vulcanian eruption oor Spaans
vulcanian eruption
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erupción vulcaniana
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type of volcanic eruption
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erupción volcánica de tipo explosivo
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The style of eruption seen on the Fossa cone is called a Vulcanian eruption, being the explosive emission of pyroclastic fragments of viscous magmas caused by the high viscosity preventing gases from escaping easily.
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Small vulcanian eruptions and lava through S flank.
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Further activity in 2007 ejected notable amounts (40-65%) of recycled material during Vulcanian eruptions.
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Explosion of magma at Krakatau at the beginning of a vulcanian eruption
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Video showing a vulcanian eruption at Fuego volcano on 11 January.
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Its eruptions, which often occur several times an hour, are classified as Strombolian or Vulcanian.
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Between these two extremes, there are the Strombolian erup- tions, of medium explosivity and small quanti- ties of lava, and the Vulcanian eruptions, some- what more explosive and with more lava.
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Most of the eruptions have consisted of short- lived explosions, Strombolian eruptions, hydro-volcanic interactions triggering Vulcanian eruptions, one Subplinian event and transitional style phases, which is supported by analysis of tephra components.
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Volcanic Activity: Vulcanian and strombolian eruptions (explosive eruptions) with tephra emission and ejection, lava flows, pyroclastic flows, ash and gases.
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The volcano usually generates Vulcanian to Plinian eruptions, which produce swift-moving currents of hot gas and rock called pyroclastic flows.
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Degasification is considered the principal cause that controls the variations of the physical properties. The “open system” eruptive activity is related to high degasification rates, low generation of ash and a greater amount of particles with micro-vesicle. The high explosive eruptive activity is characterized by strong explosions (IRP “Infrasound Reduced Pressure” >100 Pa) and has been defined in this report as “intermittent vulcanian eruptions”.
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Vulcanian or Vesubian type volcanoes, on the contrary, are highly dangerous due to the type of eruption, the fact that they usually emit ash, as well as due to other associated phenomena.
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Our goal is to quantify the amount of both “phases” in the ash samples to related with the possible mechanisms that triggers the eruption...for those who are geologists/volcanologists that means to distinguish between Strombolian (magma or juvenil) and Vulcanian activity (dome destruction).
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13 sinne gevind in 6 ms. Hulle kom uit baie bronne en word nie nagegaan nie.