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strombolian eruption sentence in Hindi

"strombolian eruption" meaning in Hindistrombolian eruption in a sentence
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  • Strombolian eruptions are similar to Hawaiian eruptions, but there are differences.
  • The lahar had been caused by a strombolian eruption in Villarrica Volcano.
  • The field was probably formed by Strombolian eruptions accompanied by lava fountaining.
  • The tephra is dispersed over a wider area than that from Strombolian eruptions.
  • The volcano has scoria cones suggesting Strombolian eruptions.
  • The volcano usually generates strombolian eruptions, with ejection of incandescent pyroclasts and lava flows.
  • They typically form proximally during Strombolian eruptions, and are common at strongly peralkaline volcanoes.
  • The strombolian eruptions which started five months after on January 31, 1968 produced the first historical lava fountaining witnessed from Taal.
  • The lavas formed by Strombolian eruptions are a form of relatively viscous basaltic lava, and its end product is mostly scoria.
  • Imbabura is the product of Strombolian Eruptions, which, in comparison to Plinian Eruptions, are relatively low-intensity and low volume.
  • Plinian eruptions are similar to both Vulcanian and Strombolian eruptions, except that rather than creating discrete explosive events, Plinian eruptions form sustained eruptive columns.
  • Characteristic eruptive activity consists of Strombolian eruptions from the lava lake or from one of several subsidiary vents, all within the volcano's inner crater.
  • His descriptions of these eruptions became the basis for two indices in the Volcanic Explosivity Index : 1-Strombolian eruption, and 2-Vulcanian eruption.
  • In reality, true Strombolian eruptions are characterized by short-lived and explosive eruptions of lavas with intermediate viscosity, often ejected high into the air.
  • Surtseyan eruptions are the " wet " equivalent of ground-based Strombolian eruptions, but because of where they are taking place they are much more explosive.
  • Strombolian eruptions during the second and final eruptive period about 10, 000 years ago constructed a small pyroclastic cone on the eastern rim of the older basaltic andesite tuff ring.
  • To distinguish between them, Mercalli defined Strombolian eruptions as " . . . " Mildly explosive at discrete but fairly regular intervals of seconds to minutes " . . ."
  • The products of Surtseyan eruptions are generally oxidized palagonite basalts ( though andesitic eruptions do occur, albeit rarely ), and like Strombolian eruptions Surtseyan eruptions are generally continuous or otherwise rhythmic.
  • Another strombolian eruption followed a year later on October 29, 1969 . The massive flows from the two eruptions eventually covered the bay created by the 1965 eruption, reaching the shore of Lake Taal.
  • The relative passivity of Strombolian eruptions, and its non-damaging nature to its source vent allow Strombolian eruptions to continue unabated for thousands of years, and also makes it one of the least dangerous eruptive types.
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