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Not necessarily. A summit eruption may be explosive or effusive. It is considered a summit eruption when material erupts at or near the volcano's peak as opposed to on its flanks.
Most explosive volcanoes are stratovolcanoes, also called composite volcanoes.
As of 2010, Popocatepetl is erupting. According to the Smithsonian National Museum of Natural History, continuous activity since Jan. 2005 has resulted in phreatic explosions, which occur when molten lava contacts water. In Popocatepetl's case the water inside the crater comes from the heat of the rising magma melting the glaciers on its peak.
Igneous rock that flowed out of the surface if lava; lava blown out of explosive eruptions is Volcanic Ash, or Tuff.
A lateral blast is an explosive volcanic eruption the ejects material horizontally to one side rather than vertically as most explosive eruptions do.
Not necessarily. A summit eruption may be explosive or effusive. It is considered a summit eruption when material erupts at or near the volcano's peak as opposed to on its flanks.
No. Magma is molten rock that has not erupted. After it erupts it may or may not form pyroclastic material depending on how explosive the eruption is.
Most explosive volcanoes are stratovolcanoes, also called composite volcanoes.
usually when it erupts its pretty much effusive or explosive
If the composition of the magma is high in silica, the eruption will be explosive. The Eruption of Mt. St. Helens was an explosive eruption. If the composition of the magma is low in silica, it will produce a quiet eruption. The eruption(s) of Mt. Kilauea are quiet eruptions.
During an explosive eruption, a volcano sends out superheated ash, gas, and rock. Depending on the nature of the eruption, pyroclastic flows can develop in three ways:A lateral blast directly ejects the flow, though this is a rather rare event. In another scenario, dense pyroclastic material erupts and spills out of the vent or over the crater rim. In still other cases a vertical eruption column collapses and material flows downhill.In all cases the flow involves a mass of ash, rock, and gas that is too dense to rise on its own, and instead hugs the ground.Most pyroclastic flows are produced during explosive eruptions of stratovolcanoes.
As of 2010, Popocatepetl is erupting. According to the Smithsonian National Museum of Natural History, continuous activity since Jan. 2005 has resulted in phreatic explosions, which occur when molten lava contacts water. In Popocatepetl's case the water inside the crater comes from the heat of the rising magma melting the glaciers on its peak.
A volcano erupts because there is mass pressure under it. In a volcano there is hot, melted rock called lava. The hot lava produces gasses that build up underground until there is too much for the rock to contain, that makes the eruption. When there is too much, it bursts the volcano. There are two types of eruptions. Non explosive and explosive. When they are explosive, it is caused by clouds of hot debris and gases.
When a volcano erupts explosively it does not produce lava; it produces ash and pumice. The magma involved in an explosive eruption is usually felsic or intermediate. Rhyolite, dacite, and andesite are the most commonly discussed in beginner-level geology classes. However, if water gets into the volcano any type of magma can produce an explosive eruption.
Yes, Mount Etna does have explosive eruptions. This is because the eruption releases pyroclastic material, made up of felsic lava which is rich in silicate materials. Therefore, causing the giant explosion!
The composition of the magma affects how explosive a volcanic eruption will be.
its like josephs farts explosive!