Pinatubo, 1991.jpg
Explosive eruption, late June 1991
- Ashfall from Pinatubo, 1991.jpg
Snow-like ashfall caused by heavy rain mixing with ash columns
- Pinatubo - pyroclastic fall.jpg
Erosional dissection of ash deposits on Pinatubo
- Collapsed hangars at Clark Air Base.jpg
Aircraft hangars at Clark Air Base destroyed by ashfall
- Lahars from Pinatubo volcano.jpg
Lahars from Pinatubo volcano fill the broad Santo Tomás River valley SW of the volcano
- Ash from Mount Pinatubo covers NS Subic Bay.jpg
Ashes from the then eruption of Pinatubo covers the U.S. Naval Base in Subic Bay, Zambales
Activity since 1991
Following the climactic eruption of June 15, 1991, activity at the volcano continued at a much lower level, with continuous ash eruptions lasting until August 1991 and episodic eruptions continuing for another month. Activity then remained low until July 1992 when a new lava dome started growing in the caldera. Volcanologists suspected that further violent eruptions could be possible, and some areas were evacuated. However, the eruption was only minor and since that episode, the volcano has been quiet.
Lake Pinatubo
The 1991 caldera was subsequently filled with water from monsoon rains and a crater lake, Lake Pinatubo, was formed. In 1992, the growth of a lava dome formed an island, which was eventually flooded by the lake. Initially, the lake was hot and highly acidic, with a minimum pH of 2 and a temperature of about Template:Convert/C. Subsequent rainfall cooled and diluted the lake, lowering the temperature to Template:Convert/C and raising the pH to 5.5 by 2003.
The lake increased in depth by about Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon per month on average eventually submerging the lava dome, until September 2001, when fears that the walls of the crater might be unstable prompted the Philippine government to order a controlled draining of the lake. An estimated 9,000 people were once again evacuated from surrounding areas in case a large flood was accidentally triggered. Workers cut a Template:Convert/LoffAonDbSoffTemplate:Convert/test/Aon notch in the crater rim, and successfully drained about a quarter of the lake's volume.[24]
Recent activity
On the 26th of July 2011, a 5.9 magnitude earthquake struck close to Pinatubo, however no major damages or casualties were reported.[25]
Cultural history
The word pinatubo could mean a fertile place where one can make crops grow or could mean "made to grow" in Tagalog and Sambal, which may suggest a knowledge of its previous eruption in about 1500 AD. There is a local oral tradition that is suggestive of a folk memory of earlier large eruptions; ancient legend tells of Bacobaco, the terrible spirit of the sea, who could metamorphose into a huge turtle and who threw fire from his mouth. When being chased by the spirit hunters, Bacobaco fled to the mountain and dug a great hole in its summit showering the surrounding land with rock, mud, dust and fire for three days; howling so loudly that the earth shook.[26]
History among Aetas
Aeta elders tell many stories about the history of the mountain, the best known being that it was once a Batung Mabye (Kapampangan for living stone). It was said to have been planted on a kingdom by a displeased sorcerer but relocated by a hero. The mountain was soon turned into the abode of Apo Namalyari ("The lord of happenings/ events"), the pagan deity of the Sambal, Aeta, and Kapampangans living on the Zambales range. It was said to comprise the whole mountain range until Sinukuan of Mount Arayat (the god of the Kapampangans) became a strong rival of Namalyari. Their fight, which took place over the center plains, involved the shattering of the mountain into smaller bodies while Mount Arayat lost its center peak. Other versions have it that Pinatubo's peak shattered because of Namalyari's immense fury in an attempt to teach humans the meaning of fear and show how misdeeds will be punished.Template:Citation needed
According to the elders, Apo Namalyari, caused the 1991 eruption because of displeasure toward illegal loggers and Philippine National Oil Company executives who performed deep exploratory drilling and well testing on the mountain looking for geothermal heat from 1988 to 1990.[27] Discouraging results from the wells forced the abandonment of the prospect 13 months before the April 2, 1991 explosions.[28]
