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S. R. Young

Researcher at Montserrat Volcano Observatory

Publications -  33
Citations -  3392

S. R. Young is an academic researcher from Montserrat Volcano Observatory. The author has contributed to research in topics: Volcano & Magma. The author has an hindex of 25, co-authored 33 publications receiving 3218 citations. Previous affiliations of S. R. Young include British Geological Survey.

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Magma flow instability and cyclic activity at soufriere hills volcano, montserrat, british west indies

TL;DR: Dome growth at the Soufriere Hills volcano (1996 to 1998) was frequently accompanied by repetitive cycles of earthquakes, ground deformation, degassing, and explosive eruptions, which allowed short-term forecasting of timing, and of eruption style related to explosivity potential.
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Episodes of cyclic Vulcanian explosive activity with fountain collapse at Soufrière Hills Volcano, Montserrat

TL;DR: In 1997, the Soufriere Hills Volcano on Montserrat produced 88 Vulcanian explosions, with an initial high-intensity phase lasting a few tens of seconds and a lower-intensity, waning phase lasting 1 to 3 hours as mentioned in this paper.
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Growth patterns and emplacement of the andesitic lava dome at Soufrière Hills Volcano, Montserrat

TL;DR: The Soufriere Hills Volcano on Montserrat allowed the detailed documentation of a Pelean dome-forming eruption as discussed by the authors, which produced over 0.3 km 3 of crystal-rich andesitic lava.
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Overview of the eruption of Soufriere Hills Volcano, Montserrat, 18 July 1995 to December 1997

TL;DR: The onset of phreatic volcanic activity at the Soufriere Hills volcano, Montserrat on 18 July 1995 followed a three-year period of heightened volcano-seismic activity beneath the island as mentioned in this paper.
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The role of magma mixing in triggering the current eruption at the Soufriere Hills Volcano, Montserrat, West Indies

TL;DR: The andesite lava currently erupting at the Soufriere Hills volcano, Montserrat, contains ubiquitous mafic inclusions which show evidence of having been molten when incorporated into the andesites.