Valley Fault System (VFS)

July 16, 1990 Luzon Earthquake

Subduction Zones Located in Developing Countries

 

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Phreatic - explosion driven by steam produced by heating and expansion of groundwater due to an underlying hot source.  This type involves only water, steam and ash with other rock fragments derived from pre-existing rocks, without ejection of fresh magmatic materials.

 

Examples: 

1993 & 1996 eruptions of Canlaon Volcano

1988 eruption of Bulusan Volcano

Phreatomagmatic - eruption resulting from the ejection of magmatic gases and steam produced by the conversion of groundwater to steam by ascending magma, mixed with water, fine ash with or without accretionary lapilli and variably-sized volcanic bombs fragmented from the pre-existing rock formations, and fresh magmatic ejecta.  The eruption forms a high eruption column with a radially spreading ring-shaped horizontal cloud at the base due to peeling of the crater lip or deflection in the rise of later ejections caused by the pressure of falling pyroclastic materials.

Example:

1965 & 1967 eruptions of Taal Volcano

Strombolian - weak to violent eruption characterized by lava fountaining and effusion of molten lava.  Typical ejecta are ovoid and fusiform bombs and scoria (cinders).  Ash is relatively minor in amount and eruption cloud is generally yellowish to white in color.

Examples:

1968 & 1969 eruptions of Taal Volcano

1978 eruption of Mayon Volcano

First phase of 2001 eruption of Mayon Volcano

 

Vulcanian - eruption resulting from the release of large quantities of accumulated magmatic gas which lefts fine ashes and blocks coming from the magma with great force high in the air forming voluminous eruption clouds.

Examples:

First phase of 1993 eruption of Mayon Volcano

2nd phase of 2000 & 2001 eruptions of Mayon Volcano

Peleean - eruption caused by the release of large quantities of gas from an extremely viscous magma that hurls out ash and other pyroclastic materials and is characterized by the presence of nuee ardente or glowing avalanche consisting of hot gases made dense by a suspended load of pyroclastic material.

Example:

1948-1953 eruption of Hibok-Hibok Volcano

Plinian - eruption of great violence characterized by voluminous explosive ejections of pumice and pyroclastic flows. The copious extrusion of gas-rich silicious magma is commonly accompanied by collapse of the top of the volcanic cone forming a caldera. Example: Pinatubo Volcano 1991 eruption.

Example:

1991 eruption of Pinatubo Volcano



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