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Contents

   



(Top)
 


1 Location  





2 Physical features  



2.1  Tiwi Geothermal Power Plant  







3 Classification  





4 Eruptions & activities  



4.1  1970 earthquake swarms  





4.2  Small explosion in 1980  







5 Mythology  





6 See also  





7 References  





8 External links  














Malinao Volcano






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Coordinates: 13°2458N 123°3630E / 13.41611°N 123.60833°E / 13.41611; 123.60833
 

From Wikipedia, the free encyclopedia
 


Mount Malinao
Mount Malinao
Mount Malinao with Tiwi Geothermal Field in the foreground
Highest point
Elevation1,548 m (5,079 ft)[1][2]
Prominence1,400 m (4,600 ft)
ListingPotentially active volcano
Coordinates13°24′58N 123°36′30E / 13.41611°N 123.60833°E / 13.41611; 123.60833
Geography
Mount Malinao is located in Albay
Mount Malinao

Mount Malinao

Location within Albay

Mount Malinao is located in Luzon
Mount Malinao

Mount Malinao

Mount Malinao (Luzon)

Mount Malinao is located in Philippines
Mount Malinao

Mount Malinao

Mount Malinao (Philippines)

CountryPhilippines
RegionBicol Region
Provinces
  • Camarines Sur
  • City/municipality
  • Malinao
  • Tiwi
  • Geology
    Age of rock500,000-600,000 years
    Mountain typestratovolcano
    Volcanic arc/beltBicol Volcanic Chain
    Last eruption1980
    Map

    Mount Malinao is a potentially active[3] stratovolcano located in the Bicol Region of the Philippines. The volcano displays strong fumarolic activity which is harnessed for generating electricity. Located on its slope is Tiwi Geothermal Power Plant, one of the first geothermal energy plant commissioned in the country.[4]

    Location[edit]

    Malinao Volcano is situated between the provincesofAlbay and Camarines Sur in the southeastern region of Luzon Island; about 20 km (12 mi) north-northwest of Mayon volcano, the most active volcano in the Philippines.

    Physical features[edit]

    The mountain is forested with an elevation of 1,548 metres (5,079 ft) above sea level and a base diameter of 22.5 kilometres (14.0 mi). On the summit of the volcano is a large crater with bare inner walls that are breached on the eastern side. On the lower flank this side of the predominantly andesitic volcano, is Luzon's largest solfataras and hot springs, some of which deposit siliceous sinter. Naglagbong and Jigabo are two thermal wells located on the volcano. Temperatures up to 108 °C (226 °F) were recorded on the fumaroles of Naglagbong.[1][2]

    Tiwi Geothermal Power Plant[edit]

    This area was one of the first studied for generating electricity starting with a 250 kW power plant in 1967.[5] In 1979, the first of the three 110 MW geothermal power plant was commissioned that year; the other two, in 1980 and 1982. At its peak, the plant was producing a maximum of 330 MW output. Recently, the 1979 plant was decommissioned due to decrease in steam supply.[6][7]

    Classification[edit]

    The Philippine Institute of Volcanology and Seismology (PHIVOLCS), the government bureau that deals with volcanism in the country classifies Malinao as a potentially active volcano.[8][2]

    Eruptions & activities[edit]

    There are no historical eruptions from Malinao which is believed to have been active from about 500,000 years ago until 60,000 years ago.[1]

    1970 earthquake swarms[edit]

    There was an increase in seismicity in 1970 accompanied by rumbling noises in Malinao prompting an issue of warning that the mountain might be reactivating. The tremors detected were ranging from 1 to 5 in intensity.[1]

    Small explosion in 1980[edit]

    There was a minor phreatic explosion in the Naglagbong pool area in Tiwi on July 29, 1980, ejecting mud and rocks up to 23 metre (2 ft 2 in), reaching 150 metres (490 ft) in height and distances up to 350 metres (1,150 ft). One person was injured and two buildings were damaged by the explosion. Prior to the event, as early as July 6, the area was experiencing unusual microseisms recorded at seismic station of the Commission on Volcanology (COMVOL) - the predecessor of PHIVOLCS - in the area. Geysering was also observed on the pool, two hours before the explosion. One theory about the cause of the explosion was water drawdown during the development of the Tiwi geothermal field.[1]

    Mythology[edit]

    The volcano is believed to be the home of the ancient Bicolano god of beasts, Asuang, who challenged the supreme god of the Bicolano, Gugurang. He is worshiped alongside his friend, Bulan, the boy-god of the moon.[3]

    See also[edit]

    References[edit]

    1. ^ a b c d e "Malinao". Global Volcanism Program. Smithsonian Institution.
  • ^ a b c "Malinao". Philippine Institute of Volcanology and Seismology. Archived from the original on 5 October 2011. Retrieved 19 March 2019.
  • ^ a b "Bicolano Pantheon of Deities and Creatures | Philippine Mythology • THE ASWANG PROJECT". 8 February 2016.
  • ^ (2009-01-20). "The Tiwi Geothermal Power Plant" Archived 2011-08-06 at the Wayback Machine. JCMiras.net. Retrieved on 2011-09-24.
  • ^ (2009-01-20). "The History of Geothermal Energy Development and Production in the Philippines" Archived 2011-08-06 at the Wayback Machine. JCMiras.net. Retrieved on 2011-09-24.
  • ^ (2008-06-17). "Geothermal Power Plants in the Philippines. Archived 2011-09-27 at the Wayback Machine. JCMiras.net. Retrieved on 2011-09-24.
  • ^ (2008-02-24). "Geothermal Energy Resources in the Philippines". JCMiras.net. Retrieved on 2011-09-24.
  • ^ "Potentially Active". Philippine Institute of Volcanology and Seismology. 30 Jul 2008. Archived from the original on 13 February 2012. Retrieved 19 March 2019.
  • External links[edit]


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Malinao_Volcano&oldid=1199048356"

    Categories: 
    Stratovolcanoes of the Philippines
    Subduction volcanoes
    Volcanoes of Luzon
    Mountains of the Philippines
    Landforms of Albay
    Landforms of Camarines Sur
    Potentially active volcanoes of the Philippines
    Pleistocene stratovolcanoes
    Hidden categories: 
    Pages using gadget WikiMiniAtlas
    Webarchive template wayback links
    Articles with short description
    Short description is different from Wikidata
    Coordinates on Wikidata
    Infobox mapframe without OSM relation ID on Wikidata
    Articles with GVP identifiers
    Pages using the Kartographer extension
     



    This page was last edited on 25 January 2024, at 19:43 (UTC).

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