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Publikováno v:
Journal of Volcanology and Geothermal Research, Vol. 335 (2017) pp. 92-112
On 11 February 2010, Soufriere Hills Volcano, Montserrat, underwent a partial dome collapse (~ 50 × 106 m3) and a short-lived Vulcanian explosion towards the end. Three main pyroclastic units were identified N and NE of the volcano: dome-collapse py