bubbles
Nonexplosive eruptions typically produce lava flows, which are molten rock that emerges from the volcano and flows slowly down its slopes. This type of eruption is characterized by the relatively gentle release of magma and gas, without the violent ejection of material seen in explosive eruptions.
The Unzen volcano in Japan has mainly produced explosive eruptions, characterized by the ejection of ash, rocks, and pyroclastic flows. These eruptions are caused by the build-up of pressure from magma beneath the surface.
Paricutin is an explosive volcano. It is classified as a scoria cone volcano, which is a type of volcanic cone that is formed by explosive eruptions. Paricutin's eruptions were characterized by the ejection of molten rock fragments, ash, and gases, leading to the formation of a cone-shaped structure. The explosive nature of Paricutin's eruptions is attributed to the high gas content and viscosity of the magma beneath the volcano.
It is a composite volcano, so the kind of eruptions it has is explosive.
Magma that tends to cause explosive eruptions is typically high in silica content, making it thick and viscous. This results in gas build-up and pressure within the magma chamber, leading to explosive eruptions.
Non-explosive and Explosive
Nonexplosive eruptions typically produce lava flows, which are molten rock that emerges from the volcano and flows slowly down its slopes. This type of eruption is characterized by the relatively gentle release of magma and gas, without the violent ejection of material seen in explosive eruptions.
The Unzen volcano in Japan has mainly produced explosive eruptions, characterized by the ejection of ash, rocks, and pyroclastic flows. These eruptions are caused by the build-up of pressure from magma beneath the surface.
Paricutin is an explosive volcano. It is classified as a scoria cone volcano, which is a type of volcanic cone that is formed by explosive eruptions. Paricutin's eruptions were characterized by the ejection of molten rock fragments, ash, and gases, leading to the formation of a cone-shaped structure. The explosive nature of Paricutin's eruptions is attributed to the high gas content and viscosity of the magma beneath the volcano.
Explosive
It is a composite volcano, so the kind of eruptions it has is explosive.
are also known as Strato volcanoes. They are the most common type of volcano, and are formed by explosive eruptions of pyroclastic material followed by a quiet outpouring of lava.
It's has explosive eruptions not quiet ones.
Magma that tends to cause explosive eruptions is typically high in silica content, making it thick and viscous. This results in gas build-up and pressure within the magma chamber, leading to explosive eruptions.
Soufriere Hills volcano in Montserrat has primarily experienced explosive eruptions. These eruptions are characterized by the ejection of ash, gas, and pyroclastic material from the volcano. However, there have been periods of effusive eruptions as well, where lava flows have been released from the volcano.
Rhyolite is associated with explosive eruptions.
The answer is Explosive . It is explosive because during a explosive eruption there are clouds of ash, gas , and rock , and with a pyroclastic flow there is dust and ash . there for the answer must be explosive .