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español: Ceniza volcánica
English: Volcanic ash consists of small tephra, which are bits of pulverized rock and glass created by volcanic eruptions,[1] less than 2 millimetres (0,079 in) in diameter. There are three mechanisms of volcanic ash formation: gas release under decompression causing magmatic eruptions; thermal contraction from chilling on contact with water causing phreatomagmatic eruptions and ejection of entrained particles during steam eruptions causing phreatic eruptions[2].
Referencias[]
- ↑ United States Geological Survey. Tephra: Volcanic Rock and Glass Fragments. Retrieved on 2008-01-23.
- ↑ Heiken, G. & Wohletz, K. 1985. Volcanic Ash. University of California Press, Berkeley.