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This is another example and image. Mount Pinatubo is an active stratovolcano in the Cabusilan Mountains on the island of Luzon, near the tripoint of the Philippine provinces of Zambales, Tarlac and Pampanga. 

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This is another example and image. Mount Pinatubo is an active stratovolcano in the Cabusilan Mountains on the island of Luzon, near the tripoint of the Philippine provinces of Zambales, Tarlac and Pampanga. 

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This is an example and image.  Mount St. Helens is a Stratovolcano located  in Washington.  This volcano is still active.

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This is an example and image.  Mount St. Helens is a Stratovolcano located  in Washington.  This volcano is still active.

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Another very common and deadly hazard at most strato volcanoes  is called a Lahar.  Lahar is an Indonesian  word for a mudflow, and most geologists use the term to mean a  mudflow on an active volcano.

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Another very common and deadly hazard at most strato volcanoes  is called a Lahar.  Lahar is an Indonesian  word for a mudflow, and most geologists use the term to mean a  mudflow on an active volcano.

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This is an image of a lahar.

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Additionally, strato volcanoes  are steep piles of ash, lava, and domes that are often rained  heavily on, shaken by earthquakes, or oversteepened by intruding  blobs of magma (or all of these). This makes the likelihood of  landslides, avalanches, and mudflows all very high. 

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Additionally, strato volcanoes  are steep piles of ash, lava, and domes that are often rained  heavily on, shaken by earthquakes, or oversteepened by intruding  blobs of magma (or all of these). This makes the likelihood of  landslides, avalanches, and mudflows all very high. 

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First is that there  are so many more strato volcanoes than any of the other types.  This means that there will also be lots of people who end up living  on the flanks of these volcanoes.

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First is that there  are so many more strato volcanoes than any of the other types.  This means that there will also be lots of people who end up living  on the flanks of these volcanoes.

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Although they are not as explosive as large silicic caldera complexes,  strato volcanoes have caused by far the most casualties of any  type of volcano.

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Although they are not as explosive as large silicic caldera complexes,  strato volcanoes have caused by far the most casualties of any  type of volcano.

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Examples of strato volcanoes include  Mt. St. Helens, Mt. Rainier, Pinatubo, Mt. Fuji, Merapi, Galeras,  Cotopaxi, and plenty others.

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Examples of strato volcanoes include  Mt. St. Helens, Mt. Rainier, Pinatubo, Mt. Fuji, Merapi, Galeras,  Cotopaxi, and plenty others.

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This is the cause of the cooler and differentiated  magma compositions and the reason for the usually long repose  periods between eruptions.

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This is the cause of the cooler and differentiated  magma compositions and the reason for the usually long repose  periods between eruptions.

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Strato volcanoes are commonly found along  subduction-related  volcanic arcs, and the magma supply rates to strato volcanoes  are lower. 

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Strato volcanoes are commonly found along  subduction-related  volcanic arcs, and the magma supply rates to strato volcanoes  are lower. 

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The lava  at strato volcanoes  occasionally forms 'a'a, but more commonly it barely flows at  all, preferring to pile up in the vent to form volcanic domes.  Some strato volcanoes are just a collection of domes piled up  on each other. 

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The lava  at strato volcanoes  occasionally forms 'a'a, but more commonly it barely flows at  all, preferring to pile up in the vent to form volcanic domes.  Some strato volcanoes are just a collection of domes piled up  on each other. 

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Strato volcanoes are usually about half-half  lava and pyroclastic material, and the layering  of these products gives them their other common name of composite  volcanoes.

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Strato volcanoes are usually about half-half  lava and pyroclastic material, and the layering  of these products gives them their other common name of composite  volcanoes.

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Most strato volcanoes are characterized by eruptions  of andesite and dacite - lavas that are cooler and more viscous  than basalt. These more viscous lavas allow gas pressures to build  up to high levels (they are effective "plugs" in the  plumbing), therefore these volcanoes often suffer explosive eruptions.

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Most strato volcanoes are characterized by eruptions  of andesite and dacite - lavas that are cooler and more viscous  than basalt. These more viscous lavas allow gas pressures to build  up to high levels (they are effective "plugs" in the  plumbing), therefore these volcanoes often suffer explosive eruptions.

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Strato Volcanoes comprise the largest percentage (~60%) of the  Earth's individual volcanoes. 

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Strato Volcanoes comprise the largest percentage (~60%) of the  Earth's individual volcanoes. 