Aetas granted ownership of Pinatubo
After being driven away by the 1991 eruption of Mount Pinatubo, in May 2009 some 454 Aeta families in Pampanga were given the first clean ancestral land ownership on Mount Pinatubo with the Certificate of Ancestral Domain Title (CADT) by the National Commission on Indigenous Peoples (NCIP), the government agency that deals with issues concerning indigenous people of the Philippines. The approved and declared net land area of Template:Convert/haTemplate:Convert/test/Aon covers the barangays of Mawakat and Nabuklod in Floridablanca, Pampanga, plus a portion of San Marcelino, Zambales, and a portion of Barangay Batiawan in Subic, Zambales.[29]
On January 14, 2010, some 7,000 Aeta families from Zambales were officially granted the Certificate of Ancestral Domain Title (CADT) covering the Zambales side of Pinatubo which includes the summit and Lake Pinatubo, officially becoming their lutan tua (ancestral land). The ancestral domain title covers Template:Convert/haTemplate:Convert/test/Aon and includes the villages of Burgos, Villar, Moraza and Belbel in Botolan and portions of the towns of Cabangan, San Felipe and San Marcelino.[30][31]
Having the land title will protect them from others — including foreigners — from exploiting their land without compensation to the indigenous tribes. In the past, the Aetas had to contend with mining companies, loggers, and, recently, tourist companies who earn from Mount Pinatubo but do not compensate the local tribes.[31]
Ancestral domain titles are awarded to a certain community or indigenous group who have occupied or possessed the land continuously in accordance with their customs and traditions since time immemorial. They have the legal right to collectively possess and to enjoy the land and its natural resources to the exclusion of others.[31]
Pinatubo in popular culture
Long before Mt. Pinatubo became famous for its cataclysmic eruption, Philippine President Ramon Magsaysay, a native of Zambales, named his C-47 presidential plane "Mt. Pinatubo". The plane crashed in 1957, killing the President and 24 others on board.[32]
Hiking Pinatubo
The caldera formed and Lake Pinatubo has since become a tourist attraction with the preferred route through Barangay Santa Juliana in Capas, Tarlac.[33]
See also
- Active volcanoes in the Philippines
- Inactive volcanoes in the Philippines
- Potentially active volcanos in the Philippines
- List of volcanic eruptions by death toll
- Timetable of major worldwide volcanic eruptions
Notes
- ↑ 1.0 1.1 "Tarlac map". University of Texas in Austin Library. Retrieved on 2011-08-02.
- ↑ "Report of the Philippine Commission to the President, 1901 Vol. III", pg. 141. Government Printing Office, Washington, 1901.
- ↑ 3.0 3.1 "The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines". http://pubs.usgs.gov/fs/1997/fs113-97/. Retrieved 2007-04-09.
- ↑ Rodolfo, Umbal, and Alonso. "Two Years of Lahars on the Western Flank of Mount Pinatubo: Initiation, Flow Processes, Deposits, and Attendant Geomorphic and Hydraulic Changes". USGS Publications. Retrieved on 2012-03-07.
- ↑ 5.0 5.1 "Mt. Pinatubo's cloud shades global climate". Science News. http://www.thefreelibrary.com/Mt.+Pinatubo's+cloud+shades+global+climate.-a012467057. Retrieved 2010-03-07.
- ↑ Tactical Pilotage Chart, Sheet K-11B, Defense Mapping Agency, Department of Defense, 1982.
- ↑ U.S. War Department. "Report of the Philippine Commission, 1901 Vol. III"), pg. 141. Government Printing Office, Washington.
- ↑ Topinka, Lyn (July 13, 2009). "Description: Mount Pinatubo, Philippines". United States Geological Survey. http://vulcan.wr.usgs.gov/Volcanoes/Philippines/Pinatubo/description_pinatubo.html. Retrieved April 18, 2010.
- ↑ 9.0 9.1 9.2 9.3 9.4 9.5 9.6 9.7 Template:Cite book
- ↑ Delfin, F.G.; Villarosa, H.G.; and Layugan, D.B. "Geothermal Exploration of the pre-1001 Mount Pinatubo Hydrothermal System". United States Geological Survey Publications. Retrieved on 2012-03-07.
- ↑ USGS. "Earthquake Information for 1990". http://neic.usgs.gov/neis/eq_depot/1990/. Retrieved 2010-03-06.
