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Context
WHEN BULUSAN AWAKES

The clock is ticking

To date it has proved extremely difficult to forecast when a particular volcano is going to erupt. In the case of Pinatubo we knew a few days beforehand that there was a high risk of eruption. The scale and seriousness of the eruption were not forecasted, however. The challenge is therefore to draw up, for these regions, a kind of 'scenario' of what could happen if a certain volcano were to erupt. It is important to know what kind of eruption can be expected and what areas are potentially threatened by various kinds of volcanic dangers, such pyroclastic flows, lava flows and lava domes, lahars or volcanic mudflows, and tephra fall or ash rain.

 


The landscape around Mt. Pinatubo
before the eruption (1991) (photo USGS)

 

Will it be violent?

Depending on the type of volcano, various kinds of eruption are possible, ranging from the very explosive to those on Hawaii where the lava flow is relatively calm. Most of the volcanoes in the Philippines are of the explosive variety and consequently pose a serious potential risk to the environment.
It is difficult to say what kind of volcanic hazard could be faced. In most cases it is a combination of various hazards. The assumption is that future eruptions will be of the same type as past eruptions. Descriptions of previous eruptions are often to be found in reports or other historical documents. But in most cases these descriptions do not make it possible to identify what kind of eruption took place and when, and a detailed field study by geologists and volcanologists is necessary before this can be ascertained. Modern carbon and other dating methods allow us to determine when an eruption took place.

In this study, hazard zonation maps is drawn up for the Bulusan volcano, for various types of eruption.

 


Eruption of the Pinatubo volcano (1991) (photo: David H. Harlow, USGS).


The landscape around Mt. Pinatubo after the eruption (1991) (photo USGS)

 

Slowly flowing lava and hot ash clouds

The Bulusan volcano is what is known as an andesitic stratovolcano. The base of the present Bulusan volcano consists of older volcanic dome structures and deposits and is relatively low and very irregular in shape.
The crater is at a height of 1560 m above sea level. The top of the volcano is much steeper and has a domed shape formed by the most recent lava flows. These domes were principally formed as a result of the high viscosity of the andesitic lava. The lava flows very slowly and cools close to the crater opening. As a result, the lava accumulates close to the crater and a typical dome structure is formed.

The biggest danger posed by the formation of lava domes is the collapse of the steep mass of lava, which can result in the formation of pyroclastic flows (hot ash flows or 'nuées ardentes'). These hot ash and stone avalanches move extremely quickly and are very destructive. As the highly viscous lava can block the crater opening, there is also the risk of high pressure building up underneath it. This can lead to the explosion of the mass of hot lava and the formation of very powerful pyroclastic flash flows.

Past eruptions


Panoramic view of the Bulusan volcano, looking northeast.
On the left of the photo is the Jormahan dome and in the
foreground the fertile Irosin Valley (photo: S. Slob, Sept. 1996)

 

Historical sources showed that the Bulusan volcano had known 15 eruptive periods since 1852. Most were phreatic eruptions however, and were relatively harmless and accompanied only by light ash rain and falling boulders. No mention was found of human casualties or serious damage to property.
During the active period from 1918-1922, lava flows were observed and described that could indicate that pyroclastic flows were produced.