The 1995–present eruption of Soufrière Hills Volcano on Montserrat has produced over a
cubic kilometre of andesitic magma, creating a series of lava domes that were successively …

Volcano slope instability manifests in many forms, ranging from steady state to punctuated
movement, or shallow erosion to deep-seated spreading. The interplay of gravity, magmatic …

Volcanic eruptions on land create hot and fast pyroclastic density currents, triggering
tsunamis or surges that travel over water where they reach the ocean. However, no field …

Turbidity currents, and other types of underwater sediment density flow, are arguably the
most important flow process for moving sediment across our planet. Direct monitoring …

Abstract In 1997 Soufriére Hills Volcano on Montserrat produced 88 Vulcanian explosions:
13 between 4 and 12 August and 75 between 22 September and 21 October. Each episode …

An 11-minute sequence of laterally-directed explosions and retrogressive collapses on 5
November 2010 at Merapi (Indonesia) destroyed a rapidly-growing dome and generated …

The large explosive eruption of Merapi volcano, Indonesia, in 2010 presented a key, and
rare, opportunity to study the impacts of a major explosive eruption in a densely populated …

Eruption of the Soufrière Hills Volcano on Montserrat allowed the detailed documentation of
a Pélean dome-forming eruption. Dome growth between November 1995 and March 1998 …

The time series of sulphur dioxide (SO2) emissions during the continuing eruption of
Soufrière Hills Volcano, Montserrat, yields insights into conduit permeability and driving …

Pyroclastic flows were formed at Soufrière Hills Volcano by lava-dome collapse and by
fountain collapse associated with Vulcanian explosions. Major episodes of dome collapse …