- ↑ USGS Earthquake Magnitude Policy
- ↑ "The July 16 Luzon Earthquake: A Technical Monograph". Inter-Agency Committee for Documenting and Establishing Database on the July 1990 Earthquake. Philippine Institute of Volcanology and Seismology. 2001. http://earthquake.phivolcs.dost.gov.ph/update_SOEPD/Earthquake/1990LuzonEQ_Monograph/foreword.html. Retrieved 2009-01-07.
- ↑ Template:Cite journal
- ↑ In 1991, it was Pinatubo - INQUIRER.net, Philippine News for Filipinos
- ↑ "Mt. Pinatubo, Luzon, Philippines". National Geophysical Data Center (U.S. NOAA). http://www.ngdc.noaa.gov/seg/hazard/stratoguide/pinfact.html. Retrieved 2007-12-02.
- ↑ CoolGeography - Mount Pinatubo
- ↑ Template:Cite book.
- ↑ 19.0 19.1 19.2 Template:Harvnb.
- ↑ Template:Cite book
- ↑ Template:Harvnb.
- ↑ Template:Cite journal
- ↑ Shimizu, Hiromu (2002), Struggling for Existence after the Pinatubo Eruption 1991: Catastrophe, Suffering and Rebirth of Ayta Communities. Paper presented inter-congress of the International Union of Anthropological and Ethnological Sciences, Tokyo, Japan. Retrieved from the original on 2004-08-15.
- ↑ (2001_0907). "Filipinos return as volcano lake drains". BBC News.
- ↑ Gonzaga, Robert and Orejas, Tonette (2011-07-26). "5.9-magnitude quake jolts households in Luzon, Metro areas". Inquirer News.
- ↑ Rodolfo, K.S. & Umbal, J.V. (2008) "A prehistoric lahar-dammed lake and eruption of Mount Pinatubo described in a Philippine aborigine legend", J. Volcanol. Geotherm. Res., 176, 432-437
- ↑ Template:Cite news
- ↑ Delfin Jr., F.G., Villarosa, H.G.. "Geothermal Exploration of the pre-1991 Mount Pinatubo Hydrothermal System". USGS. Retrieved on 2011-08-14.
- ↑ (2009-05-27). "Aetas in Pampanga awarded first clean title of ancestral domain". Scribd. Retrieved on 2011-08-14.
- ↑ Orejas, Tonette (2009-11-27). "It’s official: Pinatubo is now owned by Aetas". Piplinks (originally from Philippine Daily Inquirer). Retrieved on 2011-08-14.
- ↑ 31.0 31.1 31.2 Valdez, Katrina Mennen A. (2010-01-14). "Aetas to receive title to domain at Mt. Pinatubo". Preda Foundation. Retrieved on 2011-08-14.
- ↑ Template:Cite news
- ↑ Template:Cite news
References
- Decker, R. and Decker, B. (1997) Volcanoes, 3rd edition, WH Freeman, New York.
- Template:Cite journal
- Template:Cite book
- Template:Cite book
- Template:Cite document
- Scaillet, B. and Evans, B. W. (1999) The June 15, 1991 Eruption of Mount Pinatubo. I. Phase Equilibria and Pre-eruption P–T–fO2–fH2O Conditions of the Dacite Magma. Journal of Petrology, v. 40, 381–411.
- Stimac J.A., Goff F., Counce D., Larocque A.C.L., Hilton D.R. (2003), The crater lake and hydrothermal system of Mount Pinatubo, Philippines: evolution in the decade after eruption, Bulletin of Volcanology, v. 66, p. 149–167
- Wiesner, M.G., Wetzel, A. Catane, S.G., Listanco, E.L. and Mirabueno, H.T. (2004) Grain size, areal thickness distribution and controls on sedimentation of the 1991 Mount Pinatubo tephra layer in the South China Sea. Bulletin of Volcanology, v. 66, 226–242.
- Dhot, S. Mt Pinatubo Safety.
External links
Template:Commons category Template:Spoken Wikipedia
- Fire and Mud. Eruptions and Lahars of Mount Pinatubo, United States Geological Survey site
- Mount Pinatubo page. Philippine Institute of Volcanology and Seismology
- Weather effects of the 1991 eruption EOS Volcanology.
- CVO Pinatubo photo archive Cascades Volcano Observatory
- The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines. United States Geological Survey site
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