Mount Pinatubo is a stratovolcano, which is characterized by having a tall, conical shape with steep sides. Stratovolcanoes like Pinatubo typically have explosive eruptions and are associated with magma that is high in silica content, resulting in thick and viscous lava flows.
Mount Pinatubo is predominantly composed of andesite, which is an intermediate volcanic rock type. This rock type is typically associated with explosive volcanic activity due to its high silica content.
The magma that erupts at Mount Pinatubo is mainly dacitic in composition, which is a type of intermediate magma that is rich in silica. This type of magma typically leads to explosive eruptions due to its high viscosity and gas content.
A type of eruption that produces a viscous magma with 53 percent silica and a gas content of 2 percent is typically associated with a stratovolcano or a composite volcano. These eruptions are explosive due to the high viscosity of the magma, leading to the buildup of gas pressure before an explosive release. Example volcanoes with this type of eruption style include Mount St. Helens in the United States and Mount Pinatubo in the Philippines.
Mount St. Helens is a stratovolcano, also known as a composite volcano. This type of volcano is characterized by its steep slopes and explosive eruptions due to a mixture of lava flows and pyroclastic material.
Mount Mahuja is a stratovolcano, also known as a composite volcano. These are characterized by their steep-sided symmetrical cones and explosive eruptions due to the high viscosity of the magma. They typically alternate between explosive and effusive eruptions.
mt. Pinatubo is a fold mountain-mitzie...(Philippines)
Mount Pinatubo is a stratovolcano or composite volcano. The last eruption happened in 1993
Mount Pinatubo is a Stratovolcano or also known as Composite Volcano
Mount Pinatubo is a stratovolcano or composite volcano. The last eruption happened in 1993
About 300 people were killed in the 1991 Mount Pinatubo lahar disaster in the Philippines. The lahar, which is a type of volcanic mudflow, was triggered by the eruption of Mount Pinatubo. It caused widespread destruction in the surrounding areas.
Mount Pinatubo had LATERAL eruption. It means, generally volcano erupts at its highest peak where its vent finds an opening, but mount Pinatubo got a weak side and therefore it erupted laterally.
Mount Pinatubo primarily erupts dacitic magma.
It is a Composite Volcano (Stratovolcano) and is located in the Philippines
yes Mt Pinatubo is a composite volcano
Composite, or Stratovolcano
Mount Pinatubo is a composite volcano, also known as a stratovolcano. It is characterized by its steep symmetrical cone shape and explosive eruptions caused by the combination of lava flows and pyroclastic material.
volcanos